<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Boukhenissa, Fares</style></author><author><style face="normal" font="default" size="100%">Drias, Tarek</style></author><author><style face="normal" font="default" size="100%">Azizi, Yacine</style></author><author><style face="normal" font="default" size="100%">Boufekane, Abdelmadjid</style></author><author><style face="normal" font="default" size="100%">Benabbas, Leyla</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Assessment of groundwater potential zones in an arid watershed using GIS and multi-criteria analysis: case of Khanguet Sidi Nadji, North-Eastern Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">Euro-Mediterranean Journal for Environmental Integration</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2026</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://link.springer.com/article/10.1007/s41207-025-01019-2</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">11</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	Arid regions of Algeria face persistent water crises due to recurrent droughts and growing water demand, especially for drinking water and agriculture. This pressure have led to overexploitation of local aquifers. Accurately identifying potential groundwater recharge zones is therefore critical for sustaining aquifer replenishment and water security. In this study, we assess groundwater recharge potential zones in the Khanguet Sidi Nadji watershed in North-Eastern Algeria, employing a spatial multi-criteria decision-making (MCDM) methodology which is based on the AHP, that integrates remote sensing and Geographic Information Systems (GIS). The work methodology uses essential data from ten (10) factors, including lithology, rainfall, curve number, land use, lineament density, slope, drainage density, peak runoff, and soil hydrogeological group. Thematic maps /layers of each factor are produced using ArcGIS 10.8 and integrated using AHP to generate a composite groundwater recharge potential map. Results indicate that areas with high recharge potential comprise approximately one-third of the watershed, covering 27% of the area, moderate potential covers 41% and low potential covers 32%. We validated the final recharge potential map by comparing it with data from 55 high-yield wells distributed across the watershed. A strong correlation (r = 0.74) was found between high-potential zones and well locations. Overall, the findings of this study provide a powerful decision-making tool that contributes to the improved exploitation and protection of groundwater resources, thereby enhancing sustainable water resources management and assisting in addressing the growing challenges of water scarcity in the arid regions of Algeria.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">6</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Schlüter, Nils</style></author><author><style face="normal" font="default" size="100%">Slami, Rafika</style></author><author><style face="normal" font="default" size="100%">Benyoucef,  Madani</style></author><author><style face="normal" font="default" size="100%">Garah,  Abdelmoumen</style></author><author><style face="normal" font="default" size="100%">Kennedy, W. James</style></author><author><style face="normal" font="default" size="100%">Walaszczyk, Ireneusz</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Coniacian (Late Cretaceous) echinoids from the southern Tethyan shelf (NE Algeria) with remarks on their palaeobiology and palaeobiogeography</style></title><secondary-title><style face="normal" font="default" size="100%">Cretaceous Research</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2026</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.1016/j.cretres.2025.106261</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">179</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	Thirteen echinoid taxa are described from Coniacian marl-limestone alternations in three sections south and east of Djebel Metlili, on the southwestern margin of the Aures Mountains in northeastern Algeria. The biostratigraphic framework, based on ammonites and inoceramids, indicates an early to middle Coniacian age. The identified taxa include:&amp;nbsp;&lt;em&gt;Rachiosoma rectilineatum&lt;/em&gt;,&amp;nbsp;&lt;em&gt;Phymosoma tamarinense&lt;/em&gt;,&amp;nbsp;&lt;em&gt;P&lt;/em&gt;. cf.&amp;nbsp;&lt;em&gt;P. mansour&lt;/em&gt;,&amp;nbsp;&lt;em&gt;Gomphechinus meslei&lt;/em&gt;,&amp;nbsp;&lt;em&gt;Coenholectypus subcrassus, Parapygus coquandi&lt;/em&gt;,&amp;nbsp;&lt;em&gt;Petalobrissus trigonopygus&lt;/em&gt;,&amp;nbsp;&lt;em&gt;P&lt;/em&gt;.&amp;nbsp;&lt;em&gt;rimula&lt;/em&gt;,&amp;nbsp;&lt;em&gt;Hemiaster&lt;/em&gt;&amp;nbsp;sp., and&amp;nbsp;&lt;em&gt;Mecaster fourneli&lt;/em&gt;. Three new species are described,&amp;nbsp;&lt;em&gt;Orthopsis metliliae&lt;/em&gt;&amp;nbsp;sp. nov.,&amp;nbsp;&lt;em&gt;Coenholectypus sulcatus&lt;/em&gt;&amp;nbsp;sp. nov. and a new genus and species referred to the family Phymosomatoidae,&amp;nbsp;&lt;em&gt;Triboporus luluatus&lt;/em&gt;&amp;nbsp;gen. et sp. nov. A large amount of well-documented material, comprising 579 specimens, was collected, with the fauna being dominated by the spatangoid&amp;nbsp;&lt;em&gt;Mecaster fourneli&lt;/em&gt;. At the genus level, the fauna exhibits characteristics typical of the Tethyan realm, and includes&amp;nbsp;&lt;em&gt;Rachiosoma&lt;/em&gt;,&amp;nbsp;&lt;em&gt;Gomphechinus&lt;/em&gt;,&amp;nbsp;&lt;em&gt;Mecaster&lt;/em&gt;,&amp;nbsp;&lt;em&gt;Parapygus&lt;/em&gt;&amp;nbsp;and&amp;nbsp;&lt;em&gt;Petalobrissus&lt;/em&gt;. However, at the species level, most taxa are restricted to Algeria. Some are also found in adjacent countries such as Tunisia and Egypt.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Benmansour, Sana</style></author><author><style face="normal" font="default" size="100%">Kherchouche, Adila</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">New data on the genus Hemipneustes from the Upper Cretaceous of the Aurès Basin (NE Algeria)</style></title><secondary-title><style face="normal" font="default" size="100%">Journal of African Earth Sciences</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2026</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.sciencedirect.com/science/article/abs/pii/S1464343X25003656?via%3Dihub</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">223</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	This study investigates the biostratigraphic and paleobiogeographic significance of&amp;nbsp;&lt;em&gt;Hemipneustes africanus&lt;/em&gt;&amp;nbsp;Deshayes, 1848, with a special attention on its temporal extent and geographical distribution during the Late Cretaceous. The overarching scientific question investigated herein tackles the significance of the distribution and stratigraphic position of this taxon in elucidating its faunal provincialism and dispersal limits within the southern Tethys.
&lt;/p&gt;

&lt;p style=&quot;text-align: justify;&quot;&gt;
	A newly discovered and well-dated occurrence of&amp;nbsp;&lt;em&gt;H. africanus&lt;/em&gt;&amp;nbsp;is described in a new area of the Aurès Basin, within the Beni Fedhala syncline (Maafa–Djebel Gueroun, Algeria). This taxon was found associated with the ammonite index species&amp;nbsp;&lt;em&gt;Nostoceras&lt;/em&gt;&amp;nbsp;(&lt;em&gt;Bostrychoceras&lt;/em&gt;)&amp;nbsp;&lt;em&gt;polyplocum&lt;/em&gt;&amp;nbsp;(Roemer, 1841), within the Total Range Zone of the planktic foraminifer&amp;nbsp;&lt;em&gt;Globotruncana calcarata&lt;/em&gt;&amp;nbsp;Cushman, 1927, which indicates a Late Campanian age.
&lt;/p&gt;

&lt;p style=&quot;text-align: justify;&quot;&gt;
	The present record represents one of the earliest chronostratigraphically constrained reports of the genus&amp;nbsp;&lt;em&gt;Hemipneustes&lt;/em&gt;&amp;nbsp;in the upper Campanian. The limited geographic distribution of the species, restricted to Algeria, Tunisia and Spain, suggests low dispersal ability, further contributing to our general understanding of the regional faunal differentiation within the southern Tethyan region during the Late Cretaceous.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Moud, Fatma-Zohra</style></author><author><style face="normal" font="default" size="100%">Benmansour, Sana</style></author><author><style face="normal" font="default" size="100%">Reolid, Matías</style></author><author><style face="normal" font="default" size="100%">Brahim, El Hadj-Youcef</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Shallow marine carbonates from the middle Turonian-Coniacian of the Bellezma-Batna mountains (northeastern Algeria): facies analysis, sequence stratigraphy and palaeoenvironmental reconstruction</style></title><secondary-title><style face="normal" font="default" size="100%">Carbonates and Evaporites</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2026</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://link.springer.com/article/10.1007/s13146-025-01222-w</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">41</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	A comprehensive study of the lithological, sedimentological and palaeontological characteristics of deposits belonging to the middle Turonian to Coniacian age in the Bellezma-Batna Mountains was carried out in order to establish a new biostratigraphic framework and interpret the evolution of the palaeoenvironment and sea-level fluctuation during this period. The studied sequences, exposed at Chaabet (Djebel Boukezzez) and Chihat, are mostly composed of marls and limestones. They are mainly composed of three formations: the Marly Limestone of the Chaabet Formation, the Upper Limestone of the Berriche Formation and the Marls of the Chaabet Formation. Biostratigraphic interpretations were based mainly on planktic and benthic foraminifera (&lt;i&gt;H. helvetica&lt;/i&gt;,&amp;nbsp;&lt;i&gt;Marginotruncana&lt;/i&gt;&amp;nbsp;cf.&amp;nbsp;&lt;i&gt;sigali&lt;/i&gt;,&amp;nbsp;&lt;i&gt;Discorbis turnicus&lt;/i&gt;,&amp;nbsp;&lt;i&gt;Nezzazatinella picardi&lt;/i&gt;&amp;nbsp;HENSON), ostracods (&lt;i&gt;Ovocytheridea&lt;/i&gt;&amp;nbsp;sp.,&amp;nbsp;&lt;i&gt;Brachycythere ekpo&lt;/i&gt;), and rudists&amp;nbsp;&lt;i&gt;Vaccinites praegiganteus&lt;/i&gt;, from the lower limestone member at both the Chaabet and Chihat sections, which is considered as a good indicator of the Upper Turonian age. Fourteen types of microfacies were identified and grouped into three facies assemblages- outer, middle, and inner ramp—based on sedimentological and palaeontological features. Sequence stratigraphic analysis establishes five sedimentary sequences that mark successive cycles of transgression and regression. A significant rise in sea level during the middle Turonian led to deep open marine conditions, followed by a regression in the late Turonian and early Coniacian that led to progressively shallower environments. These fluctuations reflect the combined effects of eustatic changes and regional tectonic movements.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">21</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Moud, Fatma-Zohra</style></author><author><style face="normal" font="default" size="100%">Benmansour, Sana</style></author><author><style face="normal" font="default" size="100%">Reolid, Matías</style></author><author><style face="normal" font="default" size="100%">Brahim,  El Hadj Youcef</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Shallow marine carbonates from the middle Turonian-Coniacian of the Bellezma-Batna mountains (northeastern Algeria): facies analysis, sequence stratigraphy and palaeoenvironmental reconstruction</style></title><secondary-title><style face="normal" font="default" size="100%">Carbonates and Evaporites</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2026</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://link.springer.com/article/10.1007/s13146-025-01222-w</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">41</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	A comprehensive study of the lithological, sedimentological and palaeontological characteristics of deposits belonging to the middle Turonian to Coniacian age in the Bellezma-Batna Mountains was carried out in order to establish a new biostratigraphic framework and interpret the evolution of the palaeoenvironment and sea-level fluctuation during this period. The studied sequences, exposed at Chaabet (Djebel Boukezzez) and Chihat, are mostly composed of marls and limestones. They are mainly composed of three formations: the Marly Limestone of the Chaabet Formation, the Upper Limestone of the Berriche Formation and the Marls of the Chaabet Formation. Biostratigraphic interpretations were based mainly on planktic and benthic foraminifera (&lt;i&gt;H. helvetica&lt;/i&gt;,&amp;nbsp;&lt;i&gt;Marginotruncana&lt;/i&gt;&amp;nbsp;cf.&amp;nbsp;&lt;i&gt;sigali&lt;/i&gt;,&amp;nbsp;&lt;i&gt;Discorbis turnicus&lt;/i&gt;,&amp;nbsp;&lt;i&gt;Nezzazatinella picardi&lt;/i&gt;&amp;nbsp;HENSON), ostracods (&lt;i&gt;Ovocytheridea&lt;/i&gt;&amp;nbsp;sp.,&amp;nbsp;&lt;i&gt;Brachycythere ekpo&lt;/i&gt;), and rudists&amp;nbsp;&lt;i&gt;Vaccinites praegiganteus&lt;/i&gt;, from the lower limestone member at both the Chaabet and Chihat sections, which is considered as a good indicator of the Upper Turonian age. Fourteen types of microfacies were identified and grouped into three facies assemblages- outer, middle, and inner ramp—based on sedimentological and palaeontological features. Sequence stratigraphic analysis establishes five sedimentary sequences that mark successive cycles of transgression and regression. A significant rise in sea level during the middle Turonian led to deep open marine conditions, followed by a regression in the late Turonian and early Coniacian that led to progressively shallower environments. These fluctuations reflect the combined effects of eustatic changes and regional tectonic movements.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">21</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Athamena, Ali</style></author><author><style face="normal" font="default" size="100%">Gaagai, Aissam</style></author><author><style face="normal" font="default" size="100%">Aouissi, Hani-Amir</style></author><author><style face="normal" font="default" size="100%">Cheniti, Hamza</style></author><author><style face="normal" font="default" size="100%">Halima Belalite</style></author><author><style face="normal" font="default" size="100%">Touati, Billel</style></author><author><style face="normal" font="default" size="100%">Yahyaoui, Habibi</style></author><author><style face="normal" font="default" size="100%">Kebaili, Feriel-Kheira</style></author><author><style face="normal" font="default" size="100%">Ziad, Sabrina</style></author><author><style face="normal" font="default" size="100%">Elsayed, Salah</style></author><author><style face="normal" font="default" size="100%">Elbeltagi, Ahmed</style></author><author><style face="normal" font="default" size="100%">Salem, Ali</style></author><author><style face="normal" font="default" size="100%">Yaseen, Zaher Mundher</style></author><author><style face="normal" font="default" size="100%">Gad, Mohamed</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Groundwater quality assessment for agricultural utilizing indexical and machine learning techniques in Ouled Djellal Aquifer, Southern Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">scientific reports </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2026</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.nature.com/articles/s41598-026-38208-0</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	Groundwater represents the main water resource for irrigation in the Ouled Djellal region (southeast of Algeria). Despite the importance of groundwater in this area, its quality and sustainability remain insufficiently studied. Therefore, this study aimed to introduce an integrated analytical framework by combining multivariate statistical techniques i.e., Principal Component Analysis (PCA) and Hierarchical Ascending Classification (HAC), irrigation indices (IWQI, SAR, Na%, SSP, PS, and RSC), and machine learning (ML) models such as Artificial Neural Network (ANN), Support Vector Machine (SVM), and Multiple Linear Regression (MLR) to assess and predict groundwater quality for irrigation. The main difference with previous studies is the fact that this work applied Empirical Bayesian Kriging Regression Prediction (EBKRP) to spatialize irrigation indices derived from ML with higher precision. The approach enables cross-validation of model performance and captures complex nonlinear interactions among hydrochemical parameters. The attained results revealed that groundwater quality was varied from moderate to poor for irrigation, driven mainly by salinity and sodicity effects. In addition, the ANN model achieved the highest predictive accuracy (R² = 0.97, RMSE = 1.50), confirming its superiority in modelling complex hydrochemical behavior. The proposed modelling framework represents a methodological advancement for data-scarce arid regions, serving as a practical tool adaptable to groundwater monitoring and irrigation planning in similar regions.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Khelili, M</style></author><author><style face="normal" font="default" size="100%">Anoune, N</style></author><author><style face="normal" font="default" size="100%">Haoues,  Cherif</style></author><author><style face="normal" font="default" size="100%">Abdelhamid Khedidja</style></author><author><style face="normal" font="default" size="100%">Drifi, Naima</style></author><author><style face="normal" font="default" size="100%">Chorfi, K</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Multi-Criteria Evaluation of Land Suitability for Urban Extension Areas Identified in the PDAU of Setif City Using GIS and AHP</style></title><secondary-title><style face="normal" font="default" size="100%">International Journal of Geoinformatics</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2025</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.52939/ijg.v21i11.4603</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">21</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	Urban planning plays a critical role in sustainable city development by guiding urban expansion efficiently. In Algeria, the master plan for development and urban planning (PDAU) designates specific areas for city growth, yet the suitability of these areas for urban extension often remains unassessed using systematic methods. Most PDAU, including the plan for Setif City established in 2016, rely on planning approaches and data that risk becoming outdated due to rapid urban changes and evolving spatial dynamics. As a result, there is a pressing need to critically assess and validate these designated extension zones using updated, objective analytical tools. This study addresses this gap by applying an integrated approach combining Geographic Information Systems (GIS) and the Analytic Hierarchy Process (AHP) to evaluate land suitability for urban extension in Setif City.&amp;nbsp;Fifteen socio-economic, physical, environmental, and accessibility criteria were applied to assess areas designated in the PDAU. The methodology enables a multi-criteria, data-driven analysis to prioritize zones for sustainable urban growth. About 21.5% of the study area is categorized as very high suitability, and most of these sites are concentrated around the edges of the city.&amp;nbsp;36.7% is classified as high suitability, according to the suitability analysis for future urban expansion. Moderately and poorly suitable areas make up 23.79% and 13% of the total. Merely 5% of the land is deemed to be extremely unsuitable for the extension. The findings support evidence-based urban planning, offering actionable insights for policymakers and urban planners. This study contributes methodologically by demonstrating the effective integration of AHP with GIS in an Algerian context, encouraging replication and further research in similar urban environments.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">11</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Mansouri, Zineb</style></author><author><style face="normal" font="default" size="100%">Dinar, Haythem</style></author><author><style face="normal" font="default" size="100%">Belkendil, Abdeldjalil</style></author><author><style face="normal" font="default" size="100%">Bakelli, Omar</style></author><author><style face="normal" font="default" size="100%">Drias, Tarek</style></author><author><style face="normal" font="default" size="100%">Assadi, Amine-Aymen</style></author><author><style face="normal" font="default" size="100%">Khezami, Lotfi</style></author><author><style face="normal" font="default" size="100%">Mouni, Lotfi</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Integrated Groundwater Quality Assessment for Irrigation in the Ras El-Aioun District: Combining IWQI, GIS, and Machine Learning Approaches</style></title><secondary-title><style face="normal" font="default" size="100%">Water</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2025</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.3390/w17111698</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">17</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	This study focuses on assessing the hydrogeochemical characteristics and irrigation suitability of groundwater in the Ras El Aioun and Merouana districts, using an integrated approach that combines physicochemical analysis, machine learning (ML), and Geographic Information Systems (GISs). Thirty groundwater samples were collected in June 2023 and subjected to extensive analyses, including major ions (Ca&lt;sup&gt;2+&lt;/sup&gt;, Mg&lt;sup&gt;2+&lt;/sup&gt;, Na&lt;sup&gt;+&lt;/sup&gt;, K&lt;sup&gt;+&lt;/sup&gt;, HCO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;−&lt;/sup&gt;, Cl&lt;sup&gt;−&lt;/sup&gt;, SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2−&lt;/sup&gt;), pH, TDS, alkalinity, and hardness. Hydrochemical facies analysis revealed that the Ca-HCO&lt;sub&gt;3&lt;/sub&gt;&amp;nbsp;type was dominant (93.33%), with some samples exceeding FAO limits, particularly for Na&lt;sup&gt;+&lt;/sup&gt;, K&lt;sup&gt;+&lt;/sup&gt;, SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2−&lt;/sup&gt;, Cl&lt;sup&gt;−&lt;/sup&gt;, Mg&lt;sup&gt;2+&lt;/sup&gt;, and HCO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;−&lt;/sup&gt;. Assessment of groundwater irrigation suitability revealed generally favorable conditions based on three key parameters: all samples (100%) were classified as excellent based on the Sodium Adsorption Ratio (SAR &amp;lt; 10), 70% showed good-to-permissible status by Sodium Percentage (Na% &amp;lt; 60), and 83.3% were within safe limits for Residual Sodium Carbonate (RSC &amp;lt; 1.25 meq/L). However, the Permeability Index (PI &amp;gt; 75%) categorized 96.7% of samples as unsuitable for long-term irrigation due to potential soil permeability reduction. Additionally, Total Hardness (TH &amp;lt; 75 mg/L) indicated predominantly soft water characteristics (90% of samples), particularly in the central study area, suggesting possible limitations for certain agricultural applications that require mineral-rich water. GIS-based spatial analysis showed that irrigation suitability was higher in the eastern and western regions than in the central zone. Advanced machine learning algorithms provide superior predictive capability for water quality parameters by effectively modeling complex, non-linear feature interactions that conventional statistical approaches frequently fail to capture. Three ML models—Support Vector Regression (SVR), Random Forest (RF), and Extreme Gradient Boosting (XGBoost)—were used to predict the Irrigation Water Quality Index (IWQI). XGBoost outperformed the others (RMSE = 2.83, R&lt;sup&gt;2&lt;/sup&gt;&amp;nbsp;= 0.957), followed by RF (RMSE = 3.12, R&lt;sup&gt;2&lt;/sup&gt;&amp;nbsp;= 0.93) and SVR (RMSE = 3.45, R&lt;sup&gt;2&lt;/sup&gt;&amp;nbsp;= 0.92). Integrating ML and GIS improved groundwater quality assessment and provided a robust framework for sustainable irrigation management. These findings provide critical insights for optimizing agricultural water use in water-scarce regions.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">11</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Reghais, Azzeddine</style></author><author><style face="normal" font="default" size="100%">Drouiche, Abdelmalek</style></author><author><style face="normal" font="default" size="100%">Zahi, Faouzi</style></author><author><style face="normal" font="default" size="100%">Ewuzie, Ugochukwu</style></author><author><style face="normal" font="default" size="100%">Debieche, Taha-Hocine</style></author><author><style face="normal" font="default" size="100%">Drias, Tarek</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Risk assessment of potentially toxic elements and mapping of groundwater pollution indices using soft computer models in an agricultural area, Northeast Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">Journal of Hazardous Materials</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2025</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.1016/j.jhazmat.2025.137991</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">491</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	Groundwater (GW) quality and contamination by potentially toxic elements (PTEs) are major concerns for environmental&amp;nbsp;sustainability, particularly in arid regions. The aim of this study was to assess the human health risks associated with&amp;nbsp;GW contamination&amp;nbsp;by PTEs in the Terminal Complex (TC) aquifer of the Tolga oasis, located in northeastern Algeria. Seventeen GW samples were analyzed using standard methods to determine contamination levels and associated health risks. Results showed that GW was generally contaminated with lead (Pb), which exceeded the WHO permissible limit of 0.01 mg/L in 76.47 % of the samples. Although some samples were rich in Cr and Mn, their levels were below WHO guidelines.&amp;nbsp;Pollution indices, including Contamination Factor (CF), Heavy Metal Pollution Index (HMI), and Nemerow Pollution Index (NPI), indicated that over 50 % of the samples had medium to high pollution levels. These indices were further estimated using&amp;nbsp;artificial neural network&amp;nbsp;(ANN) and Multiple Linear Regression (MLR) machine learning models, whose performances were validated by&amp;nbsp;Root Mean Square Error&amp;nbsp;(RMSE), Mean Absolute Error (MAE), and Nash-Sutcliffe Efficiency Coefficient (NSE). The Taylor diagram analysis showed that MLR models were more accurate than ANN models in estimating GW pollution indices. Mapping these indices using&amp;nbsp;support vector machine&amp;nbsp;(SVM) algorithms and applying chemometric statistical techniques, including principal component analysis (PCA), revealed that alteration of geological formations and anthropogenic activities significantly affected&amp;nbsp;GW contamination&amp;nbsp;by PTEs in the study area. The assessment of health risks associated with heavy metals revealed a significant non-carcinogenic risk, particularly for children, with 41.17 % of samples exceeding the hazard index threshold of 1 due to Pb exposure, while carcinogenic risks were low. This study establishes predictive models based on heavy metal pollution indices, providing crucial information on the spatial distribution of GW contamination. The results support the development of targeted mitigation strategies and intervention plans to safeguard GW resources and public health in the region.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Bouchemla, Imad</style></author><author><style face="normal" font="default" size="100%">Benyoucef,  Madani</style></author><author><style face="normal" font="default" size="100%">Garah,  Abdelmoumen</style></author><author><style face="normal" font="default" size="100%">Salamon, Mariusz</style></author><author><style face="normal" font="default" size="100%">Krajewski, Marcin</style></author><author><style face="normal" font="default" size="100%">Slami, Rafika</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Trace fossils from the middle Aptian sedimentary succession of the Bellezma Mountains, NE Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">Boletín de la Sociedad Geológica Mexicana</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2025</style></year></dates><volume><style face="normal" font="default" size="100%">77</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	The Aptian sedimentary succession exposed in the southern Bellezma Mountains contains a low diversity trace fossil assemblage, with ichnofossils being common in the middle part of the studied section. The recorded trace fossils comprise eight ichnogenera: Archaeonassa, Cochlichnus, Chondrites, Gyrochorte, Palaeophycus, Protovirgularia, Rhizocorallium, and Thalassinoides. Ethologically, these ichnogenera display feeding, crawling, and dwelling activities of epi- and infaunal organisms. The presence of these trace fossils is mainly related to the activity of the deposit feeders, due to the accumulation of nutrients on the seafloor in unconsolidated, poorly sorted, soft substrate after storms under good environmental conditions. Together with sedimentological features, the ichnoassemblage suggests that the studied Aptian sedimentary succession was deposited in the upper offshore zone, corresponding to the Cruziana ichnofacies. These trace fossils are reported herein for the first time in the Bellezma Mountains. Furthermore, this study represents the first investigation of Mesozoic trace fossils in eastern Algeria.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">1</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Benmansour, Sana</style></author><author><style face="normal" font="default" size="100%">Benmessaouda, Hadil</style></author><author><style face="normal" font="default" size="100%">Drifi, Naima</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Growth anatomical anomalies in Cenomanian echinoids of the Bellezma-Batna Mountains (NE Algeria)</style></title><secondary-title><style face="normal" font="default" size="100%">Journal of African Earth Sciences</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2025</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.1016/j.jafrearsci.2025.105560</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">224</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	This article reports cases of growth anatomical anomalies in two echinoid species,&amp;nbsp;&lt;em&gt;Macraster douvillei&lt;/em&gt;&amp;nbsp;(Gauthier) and&amp;nbsp;&lt;em&gt;Mecaster pseudofourneli&lt;/em&gt;&amp;nbsp;(Péron and Gauthier), from the&amp;nbsp;Cenomanian&amp;nbsp;deposits of the Bellezma-Batna mountains (northeastern Algeria). Such a topic is first reported in Algeria ever. The large collection (400 specimens) made it possible to distinguish several types of these rare pathologies, each one being illustrated by explanatory drawings. Three types of deformation directly concerning the pentamery, are presented. They are most often resulting from an additional growth zone (6 ambulacra), a complete tetramery represented by a missing growth zone (4 ambulacra) and constrictions or strangulation of the ambulacres. Abnormalities can develop in the rudiment as soon as the larva enters metamorphosis, or shortly afterwards in juvenile broods. They may alter the plate arrangement and the general shape of the test or, on the contrary, result in local deformations, influencing the arrangement or shape of the ambulacra, etc. These malformations resulted from either intrinsic (genetic) or extrinsic (ambiental) conditions.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Kherchouche, Adila</style></author><author><style face="normal" font="default" size="100%">Benmansour, Sana</style></author><author><style face="normal" font="default" size="100%">Alhejoj, Ikhlas</style></author><author><style face="normal" font="default" size="100%">Farouk, Sherif</style></author><author><style face="normal" font="default" size="100%">Feldman, Howard-R</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">The first record of the genus orbirhynchia (Brachiopoda: tetrarhynchidae) from the upper Campanian of Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">Historical Biology</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2025</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.1080/08912963.2024.2371963</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">37</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	The species&amp;nbsp;&lt;i&gt;Orbirhynchia mantilliana&lt;/i&gt;&amp;nbsp;is newly documented in Algeria, identified within the Upper Campanian marly limestone of the Akhdar Member in the Abiod Formation at Djabel Gueroun, Batna Province, Aurès Basin. It is associated with Upper Campanian faunal markers such as the ammonite species&amp;nbsp;&lt;i&gt;Nostoceras&lt;/i&gt;&amp;nbsp;(&lt;i&gt;Bostrychoceras&lt;/i&gt;)&amp;nbsp;&lt;i&gt;polyplocum&lt;/i&gt;, found within the planktic foraminifera&amp;nbsp;&lt;i&gt;Globotruncana calcarata&lt;/i&gt;&amp;nbsp;Zone. The&amp;nbsp;&lt;i&gt;O. mantilliana&lt;/i&gt;&amp;nbsp;displays a restricted geographic distribution and biogeographic range, confined to Algeria, the United Kingdom, and Germany.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">4</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>5</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Bachir Lamouri</style></author><author><style face="normal" font="default" size="100%">Labadi, Abdellah-Seddik</style></author><author><style face="normal" font="default" size="100%">Fouad Djaiz</style></author><author><style face="normal" font="default" size="100%">Guettal, Adel</style></author><author><style face="normal" font="default" size="100%">Boukoffa, Machati</style></author><author><style face="normal" font="default" size="100%">Chouaf, Ibtissem</style></author><author><style face="normal" font="default" size="100%">Bouabsa, Lakhdar</style></author><author><style face="normal" font="default" size="100%">Fagel, Nathalie</style></author><author><style face="normal" font="default" size="100%">Chouabbi, Abdelmadjid</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Mineralogical Characterization of the Eocene Clays in the Ghoufi Region &amp;ldquo;Saharan Atlas&amp;rdquo; Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">Recent Research on Sedimentology, Stratigraphy, Paleontology, Tectonics, Geochemistry, Volcanology and Petroleum Geology </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2025</style></year></dates><pages><style face="normal" font="default" size="100%">57-61</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	The aim of this work is to characterize clays of Middle Eocene age from the Ghoufi-Atlas Saharan region, Algeria, in order to know the fields of their use and their eventual valuation. To this end, an outcrop sampling campaign was carried out across these formations. The samples collected were analyzed by X-ray diffraction (XRD), X-ray fluorescence (XRF), and Scanning Electron Microscopy (SEM). Potential samples rich in clay fraction were further analyzed using laser granulometry, physicochemical tests, and copper adsorption recovery tests. The results showed that the clay fraction, which varies between 71 and 86%, are entirely represented Palygorskite, accompanied by 06–18% of dolomite, 03–7% of calcite, and traces of quartz as non-clay minerals. Further analysis showed that these clays have a cation exchange capacity (CEC) of 07 and 07.16 meq/100 g and a specific surface area (SS) of 57 and 60 m&lt;sup&gt;2&lt;/sup&gt;/g. Copper adsorption tests have shown that fixation kinetics are very rapid and that these clays have a very high adsorption capacity.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Chairat, Imen</style></author><author><style face="normal" font="default" size="100%">Hanini, Amine</style></author><author><style face="normal" font="default" size="100%">Fouad Djaiz</style></author><author><style face="normal" font="default" size="100%">Zagrarni,Mohamed-Faouzi</style></author><author><style face="normal" font="default" size="100%">Mabrouk Boughdiri</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Integrated Analysis of Facies and Organic Matter Distribution in the Bahloul Formation (NE Algeria &amp;ndash; NW Tunisia)</style></title><secondary-title><style face="normal" font="default" size="100%">First African Conference for Early-Career Geoscientists, December </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2025</style></year></dates><pub-location><style face="normal" font="default" size="100%">Tunisia</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	This presentation examines the Cenomanian–Turonian Bahloul Formation in NE Algeria and NW Tunisia through integrated facies, stratigraphic, structural, and geochemical analysis. It highlights the role of synsedimentary tectonics and OAE2-related sea-level rise in controlling organic-matter distribution and source-rock development in the Algero-Tunisian Atlassic Basin.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Athamena, Ali</style></author><author><style face="normal" font="default" size="100%">Halima Belalite</style></author><author><style face="normal" font="default" size="100%">Aouissi, Hani-Amir</style></author><author><style face="normal" font="default" size="100%">Athamena,Malika</style></author><author><style face="normal" font="default" size="100%">Boughediri, M</style></author><author><style face="normal" font="default" size="100%">Laamouri, B</style></author><author><style face="normal" font="default" size="100%">Gaagai, Aissam</style></author><author><style face="normal" font="default" size="100%">Kebaili, Feriel-Kheira</style></author><author><style face="normal" font="default" size="100%">Benselhoub, A</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">ORIGIN, EVOLUTION AND ASSESSMENT OF THE HYDROGEOCHEMICAL FUNCTIONING OF A THERMAL MINERAL SPRING IN BATNA (EASTERN ALGERIA)</style></title><secondary-title><style face="normal" font="default" size="100%">Scientific Notes of Sumy State Pedagogical University. Geographical Sci.</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2025</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://scinotesgeo.at.ua/Vol2_Iss6/2025_SNSSPU.pdf#page=3</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">2</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	A hydrogeological study of the thermal source of Ouled Aïcha in the Aurès Mountains showed that the source emerges in a particular natural context mainly represented by the presence of a vertical fault in the NE-SW direction affecting Cretaceous limestone. This supports the increase on the surface of moderately hot water, whose temperature is approximately 30 °C and an exploited flow of 3 L·s-1. The vertical electric sounding in situ showed the in-depth presence of a saliferous conducting level within a calcareous-resistant mass, which probably settled in the fault's favor. The presence of this saliferous level strongly influences the hydrochemistry of this thermal source. Thus, the water from the source is characterized by high salinity due to its temperature, which favors the dissolution of mineral salts in sufficient quantity throughout its journey (12390 µS/cm). The high concentrations of chlorides, sodium and sulfates indicate a significant contribution of salt from evaporitic formations as for the calcium content indicates that this water is influenced by the dissolution of carbonate formations. These physicochemical characteristics provide this water therapeutic virtue, which can be attributed to its chemical composition, high rock salt content, and low nitrate content. Geothermometry has shown that these thermal waters acquire a high temperature in their original tanks coming from a depth through a fault system that affects the basement.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">6</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Touati, Billel</style></author><author><style face="normal" font="default" size="100%">Zhang, Zizhan</style></author><author><style face="normal" font="default" size="100%">Athamena, Ali</style></author><author><style face="normal" font="default" size="100%">Ni,  Sidao</style></author><author><style face="normal" font="default" size="100%">Chu, Risheng</style></author><author><style face="normal" font="default" size="100%">Wang,  Yan</style></author><author><style face="normal" font="default" size="100%">Yahyaoui, Habibi</style></author><author><style face="normal" font="default" size="100%">Xiao, Cuiyu</style></author><author><style face="normal" font="default" size="100%">Bellalem, Fouzi</style></author><author><style face="normal" font="default" size="100%">Osotuyi, Abayomi-Gaius</style></author><author><style face="normal" font="default" size="100%">Guellouh, Sami</style></author><author><style face="normal" font="default" size="100%">Chen, Yongyan</style></author><author><style face="normal" font="default" size="100%">Gu, Wangwang</style></author><author><style face="normal" font="default" size="100%">Houichi,  Larbi</style></author><author><style face="normal" font="default" size="100%">Halima Belalite</style></author><author><style face="normal" font="default" size="100%">Athamena,Malika</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Integrated analysis of precipitation and runoff trends in the Wadi Bouhamdane Basin, NE Algeria</style></title><secondary-title><style face="normal" font="default" size="100%"> Mediterranean Geoscience Reviews</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2025</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://link.springer.com/article/10.1007/s42990-025-00155-9</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">7</style></volume><pages><style face="normal" font="default" size="100%">159–179</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	Evaluating hydrological trends is crucial for the sustainable management of water resources with the escalating impacts of climate change. This study assesses the Wadi Bouhamdane Basin in Northeast Algeria, integrating data from the Gravity Recovery and Climate Experiment (GRACE) and the Follow-On mission (GRACE-FO) with hydrological observations and modeling to provide insights into precipitation and runoff dynamics since 1991. Using techniques such as linear regression, the Mann–Kendall trend test, cumulative departure, mutation analysis, and Morlet wavelet transformations, we identified a declining trend in annual rainfall (− 36.85&amp;nbsp;mm/decade) and an increase in runoff (20.65&amp;nbsp;mm/decade). Our rainfall analysis projected droughts from 2018 to 2020 and a water-rich phase in 2024, with predicted fluctuations extending into 2025. GRACE/GFO data from 2002 to 2022 revealed consistent reductions in terrestrial water storage (~ 0.35&amp;nbsp;cm/year), marked declines during projected drought periods, and insights into post-drought recovery and water accumulation trends. These findings are consistent with the projected wet–dry fluctuations from 2021 to 2023 and suggest the onset of a wetter period around 2024. The runoff sequence is projected to maintain its slight upward trend from 2018 to 2019, with fluctuations from 2018 to 2020, a dry period from 2022 to 2024, and a predicted dry year in 2025. Our combined approach of satellite data with ground-based measurements highlights the complex interactions influencing hydrological responses in semi-arid regions. This study underscores the significance of merging conventional hydrological methods with advanced satellite observations to enhance water management precision and resilience, advocating for a multi-source data framework to inform sustainable water resource policies amid evolving climate conditions.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Hfaiedh, Emna</style></author><author><style face="normal" font="default" size="100%">Gaagai, Aissam</style></author><author><style face="normal" font="default" size="100%">Ben Moussa, Amor</style></author><author><style face="normal" font="default" size="100%">Petitta, Marco</style></author><author><style face="normal" font="default" size="100%">Mlayah, Ammar</style></author><author><style face="normal" font="default" size="100%">Elsayed, Salah</style></author><author><style face="normal" font="default" size="100%">Elsherbiny, Osama</style></author><author><style face="normal" font="default" size="100%">Hamdy Eid, Mohamed</style></author><author><style face="normal" font="default" size="100%">Tariq, Aqil</style></author><author><style face="normal" font="default" size="100%">Athamena, Ali</style></author><author><style face="normal" font="default" size="100%">Gad, Mohamed</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">An Innovative ML and GIS-Integrated Approach for Predicting Irrigation Water Quality in Coastal Aquifers</style></title><secondary-title><style face="normal" font="default" size="100%">Earth Systems and Environment </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2025</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://link.springer.com/article/10.1007/s41748-025-00851-4</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	Groundwater from coastal aquifers plays a significant role in agriculture, but its diminishing of quality often impacts crop production and soil sustainability by leading to soil salinization and the deterioration of irrigation water standards. This study addresses the pressing issue at Mornang Plain in Tunisia utilizing an integrated approach that combines statistical analysis (principal component analysis (PCA) and cluster analysis (CA), geographic information system (GIS), and machine learning (ML) techniques to assess and predict irrigation water quality. Key parameters such as irrigation water quality index (IWQI), potential salinity (PS), sodium percentage (Na%), and sodium adsorption ratio (SAR) were evaluated to assess water quality for agricultural use. The study identified three main groundwater facies (Na-Cl, Ca-Mg-SO&lt;sub&gt;4&lt;/sub&gt;, Ca-Mg-Cl/SO&lt;sub&gt;4&lt;/sub&gt;), that displaying distinct chemical signatures shaped by geological, hydrological, and human processes. The analysis showed that over 65% of the groundwater samples fall within the “unsuitable” category for irrigation, with high to severe constraints for soil and crop sustainability. A novel decision tree (DT) based ML model was optimized to predict these irrigation indices, achieving high performance with fewer input parameters. With low RMSE values and R&lt;sup&gt;2&lt;/sup&gt;&amp;nbsp;values ranging from 0.706 to 0.996 across several indices, the DT models showed remarkable predictive accuracy. The models’ efficiency in producing accurate water quality forecasts at lower analytical costs is demonstrated by their R&lt;sup&gt;2&lt;/sup&gt; = 0.992 (RMSE = 1.693) for IWQI and 0.996 (RMSE = 0.822) for PS. This approach provides a cost-effective alternative to traditional methods by reducing the number of chemical parameters required for analysis. The results of this study offer significant insights for water resource management in arid and semi-arid regions, highlighting the potential of ML techniques in predicting irrigation water quality. The findings are valuable not only for Tunisia but also for similar regions worldwide, offering a tool for decision-makers to develop sustainable water management strategies and improve agricultural practices globally.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Chibane, Hocine</style></author><author><style face="normal" font="default" size="100%">Menani, Mohamed-Redha</style></author><author><style face="normal" font="default" size="100%">Bouhidel, Kamel-Eddine</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Study of the impact of various supplies on the quality of surface water</style></title><secondary-title><style face="normal" font="default" size="100%">MILITARY TECHNICAL COURIER</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2025</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.5937/vojtehg73-50508 </style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">73</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	&lt;strong&gt;Introduction purpose:&lt;/strong&gt; As population growth and industrial expansion continue, surface freshwater reservoirs such as dams have become increasingly vital due to their accessibility and ease of treatment. However, the quality of these water sources has significantly deteriorated, primarily due to the discharge of domestic and industrial wastewater. The proliferation of extensive algal blooms has led to significant challenges in maintaining drinking water quality and raised concerns about public health. This study investigates the impact of various water sources on the physicochemical quality of an Algerian dam over four seasons (December 2020 - October 2021) and explores the factors influencing the occurrence of cyanobacterial blooms to better understand and manage this excessive growth.
&lt;/p&gt;

&lt;p style=&quot;text-align: justify;&quot;&gt;
	&lt;strong&gt;Methods:&lt;/strong&gt; Physicochemical properties and algal composition of the dam water were analyzed monthly to determine nutrient sources and environmental factors affecting cyanobacterial proliferation.
&lt;/p&gt;

&lt;p style=&quot;text-align: justify;&quot;&gt;
	&lt;strong&gt;Results:&lt;/strong&gt; The analysis revealed that the Timgad stream and Reboua valley are notable sources of nutrient enrichment. Elevated temperatures and high nutrient loads, particularly total phosphorus (TP), in Timgad dam water facilitate the proliferation of blue-green algae. Additionally, limited nitrogen content favors the dominance of nitrogen-fixing cyanobacteria such as Aphanizomenon and Oscillatoria. The study also highlights that the low flow rate and high nutrient load of the Timgad stream create favorable conditions for cyanobacterial growth. Conclusions: Nutrient inputs, temperature, and hydrological conditions significantly influence cyanobacterial blooms. Understanding these factors is crucial for implementing effective water management strategies to reduce algal proliferation and protect freshwater quality.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">2</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Belgaid, Nassima</style></author><author><style face="normal" font="default" size="100%">Menani, Mohamed-Redha</style></author><author><style face="normal" font="default" size="100%">Bouhidel, Kamel-Eddine</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Removal of basic textile dyes from water by natural and modified Algerian zeolite: kinetic, thermodynamic and equilibrium studies</style></title><secondary-title><style face="normal" font="default" size="100%">Military Technical Courier</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2025</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.5937/vojtehg73-56126</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">73</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	Algerian natural zeolite (denoted NZ) was modified by Hydrochloric Acid (denoted as HZ) and Sodium Hydroxide solution (denoted as NaZ). XRF results indicate that SiO2 is the predominant mineral for the three zeolites. XRD analysis revealed that NZ is primarly&amp;nbsp; composed of mordenite, followed by chabazite and smaller amounts of quartz.&amp;nbsp; MEB-EDX results showed slight variations in the Si and Al content for HZ and NaZ, without significant changes to the core structure of the zeolite. &amp;nbsp;This study aimed to assess the impact of acid and alkalin modification on the removal of two cationic textile dyes (BR&lt;sub&gt;46&lt;/sub&gt;&amp;nbsp;and BY&lt;sub&gt;13&lt;/sub&gt;) from aqueous solutions. Initial dye concentration, contact time and pH were studied in a batch system. The adsorption capacities of NZ, NaZ and HZ increased with longer contact times, higher initial concentrations, and elevated temperatures. The equilibrium state was rapidly reached and could be described using pseudo-second-order kinetic model. The Freundlish isotherm model provided a good fit for the adsorption process. Pourcentage removal was the highest for NaZ, achieving 97.62% for BR&lt;sub&gt;46&amp;nbsp;&lt;/sub&gt;and 98.97% for BY&lt;sub&gt;13&lt;/sub&gt;. The lowest removal percentages were noted at pH= 8 for HZ and pH=10 for NZ and NaZ. Adsorption process was spontaneous and endothermic.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">3</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>47</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Djenba, Samir</style></author><author><style face="normal" font="default" size="100%">Abdelhamid Khedidja</style></author><author><style face="normal" font="default" size="100%">Adjroud, Sonia</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Geoelectric Characterization of Bir Haddada Plain, NE Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">Conference of the Arabian Journal of Geosciences</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2024</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://link.springer.com/chapter/10.1007/978-3-031-43807-3_18?utm_source=researchgate.net&amp;utm_medium=article</style></url></web-urls></urls><publisher><style face="normal" font="default" size="100%"> Advances in Science, Technology &amp; Innovation ((ASTI))</style></publisher><pages><style face="normal" font="default" size="100%"> 89–92</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	The Bir Haddada Plain is located in eastern Algeria and is characterized by a semi-arid climate with low rainfall. The irrigation of this region's agricultural lands is almost assured by hundreds of wells that exploit the shallow aquifer. The strong pumping of the shallow aquifer triggered the latter's utter exhaustion. To resolve the irrigation water shortage, we need to explore the subsoils to find potentially exploitable aquifers more closely. The objective is the geoelectric characterization of this area and also the detection of underground water aquifers. The geophysical study by vertical electrical survey (VES) is more adequate because it allows identifying the conductive and resistant layers to the electric field. Exploration by VES was carried out with a spacing of the measuring electrodes ranging from&amp;nbsp;&lt;i&gt;AB&lt;/i&gt; = 100 to&amp;nbsp;&lt;i&gt;AB&lt;/i&gt; = 1000&amp;nbsp;m. The study of the results obtained indicates that the prospective zone is distinguished by a filling exceeding 300&amp;nbsp;m corresponding to the miopliocene formations. These formations are generally clays, conglomerates, and lacustrine limestones. In contrast, the low resistivity values seem to be related to the presence of conductive formations such as Miopliocene gypsum clays or to the presence of Triassic rocks linked to the contact of the bedrock. The maps of the apparent resistivity often show a network of different direction faults.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Khelifa, Mohammed</style></author><author><style face="normal" font="default" size="100%">Abdelhamid Khedidja</style></author><author><style face="normal" font="default" size="100%">Hamidi, Mansour</style></author><author><style face="normal" font="default" size="100%">Reghais, Azzeddine</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Water resources and physicochemical properties of the Mio-Pliocene aquifer complex in the M&amp;rsquo;leta Plain, Western Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">JOURNAL OF WATER AND LAND DEVELOPMENT </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2024</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.jwld.pl/files/2024-02-JWLD-02.pdf</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">61</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	The aquifers in the M’léta Plain are crucial for supplying drinking water and supporting industrial and agricultural water needs. However, they are facing a pollution risk and environmental degradation. The present study aims to assess the groundwater quality in the M’léta Plain, focusing on its physicochemical properties, statistics of the aquifer, pollution risks, and factors influencing the water mineralisation process. The analysis of 16 samples reveals that the water contains high levels of sulphates and chlorides, often accompanied by sodium, calcium, or magnesium. This suggests two distinct water types or facies: one characterised by sodium chloride or calcium chloride, and the other with calcic or sodic sulphate waters, sometimes including magnesium sulphate. These facies may be attributed to the influence of different formations at the outcrop. Statistical analyses reveal a strong correlation between electrical conductivity and the majority of chemical elements, indicating the impact of freshwater interacting with the underlying rock formations on mineralisation. Some results also show undersaturation of certain minerals. Furthermore, the study evaluates the water's suitability for irrigation in the M’léta Plain in accordance with Richards’ classification.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Rahma, Khadri</style></author><author><style face="normal" font="default" size="100%">Abdelhamid Khedidja</style></author><author><style face="normal" font="default" size="100%">Brinis, Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">IDENTIFICATION DE LA QUALITE DES EAUX DE LA NAPPE PROFONDE DE HAMMAM BRADAA, NORD EST DE GUELMA, ALGERIE</style></title><secondary-title><style face="normal" font="default" size="100%">Journée d’étude: Réutilisation des eaux usées, entre Outlook et réalité « RSOR-2024 » .  22,Avril , à l’université de Mostefa Ben Boulaïd – Batna2-  </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2024</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	L’aquifère de Hammam Bradaa se situe au Nord-Est de Guelma à l’Est algérien. Il fait partie du bassin versant de la Seybouse et plus précisément le sous bassin de la moyenne Seybouse qui couvre une superficie de 820 km2. Du point de vue géologique, les formations rencontrées sont en majeure partie carbonatées d’âge Crétacé, avec une couverture récente hétérogène (remplissage d’âge tertiaire). L’objectif est l’identification de la qualité des eaux par l’outil statistique pour ressortir les tendances et par conséquent les groupes chimiques qui caractérisent les eaux de la nappe profonde de Hammam Bradaa. Tout d’abord, l’estimation du coefficient de variation (CV%) indique que la majorité des mesures liées à chaque variable se rapprochent de la moyenne et ne montre pas une grande dispersion, contrairement aux mesures des nitrates qui présentent une grande dispersion autour de la moyenne, ceci peut être expliqué par l’utilisation sélective des engrais chimiques pour l’agriculture des terres exploitées. Par ailleurs, la corrélation simple (matrice de corrélation) et multiple (ACP et C.A.H), mettent en évidence des liens significatifs entre les ions issus de la dissolution des minéraux carbonatés (Mg et HCO3) ainsi que ceux résultants des minéraux évaporitiques (Na et Cl). La conductivité électrique n’indique pas une bonne corrélation avec les ions témoignant ainsi de la faible minéralisation des eaux étudiées. Nous remarquons la bonne concordance entre les résultats de l’analyse statistique et ceux de l’interprétation hydro chimique.&amp;nbsp;
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Bechkit, Mohamed-Amine</style></author><author><style face="normal" font="default" size="100%">Bouaicha, Foued</style></author><author><style face="normal" font="default" size="100%">Abdelhamid Khedidja</style></author><author><style face="normal" font="default" size="100%">Barkat, Ayoub</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Hydrogeological and geophysical characterization using electrical methods, case of Wadi El Nil-Jijel plain&amp;mdash;northern east of Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">Euro-Mediterranean Journal for Environmental Integration</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2024</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://link.springer.com/article/10.1007/s41207-024-00620-1?utm_source=researchgate.net&amp;utm_medium=article</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">10</style></volume><pages><style face="normal" font="default" size="100%">721–732</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	Several hydrologists recently stated that a large portion of the world’s population will face “water stress” in the coming years due to a variety of factors, including global mismanagement of fresh water near coastal plains, which is still being ignored and has become polluted. The alluvial plain of Wadi El Nil is one of these coastal plains, located in one of the wettest regions of Algeria with an annual rainfall rate of around 1000&amp;nbsp;mm. To quantify and qualify the water potential and to design a water management policy, a study was conducted using a complex of tools, such as geological, geophysical by electrical methods, hydro-climatic, and hydrogeological, to determine the lithology, geometry, and hydrodynamic characteristics of the aquifer.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Benzerouel, Zahra</style></author><author><style face="normal" font="default" size="100%">Krajewski, Marcin</style></author><author><style face="normal" font="default" size="100%">Slami, Rafika</style></author><author><style face="normal" font="default" size="100%">Salamon, Mariusz</style></author><author><style face="normal" font="default" size="100%">Bouchemla, Imad</style></author><author><style face="normal" font="default" size="100%">Zaidi, Mohamed-Amine</style></author><author><style face="normal" font="default" size="100%">Holcová, Katarína</style></author><author><style face="normal" font="default" size="100%">Benyoucef,  Madani</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Stratigraphy and sedimentology of the upper Cenomanian&amp;ndash;lower Coniacian in the Northern Aures Range (Algeria)</style></title><secondary-title><style face="normal" font="default" size="100%">Proceedings of the Geologists' Association</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2024</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.1016/j.pgeola.2024.03.003</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">135</style></volume><pages><style face="normal" font="default" size="100%"> 613-630</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	The stratigraphical features and palaeoenvironmental conditions of the upper Cenomanian–lower&amp;nbsp;Coniacian&amp;nbsp;carbonates from the northern part of the Aures Range are described for the first time. Four formations have been recognised, namely the Arris, Adahri, Yabous, and Bou Ouali, respectively. Planktonic foraminifera enable us to assign the upper part of the Arris Formation and the lower part of the Adahri Formation to the Middle–Upper&amp;nbsp;Cenomanian&amp;nbsp;(&lt;em&gt;Rotalipora&lt;/em&gt;&amp;nbsp;sp. cf.&amp;nbsp;&lt;em&gt;R. cushmani&lt;/em&gt;&amp;nbsp;Total Range Zone), the upper part of the Adahri Formation to the Cenomanian–Turonian Transition to the lower&amp;nbsp;Turonian&amp;nbsp;(&lt;em&gt;Whiteinella archaeocretacea&lt;/em&gt;&amp;nbsp;Partial Range Zone and&amp;nbsp;&lt;em&gt;Helvetoglobotruncana helvetica&lt;/em&gt;&amp;nbsp;Total-Range Zone, respectively), the lower member of the Yabous Formation to the middle&amp;nbsp;Turonian&amp;nbsp;(&lt;em&gt;Marginotruncana sigali&lt;/em&gt;&amp;nbsp;Partial Range Zone), and the upper member of the Yabous Formation to the upper Turonian (&lt;em&gt;Marginotruncana schneegansi&lt;/em&gt;&amp;nbsp;Partial Range Zone). The Turonian–Coniancian boundary was dated approximately. This&amp;nbsp;biozonation&amp;nbsp;enables a correlation with several upper Cenomanian–lower&amp;nbsp;Coniacian&amp;nbsp;sections outside Algeria, mainly within the Tethyan and Boreal domains. Based on the field data, and&amp;nbsp;microfacies&amp;nbsp;studies, the strata of these formations are arranged into eleven&amp;nbsp;microfacies&amp;nbsp;types (MT 1 to MT 11) that are described in terms of&amp;nbsp;depositional environments, and grouped into three main facies associations (FA 1, FA 2, and FA 3): (i) a deep shelf-basin facies zone; (ii) marginal sand shoals, an open-marine/restricted platform facies zone; and (iii) an outer platform and toe-of-slope/distal slope facies zone. Analysis of the&amp;nbsp;sequence stratigraphy&amp;nbsp;has allowed the recognition of three third-order&amp;nbsp;depositional sequences&amp;nbsp;grouped into two megasequences and correlated to a regional scale.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">5</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Salamon, Mariusz</style></author><author><style face="normal" font="default" size="100%">Slami, Rafika</style></author><author><style face="normal" font="default" size="100%">Benyoucef,  Madani</style></author><author><style face="normal" font="default" size="100%">Bruno Ferré</style></author><author><style face="normal" font="default" size="100%">Bouchemla, Imad</style></author><author><style face="normal" font="default" size="100%">Garah,  Abdelmoumen</style></author><author><style face="normal" font="default" size="100%">Krajewski, Marcin</style></author><author><style face="normal" font="default" size="100%">Jain, Sreepat</style></author><author><style face="normal" font="default" size="100%">Płachno, Bartosz J</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">A remarkable thiolliericrinid crinoid from the Aptian of northeastern Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2024</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.schweizerbart.de/papers/njgpa/detail/313/106063/A_remarkable_thiolliericrinid_crinoid_from_the_Apt?af=crossref</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">313</style></volume><pages><style face="normal" font="default" size="100%">99 - 109</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	The thiolliericrinids, although having a stem in the adult stage, are classified as comatulids (Comatulida) that are usually identified as stemless forms. They first appeared in the Bajocian (Middle Jurassic), and their last occurrence is noted in the Hauterivian (Early Cretaceous). Herein we report a thiolliericrinid crinoid from the Aptian of northern Africa (Algeria). This is the youngest thiolliericrinid crinoid ever recorded. Previously, the youngest thiolliericrinid (Thiolliericrinus) came from the Hauterivian (Lower Cretaceous) of France, Germany, Portugal, and Switzerland. This youngest thiolliericrinid has a smooth and irregular centrodorsal with no cirrus socket. The radials are irregular; some of them are variable in size and display no visible basal plates externally. The latter feature is typical of evolutionarily advanced Early Cretaceous thiolliericrinids (e.g., Heberticrinus or Loriolicrinus). Additionally, the present record is also the only representative of thiolliericrinids with a cup strongly oblique on the stem.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">1</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Touahri, Abdeldjebar</style></author><author><style face="normal" font="default" size="100%">Sahraoui, Salah</style></author><author><style face="normal" font="default" size="100%">Benmansour, Sana</style></author><author><style face="normal" font="default" size="100%">Hadjkouider, Mohammed</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Tectono-sedimentologic and lithostratigraphic control in Aures Region: Case study Djebel Metlili, Batna, Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">Geomatics, Landmanagement and Landscape</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2024</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.15576/gll/2024.2.08  </style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">2</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	This research delves into the geological features of the western section of the Aures Basin, with a primary focus on Djebel Metlili. The geological characteristics span Mesozoic and Tertiary deposits, ranging from the Triassic to the Quaternary epochs. Notably, the higher Cretaceous period stands out for its substantial carbonate-rich sequence. The research relied on geological maps, field observations, core samples, and laboratory analyses, including lithostratigraphic examinations (cross-section) and thin section. Structural features show that is formed by large regular folds of ENE-WSW or E-W direction. Anticlines and synclines are often affected by transverse accidents at the axes of the folds. In its northern part is located immediately south of the Belezma-Batna mountains. Structural analysis highlights significant tectonic disturbances, oriented in a northwest-southeast direction. A detailed lithostratigraphic examination reveals marly formations interspersed with limestone-rich layers containing Inoceramus. The southern part of Dj. Metlili, particularly the Santonian-Campanian series, unveils three distinct meso-transgressive sequences, linked to sea-level fluctuations associated with sedimentary basin subsidence. The studied area exhibits three distinct facies: one characterized by gray phosphate limestone with crisscrossed stratifications and agitated bioclastic sand, another featuring a mollusk-rich bioclastic limestone indicating a turbulent intertidal environment, and a third presenting a clay limestone bank with fine to medium grains and lumachels rich in oysters and gastropods. The associated grainstone texture in the microfacies suggests an internal platform environment marked by dissolution, bioturbation, and ferruginization. This comprehensive exploration provides valuable insights into the geological history of the region, significantly contributing to our understanding of its evolution over time.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Touansa, Rachid</style></author><author><style face="normal" font="default" size="100%">Cherif,  Ichrak</style></author><author><style face="normal" font="default" size="100%">Fouad Djaiz</style></author><author><style face="normal" font="default" size="100%">Sallouhi, Houaïda</style></author><author><style face="normal" font="default" size="100%">Mabrouk Boughdiri</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">High resolution calpionellid biozonation of Upper Tithonian reference sections in NE Algeria (Jebel Azreg, Aurès Range; Jebel Toumbaït, Aïn Yaghout Mounts): correlations and geodynamic implications</style></title><secondary-title><style face="normal" font="default" size="100%">Carbonates and Evaporites </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2024</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.1016/j.pgeola.2024.08.003</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">39</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	The stratigraphic problem of the Jurassic-Cretaceous boundary (JKB) is still the object of a warm international debate. Around this limit, the Upper Tithonian substage has been the subject of significant stratigraphic investigations throughout the Tethyan Realm areas. On the southern Tethys Margin of the Maghreb, our recent works in NE Algeria have revealed sections, where good Upper Jurassic outcrops are considered as promising for the definition of a Global Standard Section and Point (GSSP) for the Jurassic-Ctretaceous boundary. In this line of interest, a high resolution calpionellid biozonation of Upper Tithonian successions from two bed-by-bed sampled key sections in the Aurès (Jebel Azreg) and Aïn Yaghout Mounts (Jebel Toumbaït) of NE Algeria is proposed here for the first time. The Crassicollaria and Calpionella Zone limits, encasing two subzones and six stratigraphic horizons, are identified. Within these sections, calpionellid distribution and resulting biostratigraphic units fit the standards referred to for the Tethyan Realm. The identified marker bioevents and associations confirm the high biostratigraphic potential of calpionellids for the JKB definition in the North Africa Maghrebian Chains. Correlation transects reveal important thickness and facies variations interpreted as the result of a synsedimentary tectonic control implying NW–SE, E-W and NE-SW major faults that led to the individualization of a mozaic of highs and depressions where Upper Tithonian deposits onset. A proposed interpretative model replaces the Upper Tithonian study successions in their regional geodynamic context.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">63</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">KEMOUKH, Sami</style></author><author><style face="normal" font="default" size="100%">Athamenani, Ali</style></author><author><style face="normal" font="default" size="100%">Fouad Djaiz</style></author><author><style face="normal" font="default" size="100%">Halima Belalite</style></author><author><style face="normal" font="default" size="100%">Athamena, Ali</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">THE SALINITY ORIGIN OF THE SURFACE WATER IN THE WATERSHED DAM ZARDEZAS, EASTERN ALGERIA</style></title><secondary-title><style face="normal" font="default" size="100%">Proceedings of the Geologists' Association</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2024</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.1016/j.pgeola.2024.08.003</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">135</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	The deterioration of the physico-chemical quality of surface waters in the Algerian Northeast is caused by several factors. Our study aims to fill the knowledge gap on the control of hydro-chemical evolution of surface waters in wetlands. The main focus is on major elements in surface waters of the Skikda region in northeastern Algeria. To address this issue, we received 45 samples during the 09 campaigns conducted during the period of low and high water of the year 2015-2016, distributed over five points, namely the tributary Oued Khemakhem, Oued Bouadjeb, Oued Safsaf, reservoir of the Zerdazas dam and the downstream of the Zerdazas dam. First, we studied the variation of physical elements such as pH and EC. Then, using PCA and FA, we characterized the physicochemical properties of the water to demonstrate the relationship between&amp;nbsp;the elements and the factors controlling the distribution of the major elements and the heavy metals Pb2+, Fe2+ and Sr2+. The specific formula of the dominance of the different concentrations in the surface waters of the study area followed the sequence: Ca-Mg-Na-K and Cl-SO4-HCO3 from which a predominant specific facies emerges on 67% of the samples, is of the chloride and sulfate-calco Magnesian facies.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">5</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Khanfer, Soumia</style></author><author><style face="normal" font="default" size="100%">Fouad Djaiz</style></author><author><style face="normal" font="default" size="100%">Sanjuan, Josep</style></author><author><style face="normal" font="default" size="100%">Antonietto, Lucas-Silveira</style></author><author><style face="normal" font="default" size="100%">Bachir Lamouri</style></author><author><style face="normal" font="default" size="100%">Cherif, Amine</style></author><author><style face="normal" font="default" size="100%">El Asmi, Hicham</style></author><author><style face="normal" font="default" size="100%">Manche, Cameron</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Early Miocene lacustrine deposits from the Oued Tilatou Formation (Aurès Massif, Eastern Algeria): Sedimentology, micropalaeontology, and palaeoenvironmental implications</style></title><secondary-title><style face="normal" font="default" size="100%">Proceedings of the Geologists' Association</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2024</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.1016/j.pgeola.2024.08.003</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">135</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	Lacustrine depositional systems provide a valuable record of palaeoenvironmental conditions since they rely on a delicate balance between accommodation space and water-sediment supply controlled by tectonic activity and climatic conditions. This study presents new sedimentological and micropalaeontological information from the early&amp;nbsp;Miocene&amp;nbsp;lacustrine Oued Tilatou Formation, northeastern Algeria. Based on sedimentary facies and&amp;nbsp;microfossil&amp;nbsp;assemblages, the Oued Tilatou Formation (OTF) is divided into two discrete units, the Lower OTF and the Upper OTF. The Lower OTF is characterised by reddish clay-rich carbonate&amp;nbsp;mudstone&amp;nbsp;containing reworked foraminifera and&amp;nbsp;ostracods&amp;nbsp;interspersed by polymodal clast-supported conglomerates attributed to alluvial deposition. The Lower OTF was deposited under fluvial–palustrine conditions, marked by a notable terrigenous sediment influx. In contrast, the Upper OTF encompasses greenish charophyte-dominated (&lt;em&gt;Sphaerochara&lt;/em&gt;&amp;nbsp;sp.) carbonate&amp;nbsp;mudstone&amp;nbsp;interbedded with silty carbonate mudstone, and dolomitic wackestone containing charophyte thalli, several ostracod species, and&amp;nbsp;stromatolites. The dominant ostracod taxa within this interval are&amp;nbsp;&lt;em&gt;Mediocypris&lt;/em&gt;&amp;nbsp;sp. cf.&amp;nbsp;&lt;em&gt;M. candonaeformis&lt;/em&gt;, indicating freshwater–brackish water conditions. The transition in depositional facies from the Lower OTF to the Upper OTF is interpreted as reflecting changes in the environment from fluvial–palustrine to shallow water lacustrine with fluctuation in&amp;nbsp;freshwater input&amp;nbsp;during the&amp;nbsp;Burdigalian&amp;nbsp;(Early Miocene). This study provides new insights on the interplay between early&amp;nbsp;Miocene&amp;nbsp;climate conditions and the tectonic uplift of the Aurès Massif, and their implications for lacustrine palaeoenvironmental conditions.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">5</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">KEMOUKH, Sami</style></author><author><style face="normal" font="default" size="100%">Athamena, Ali</style></author><author><style face="normal" font="default" size="100%">DJAIZ, Foued</style></author><author><style face="normal" font="default" size="100%">Halima Belalite</style></author><author><style face="normal" font="default" size="100%">Athamena,Malika</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">THE SALINITY ORIGIN OF THE SURFACE WATER IN THE WATERSHED DAM ZARDEZAS, EASTERN ALGERIA</style></title><secondary-title><style face="normal" font="default" size="100%">Analele Universității din Oradea, Seria Geografie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2024</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.30892/auog.34104-911   </style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">34</style></volume><pages><style face="normal" font="default" size="100%">44-63</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">The deterioration of the physico-chemical quality of surface waters in the Algerian Northeast is caused by several factors. Our study aims to fill the knowledge gap on the control of hydro-chemical evolution of surface waters in wetlands. The main focus is on major elements in surface waters of the Skikda region in northeastern Algeria. To address this issue, we received 45 samples during the 09 campaigns conducted during the period of low and high water of the year 2015-2016, distributed over five points, namely the tributary Oued Khemakhem, Oued Bouadjeb, Oued Safsaf, reservoir of the Zerdazas dam and the downstream of the Zerdazas dam. First, we studied the variation of physical elements such as pH and EC. Then, using PCA and FA, we characterized the physicochemical properties of the water to demonstrate the relationship between&amp;nbsp;the elements and the factors controlling the distribution of the major elements and the heavy metals Pb2+, Fe2+ and Sr2+. The specific formula of the dominance of the different concentrations in the surface waters of the study area followed the sequence: Ca-Mg-Na-K and Cl-SO4-HCO3 from which a predominant specific facies emerges on 67% of the samples, is of the chloride and sulfate-calco Magnesian facies.</style></abstract><issue><style face="normal" font="default" size="100%">1</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Bezai, Abderrahim</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Reghais, Azzeddine</style></author><author><style face="normal" font="default" size="100%">Djenba, Samir</style></author><author><style face="normal" font="default" size="100%">Bouzid, Khadidja</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Hydrochemical analysis and groundwater quality assessment for irrigation in the Remila Plain, Khenchela, Northeast Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">Geomatics, Landmanagement and Landscape</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2024</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.15576/GLL/2024.3.03  </style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">3</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	Water resources are facing significant challenges in result of rapidly growing demand, deteriorating quality, and the effects of climate change. Today, water quantity and quality issues have become prevalent in various regions across the globe, affecting both northern and southern territories. Among the sectors reliant on this resource, irrigation stands out as the largest consumer of water. When surface water becomes inaccessible due to insufficient precipitation or other factors, the use of groundwater becomes the only viable alternative for irrigation. The Remila Plain (Khenchela) is located in an endorean watershed in northeastern Algeria and extends over 250 km2 in a synclinal basin filled with water from the Mio-Plio Quaternary - the main aquifer of the region, widely used for irrigation. The aim of this work is to study the hydrochemistry of these waters, as well as the evolution of mineralisation, the identification of the origin of the chemistry, and the suitability of these waters for irrigation. Initial results indicate an evolution of mineralisation in the direction of groundwater flow, with electrical conductivity values varying between 1000μS/cm in the recharge zones, and 2700μS/cm at the outlet. This mineralisation is mainly due to the dissolution of evaporitic minerals and the alteration of silicates. In addition, the various water quality indices used indicate that the water can be used for irrigation without major risk to plants and soils.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Boudjema,  Abderrezak</style></author><author><style face="normal" font="default" size="100%">Guettaia, Sabrine</style></author><author><style face="normal" font="default" size="100%">Derdour, Abdessamed</style></author><author><style face="normal" font="default" size="100%">Brinis, Nafaa</style></author><author><style face="normal" font="default" size="100%">Almaliki, Abdulrazak H</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Statistical approaches for the identification of the origin mineralization groundwaters: case of the Naama Region, Far West-Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">EARTH SCIENCES  RESEARCH JOURNAL</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2024</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://bucketvirtualpro-private.s3.amazonaws.com/files-bv/20241213/281635.pdf</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">289</style></volume><pages><style face="normal" font="default" size="100%">387 - 395</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	Understanding the processes controlling groundwater mineralization is critical for preserving its quality and ensuring sustainable resource management, especially in regions like Naama, Algeria, which rely exclusively on groundwater. T his resource faces severe overexploitation and high salinity due to climatic factors and increasing industrial, agricul tural, and domestic demands, posing significant challenges to its long-term usability. Hydrochemical analyses, inclu ding graphical methods and multivariate statistical tools, were employed to investigate the groundwater chemistry and mechanisms influencing mineralization in the Naama region. The results revealed a relatively homogeneous distribu tion of groundwater samples, categorized into three hydrochemical groups. These groups are primarily dominated by calcium and magnesium chloride and sulfate waters, influenced by the geological characteristics of the region, such as gypsum-saline formations of the Upper Cretaceous and Triassic clay-gypsum-saline diapirs, and further impacted by inverse ion exchange processes. Group 1 is characterized by higher proportions of calcium and magnesium bicarbo nate waters due to the dominance of carbonate formations from the Early Jurassic or Miocene, benefiting from more dynamic recharge zones. Groups 2 and 3 exhibit similar chemical compositions, but Group 3 is distinct for its restricted recharge zones and carbonate formations, leading to the emergence of calcium and magnesium bicarbonate waters. Recharge areas associated with carbonate formations were also vulnerable to anthropogenic pollution. These findings highlight the importance of implementing strict protection measures for sensitive recharge zones to ensure the preser vation of this vital resource in the face of increasing environmental and human pressures.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">4</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Khelifa, Mohammed</style></author><author><style face="normal" font="default" size="100%">Abdelhamid Khedidja</style></author><author><style face="normal" font="default" size="100%">Hamidi, Mansour</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Assessment of the vulnerability to pollution of shallow aquifers, case study of the plain of M&amp;#39;léta NW Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">Geomatics, Natural Hazards and Risk </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2023</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.1080/19475705.2023.2184671</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">14</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	The increasing pollution of groundwater resulting from population growth and the evolution of agro-industrial activities have become a poses threat to the socio-economic development of the western Algerian region. This study aims to assess the vulnerability and pollution risks of the plain of M’léta and factors that control the transfer of pollutants, and prepare a report on the basis of a thematic map relating to the DRASTIC and DRIST method which is an improvement of the DRASTIC method. Cartographic analysis of the results of the two methods showed the M'léta Plain is characterized by low to high vulnerability, of which almost the entire plain is characterized by low to medium vulnerability. There was 53.75% for the DRASTIC method, while the second rate was 53.06% for the DRIST method, while the high vulnerability is recorded in the northern part of the plain, which swallowed 46.93% for the DRASTIC method, and for the DRIST method, it amounted to 46.24%. The result of the research shows that the preparation of an objective map avoids many risks of pollution and gives possible solutions for any future decision, and that both methods express approximately the same areas with regard to the degree of vulnerability.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">1</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Khadri, Rahma</style></author><author><style face="normal" font="default" size="100%">Abdelhamid Khedidja</style></author><author><style face="normal" font="default" size="100%">Brinis, Nafaa</style></author><author><style face="normal" font="default" size="100%">Kharroubi, Maha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Geophysical and geological contribution to determining the neriticlimestone aquifer structure of Hammam Bradaa &amp;ndash; El Fedjoudj(Seybouse medium), Northeastern Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">Mining of Mineral Deposits</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2023</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.researchgate.net/publication/369638762_Geophysical_and_geological_contribution_to_determining_the_neritic_limestone_aquifer_structure_of_Hammam_Bradaa_-El_Fedjoudj_Seybouse_medium_Northeastern_Algeria</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">17</style></volume><pages><style face="normal" font="default" size="100%">67-73</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;
	&lt;strong&gt;Purpose.&lt;/strong&gt; The neritic aquifer that extends between Hammam Bradaa and El Fedjoudj, despite its faulted and in places karstified structure, due toits capacity and lateral extension represent a strategic resource for the region. Its waters are used for drinking water supply in the neighboring towns: Heliopolis, Guelaat Bousbaa, Nechmaya and El Fedjoudj, as well as in part of the Annaba wilaya. These neritic limestones outcrop at Djebel Debagh and Bouzitoune.
&lt;/p&gt;

&lt;p&gt;
	&lt;strong&gt;Methods.&lt;/strong&gt; In order to better study the potential of this aquifer, it is essential to identify its geometry and structure by ana-lyzing the geological data, mechanical drilling data and geophysical data analysis through an electrical survey campaign.Findings. The main results indicate that the study area has identified two important aquifer formations: a formation in the Mio-Plio-Quaternary alluvium consisting of clays, marls, gravel and sand; the second is a deep carbonate aquifer composed of fissured and karstified neritic limestone of the Cretaceous age of variable depth ranging within 50 and 350 m.
&lt;/p&gt;

&lt;p&gt;
	&lt;strong&gt;Originality.&lt;/strong&gt; The originality of the study is in the fact that the studied area is characterized by the presence of thick, frac-tured and karstified carbonate formations, which are intensively tectonized and have significant aquifer potential.
&lt;/p&gt;

&lt;p&gt;
	&lt;strong&gt;Practical implications.&lt;/strong&gt; The correlation of geological data with geophysical data made it possible to conclude that the stu-died area is a sedimentary basin bounded by faults predominantly oriented to the south-west and north-east, forming a highly fractured unit consisting of horsts and grabens. The significant water potential reservoir is formed essentially by carbonate geological formations, highly fractured with the presence of karst forms represented by resistant horizons.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">1</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Dib, Imane</style></author><author><style face="normal" font="default" size="100%">Abdelhamid Khedidja</style></author><author><style face="normal" font="default" size="100%">Chettah, Wahid</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Multivariate statistical analysis of the alluvial aquifer of Tadjenanet-Chelghoum Laid (Eastern Algeria)</style></title><secondary-title><style face="normal" font="default" size="100%">Acque Sotterranee-Italian Journal of Groundwater </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2023</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.7343/as-2023-643</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">12</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	The region of Chelghoum Laid - Tadjenanet is located in eastern Algeria, in the high plains. This area is characterized by a varied age (Mio-Plio-Quaternary) formations and the human demand is answered by the groundwater hosted into the superficial aquifer of the Mio-Plio-Quaternary formations. However, the overexploitation of this aquifer leads to a drop in the piezometric surface and an increase in salinity. of this aquifer leads to a drop in the piezometric surface and an increase in the salinity of the water. A hydrochemical study using characteristic ratios and statistical tools such as principal component analysis and hierarchical ascending classification, was performed using 28 water samples. Chemical analyzes show that the waters of this aquifer are of the calcium bicarbonate type on the limits of the study area, and calcium sulphate to sodium chloride in the centre. The spatial evolution of chemical water facies is explained by the phenomenon of dissolution and ion exchange between the alkali metals and alkaline earth metals coinciding with the West-East flow direction. The application of the various tools shows that the aquifer is recharged by precipitation at the plains border, where the water acquires its original mineralization from the carbonate formations, and becomes more mineralized in chlorides, sodium and sulphates concentrations in contact with the salt-bearing terrigenous formations of the Mio-Plio-Quaternary. The salinization of the waters seems to be mainly due to the dissolution of gypsum, halite and epsomite. The application of the ascending hierarchical classification and the principal component analysis shows the existence of two groups of water whose salinity increases from the borders towards the center of the plain following the main flow direction.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">2</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Abdelhamid Khedidja</style></author><author><style face="normal" font="default" size="100%">Drias, Tarek</style></author><author><style face="normal" font="default" size="100%">Reghais, Azzeddine</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Assessment of groundwater vulnerability to pollution using DRASTIC and the SI methods: case of the alluvial aquifer in Tadjenanet-Chelghoum laid (East Algeria)</style></title><secondary-title><style face="normal" font="default" size="100%">Acque Sotterranee-Italian Journal of Groundwater</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2023</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%"> https://doi.org/10.7343/as-2023-644</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">12</style></volume><pages><style face="normal" font="default" size="100%">37-47</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	The region of Chelghoum Laid - Tadjenanet is located in the east of Algeria in the high southern plains of Setif, characterized by a highly vulnerable shallow alluvial aquifer. The vulnerability of groundwater to pollutants is a relative concept, not measurable or dimensional. The nature, quality, and reliability of used data used have a major impact on the correctness of its assessment. Its classification is usually based on the estimation of many more or less essential factors, such as the characteristics of soil and unsaturated zone, the saturated zone, the recharge , the topography and the hydraulic conductivity. The vulnerability of the aquifer to pollution was investigated using two intrinsic vulnerability methods: DRASTIC and susceptibility index (SI). SI method is an adaptation of the DRASTIC specifically design for nitrate-based pollution. The parameters used as input data are, among others, the depth of the groundwater, the soil type, the topographic slope and the groundwater recharge. The validity of the two methods for assessing the vulnerability to nitrates was established by comparing the distribution of these elements in groundwater with the distribution of the various vulnerability classes. GIS techniques were used to implement these methods. Vulnerability maps created using the DRASTIC and SI method’s depict the potential for pollutants to penetrate and spread in these locations depending on the terrain encountered on the surface and the depth of the aquifer. The comparison revealed that the SI technique is the most accurate in the studied alluvial aquifer. The establishment of the pollution vulnerability map highlighted an area of great vulnerability in the center of the plain, reflected by the fragility of the soil and the shallow depth of the water. While the average vulnerability areas are in the center, and east at the periphery of Wadi Rhumel, the rest of the field is slightly vulnerable. The vulnerability and contamination risk maps created for this study are valuable tools for environmental planning and can be used for predictive management of groundwater resources. This case study suggests that the approach may be applicable to other areas as part of efforts to target groundwater management efforts.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">2</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Khadri, Rahma</style></author><author><style face="normal" font="default" size="100%">Abdelhamid Khedidja</style></author><author><style face="normal" font="default" size="100%">Boubaya, Djamel</style></author><author><style face="normal" font="default" size="100%">Brinis, Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Integrated gravity and resistivity investigations of the deep Hammam Bradaa aquifer, Northeast Algeria: Implications for groundwater exploration</style></title><secondary-title><style face="normal" font="default" size="100%">Journal of African Earth Sciences</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2023</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.1016/j.jafrearsci.2023.105013</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">205</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	Recently, the Guelma region, located northeast of Algeria, has been facing an unusual water shortage. To bypass this situation, a geophysical study using gravity and resistivity has been initiated to enhance the understanding of the&amp;nbsp;geology&amp;nbsp;and&amp;nbsp;hydrogeology&amp;nbsp;of the deep structures of the study area. In order to accomplish this, a residual&amp;nbsp;gravity anomaly&amp;nbsp;map has been constructed by removing from the&amp;nbsp;Bouguer anomaly&amp;nbsp;map a regional gravity gradient using the upward continuation technique. For the purpose of validating the Vertical Electrical Sounding(VES) interpretation, two soundings were conducted near boreholes with known&amp;nbsp;lithology. The Hammam Bradaa deep aquifer of the Guelma region is composed of limestones that belong to the Constantine neritic domain. The Constantine neritic domain is covered by thrust nappes and outcrops in some places of the study area as tectonic windows. The exact geometry such as depth and lateral extent of the aquifer are not well known. Since limestones are characterized by high densities and resistivities relative to the host rock, the combining of gravity and VES was able to accurately map their extension among the other lithologies composing the geological section. Multiscale edge detection of gravity data known as &quot;worms&quot; made it possible to highlight the principal lineaments across the study area which may contribute to the recharge of the Hammam Bradaa aquifer. The 3D Gravity inversion enabled the mapping of the spatial configuration of limestones that are characterized by positive gravity contrast relative to the host rocks. A vertical density slice extracted from the 3D gravity inversion, running from north to south, reveals a significant thickness of limestone beneath Hammam Bradaa which suggests a strong potential for groundwater resources. The geo-electric section, constructed from the interpretation of VES data and calibrated with well&amp;nbsp;lithology, enabled the mapping of the depth to the top of limestone beneath conductive alluvium and marls.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Abdelhamid Khedidja</style></author><author><style face="normal" font="default" size="100%">Drias, Tarek</style></author><author><style face="normal" font="default" size="100%">Reghais, Azzeddine</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Assessment of groundwater vulnerability to pollution using DRASTIC and the SI methods: case of the alluvial aquifer in Tadjenanet- Chelghoum laid (East Algeria)</style></title><secondary-title><style face="normal" font="default" size="100%">Acque Sotterranee - Italian Journal of Groundwater</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2023</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.academia.edu/download/105087925/496.pdf</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">12</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	The region of Chelghoum Laid - Tadjenanet is located in the east of Algeria in the high southern plains of Setif, characterized by a highly vulnerable shallow alluvial aquifer. The vulnerability of groundwater to pollutants is a relative concept, not measurable or dimensional. The nature, quality, and reliability of used data used have a major impact on the correctness of its assessment. Its classification is usually based on the estimation of many more or less essential factors, such as the characteristics of soil and unsaturated zone, the saturated zone, the recharge , the topography and the hydraulic conductivity. The vulnerability of the aquifer to pollution was investigated using two intrinsic vulnerability methods: DRASTIC and susceptibility index (SI). SI method is an adaptation of the DRASTIC specifically design for nitrate-based pollution. The parameters used as input data are, among others, the depth of the groundwater, the soil type, the topographic slope and the groundwater recharge. The validity of the two methods for assessing the vulnerability to nitrates was established by comparing the distribution of these elements in groundwater with the distribution of the various vulnerability classes. GIS techniques were used to implement these methods. Vulnerability maps created using the DRASTIC and SI method’s depict the potential for pollutants to penetrate and spread in these locations depending on the terrain encountered on the surface and the depth of the aquifer. The comparison revealed that the SI technique is the most accurate in the studied alluvial aquifer. The establishment of the pollution vulnerability map highlighted an area of great vulnerability in the center of the plain, reflected by the fragility of the soil and the shallow depth of the water. While the average vulnerability areas are in the center, and east at the periphery of Wadi Rhumel, the rest of the field is slightly vulnerable. The vulnerability and contamination risk maps created for this study are valuable tools for environmental planning and can be used for predictive management of groundwater resources. This case study suggests that the approach may be applicable to other areas as part of efforts to target groundwater management efforts.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">2</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Boumaiza, Lamine</style></author><author><style face="normal" font="default" size="100%">Chesnaux, Romain</style></author><author><style face="normal" font="default" size="100%">Drias, Tarek</style></author><author><style face="normal" font="default" size="100%">Stotler, Randy-L</style></author><author><style face="normal" font="default" size="100%">Skrzypek, Grzegorz</style></author><author><style face="normal" font="default" size="100%">Gillon, Marina</style></author><author><style face="normal" font="default" size="100%">Wanke,  Heike</style></author><author><style face="normal" font="default" size="100%">Johannesson, Karen-H</style></author><author><style face="normal" font="default" size="100%">Stumpp, Christine</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Vadose zone water stable isotope profiles for assessing groundwater recharge: Sensitivity to seasonal soil sampling</style></title><secondary-title><style face="normal" font="default" size="100%">Journal of Hydrology</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2023</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.1016/j.jhydrol.2023.130291</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">626</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	Groundwater recharge is widely recognized as being the most important parameter for the sustainable management of water resources. In semiarid environments,&amp;nbsp;groundwater recharge&amp;nbsp;can be quantified using the piston displacement method (PDM). From a single&amp;nbsp;soil sampling&amp;nbsp;campaign, the PDM relies on linking the deeper vadose zone soil&amp;nbsp;pore water&amp;nbsp;stable isotope composition (&lt;em&gt;δ&lt;/em&gt;&lt;sup&gt;2&lt;/sup&gt;H&lt;sub&gt;H2O&lt;/sub&gt;&amp;nbsp;and&amp;nbsp;&lt;em&gt;δ&lt;/em&gt;&lt;sup&gt;18&lt;/sup&gt;O&lt;sub&gt;H2O&lt;/sub&gt;) to the local meteoric water line (LMWL). However, the isotopic composition of precipitation changes seasonally, influencing the water isotope composition of the vadose zone over time. Thus, it is important to test whether the PDM is sensitive to seasonal soil sampling and whether the assessed recharge rate is independent of the time of sampling. This study investigates the effect of seasonal soil sampling on the distribution of vadose zone stable isotope composition to determine whether the sampling time influences the estimate of recharge rate from PDM. Soil samples were obtained along vertical profiles through the vadose zone in a semiarid region during the spring, summer, and autumn seasons. Specifically, the&amp;nbsp;&lt;em&gt;δ&lt;/em&gt;&lt;sup&gt;2&lt;/sup&gt;H&lt;sub&gt;H2O&lt;/sub&gt;&amp;nbsp;and&amp;nbsp;&lt;em&gt;δ&lt;/em&gt;&lt;sup&gt;18&lt;/sup&gt;O&lt;sub&gt;H2O&lt;/sub&gt;&amp;nbsp;of the soil pore water were determined along vertical profiles, and the PDM was applied to quantify the annual recharge. The&amp;nbsp;&lt;em&gt;δ&lt;/em&gt;&lt;sup&gt;2&lt;/sup&gt;H&lt;sub&gt;H2O&lt;/sub&gt;&amp;nbsp;and&amp;nbsp;&lt;em&gt;δ&lt;/em&gt;&lt;sup&gt;18&lt;/sup&gt;O&lt;sub&gt;H2O&lt;/sub&gt;&amp;nbsp;values range from&amp;nbsp;−7.3 to&amp;nbsp;−3.5&amp;nbsp;‰ and from&amp;nbsp;−54.4 to&amp;nbsp;+7.41&amp;nbsp;‰, respectively, and plot along a continuum with a slope less than the LMWL. Samples from deeper in the vadose zone profile had distinct ranges in isotopic composition between the three soil sampling campaigns, with isotopic composition of spring sampling dominated by lower values and those from autumn with higher values. Despite these differences, the resulting annual recharge rates from the different sampling campaigns are comparable (1.5 to 2&amp;nbsp;% of annual precipitation). Even though the pore water isotopic composition changed over time, the shift between the deeper vadose zone isotopic compositions and the LMWL remained relatively constant, leading to a similar recharge estimate over time. Therefore, the PDM-based recharge assessment in the tested semiarid environment is independent of the sampling time, which indicates that sampling for assessing groundwater recharge can be undertaken during any season.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Hibi, Amal</style></author><author><style face="normal" font="default" size="100%">Drias, Tarek</style></author><author><style face="normal" font="default" size="100%">Gouaidia, Layachi</style></author><author><style face="normal" font="default" size="100%">Guefaifia, Omar</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution of gravimetry to the study of the structure of the Télidjene Basin (Eastern Algeria): Hydrogeological implications</style></title><secondary-title><style face="normal" font="default" size="100%">Seventh International Conference on Engineering Geophysics, 16–19 October </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2023</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.1190/iceg2023-015.1</style></url></web-urls></urls><pub-location><style face="normal" font="default" size="100%">Al Ain, UAE</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	This paper presents a gravimetric study aimed at analyzing the geological structure and hydrogeological potential of the Télidjene basin in eastern Algeria. The data used are based on the EGM2012 gravimetric model and have been corrected using the International Gravimetric Bureau (BGI). Bouguer anomalies were calculated using spherical harmonic coefficients and underwent topographic corrections. The upward continuation method was used to attenuate shortwavelength anomalies and separate regional and residual components. Spectral analysis allowed for determining the average depths of geological formations. The results obtained from the gravimetric processing provided valuable information on the geological structure and hydrogeological potential of the study area and enabled the creation of a structural map illustrating the fault system responsible for the structuring of the study area. This map serves as a highly useful document for guiding future hydrogeological research in the study area.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Hammadi, Aziza</style></author><author><style face="normal" font="default" size="100%">Brinis, Nafaa</style></author><author><style face="normal" font="default" size="100%">Djidel, Mohamed</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Hydrodynamic Characteristics of the &amp;ldquo;Complex Terminal&amp;rdquo; aquifer in the Region of Oued Righ North (Algerian Sahara)</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2023</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.aljest.net/index.php/aljest/article/view/879</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">9</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	&lt;em&gt;Accessibility of fresh water, the nature's gift wheels the foremost part of the world economy. The sufficient supplies of water are essential for agriculture, human intake, industry as well as regeneration.&amp;nbsp;&lt;/em&gt;&lt;em&gt;The Oued Righ region is located in Algeria's South-East, specifically in the North-East of the Sahara, on the Northern edge of the Grand Erg Oriental and the Southern border of the Aures massif. This area appears as a lower Sahara synclinal basin and is part of a broad North-South trending ditch.&lt;/em&gt;
&lt;/p&gt;

&lt;p style=&quot;text-align: justify;&quot;&gt;
	&lt;em&gt;It is famous for its date palms, the development of the date culture in this region is attributed not only to the population’s efforts, but above all to the particular climatic conditions, the favorable soil characteristics and the existence of significant groundwater. The aim of this study is to understand the&amp;nbsp;results obtained from using different approaches of water&amp;nbsp;&amp;nbsp; hydrodynamics in&amp;nbsp;&amp;nbsp; the Complex Terminal aquifer.&amp;nbsp;The aquifer’s hydrodynamic characterization was carried out using hydrodynamic parameters and piezometry. As a result, the transmissivity and permeability obtained data using traditional Cooper-Jacob method&amp;nbsp;showed&amp;nbsp;that the flow capacities of the aquifer environment and the productivities of the structures are important in the studied zone where, the highest value of transmissivity equal&amp;nbsp;2.36× 10&lt;sup&gt;2-&lt;/sup&gt;m&lt;sup&gt;2&lt;/sup&gt;/s&lt;sup&gt;&amp;nbsp;&lt;/sup&gt;is found in the central part of the study area in El-Meghair. The establishment of piezometric maps reveals a flow direction oriented toward the chott.&lt;/em&gt;
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">2</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Benyoucef,  Madani</style></author><author><style face="normal" font="default" size="100%">Salamon, Mariusz</style></author><author><style face="normal" font="default" size="100%">Bruno Ferré</style></author><author><style face="normal" font="default" size="100%">Bouchemla, Imad</style></author><author><style face="normal" font="default" size="100%">Slami, Rafika</style></author><author><style face="normal" font="default" size="100%">Veselská, Martina-Kočová</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Stratigraphy, palaeontology and sedimentology of the Upper Cretaceous of northern Tademait (Sahara, Algeria)</style></title><secondary-title><style face="normal" font="default" size="100%">Cretaceous Research</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2023</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.1016/j.cretres.2023.105547</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">149</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	Thorough sedimentological and palaeontological analyses of four expanded&amp;nbsp;Upper Cretaceous&amp;nbsp;sections in northern Tademait had allowed us to address and reconsider the stratigraphical framework of the so-called ‘Continental Intercalary’ and ‘Hamada series’ in this remote Saharan area. These four sections (i.e., Meguidene, Gara Samani, Oued El Mezaourou-Gour Louazouaza, and El Menia) document&amp;nbsp;Upper Cretaceous&amp;nbsp;strata overlying post-Palaeozoic substrata and ranging from the clastic Gara Samani Formation (of supposed early&amp;nbsp;Cenomanian&amp;nbsp;age), through the El Golea Clays (lower–middle Cenomanian), the Gour Louazouaza Formation (lowermost upper&amp;nbsp;Cenomanian, with the Oued El Mezaourou Limestone Member ranging from the&amp;nbsp;&lt;em&gt;Neolobites vibrayeanus&lt;/em&gt;&amp;nbsp;to the&amp;nbsp;&lt;em&gt;Vascoceras gamai&lt;/em&gt;&amp;nbsp;ammo&lt;a href=&quot;https://www.sciencedirect.com/topics/earth-and-planetary-sciences/ammonite&quot;&gt;nite&lt;/a&gt;&amp;nbsp;zones of the uppermost Cenomanian, and the Marls of Gara Mta El Mar Member of the&amp;nbsp;&lt;em&gt;Choffaticeras sinaiticum&lt;/em&gt;&amp;nbsp;ammonite&amp;nbsp;Zone in the lower, but not lowermost, Turonian), to the Ain El-Hadjaj Formation (of alleged&amp;nbsp;Campanian&amp;nbsp;age). Most efforts have concentrated on the ‘mid’-Cretaceous deposits that yield vertebrates and diversified ammonite and macrofossil assemblages. In spite of these improved correlations, further bio-chronostratigraphical data are needed in order to constrain the stratigraphical gap within the Gour Louazouaza Formation at the Cenomanian–Turonian boundary (C/TB) better. The succession studied can be correlated with other similar-aged sections in&amp;nbsp;North Africa&amp;nbsp;and illustrates the development of braided fluvial and aeolian dune-interdune environments followed by a ramp depositional system in response to the early&amp;nbsp;Late Cretaceous&amp;nbsp;second-order&amp;nbsp;sea level rise&amp;nbsp;along the southern margin of the&amp;nbsp;Tethys.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Benmansour, Sana</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Laffitteina from the Maastrichtian-Thanetian shallow marine carbonates of the Aurès Basin (Northeastern Algeria): microfacies and stratigraphic distribution</style></title><secondary-title><style face="normal" font="default" size="100%">Boletín de la Sociedad Geológica Mexicana</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2023</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.scielo.org.mx/scielo.php?pid=S1405-33222023000100001&amp;script=sci_arttext&amp;tlng=en</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">75</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	The Maastrichtian-Thanetian Ncham Member of the Aurès Basin in northeastern Algeria contains variably lenticular microfossils, which are defined as Laffitteina genera. It is a large benthic foraminifera, studied from three stratigraphic sections. The systematic study of Laffitteina led identification of nine species, four of which, Laffitteina marsicana, L. aff. mengaudi, L. monodi and L. erki were recorded for the first time in the study area. Various species of Laffitteina were used as index fossils to recognize the K/Pg transition in the Aurès Basin. The last occurrence of L. oztuerki marks the end of the Maastrichtian, which was found in association with Omphalocyclus macroporus (Lamarck) in the upper Maastrichtian. The first occurrence of L. erki marks the Thanetian age, while the Danian and Selandian deposits are missing in the field after a general emersion in the early Paleocene, despite the absence of a visible non unconformity. It could therefore be proposed that the K/Pg transition may occurs in the last 10 m of the Ncham Member. Concerning the paleoenvironment, Laffitteina is considered as a resistant foraminifera and thrives in meso-to eutrophic environments (lagoon). Microfacies data from the Upper Cretaceous-Lower Paleogene limestones of the Aurès Basin suggests a carbonate platform with shallowing-up sequential organization, mainly controlled by fluctuations in sea-level.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">1</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Bentaher, Fahima</style></author><author><style face="normal" font="default" size="100%">DEFAFLIA , Nabil</style></author><author><style face="normal" font="default" size="100%">Benmansour, Sana</style></author><author><style face="normal" font="default" size="100%">Fehdi, Chamseddine</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Investigation of litho-biostratigraphic characteristics and geographical distribution of Coniacian-Santonian formations: a case study in the Aures Mountains, eastern Saharan Atlas, Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">Geomatics, Landmanagement and Landscape </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2023</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.15576/gll/2023.3.73</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">3</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	The Coniacian-Santonian series in the Aures Mountains of northeastern Algeria is characterized by marly-dominated sedimentation processes. This study aims to comprehensively investigate this series by combining lithostratigraphic and biostratigraphic data. The unique paleogeographic position of the Aures basin supports the co-occurrence of diverse paleontological contents in the Upper Cretaceous sediments. The methodology employed in this study includes a detailed bio-lithostratigraphic analysis to subdivide the Coniacian-Santonian series into two distinct sets. The first set comprises alternating marl-limestone units that exhibit a high fossil concentration from the Coniacian age, while the second set mainly consists of marly sediments corresponding to the Santonian age. The results obtained from this study highlight the geographical distribution of litho-biostratigraphic characteristics and reveal the presence of two formations. The lower formation is characterized by carbonated marls intercalated with limestone banks, containing fossils of Peroniceras (Tissotia tissoto) from the Coniacian age. Meanwhile, the upper formation is predominantly marly and indicates the Santonian age by displaying fossils of Palcenticeras polypsis. Furthermore, a biostratigraphic analysis focused on foraminifers allows for the subdivision of the Coniacian-Santonian series in the Aures Mountains into three distinct biozones. The first biozone corresponds to the lower Coniacian age and is identified by the presence of Dicarinella primitiva. The second biozone represents the middle to upper coniacian age and contains Dicarinella concavata fossils. Finally, the third biozone, belonging to the Santonian age, is marked by the occurrence of Dicarinella asymetrica. The boundary between the Coniacian and Santonian series in the Aures Mountains is characterized by the first appearance of Dicarinella asymetrica and Palcenticeras polypsis species. This multidisciplinary study provides valuable insights into the litho-biostratigraphic characteristics and geographical distribution of the Coniacian-Santonian series in the Aures Mountains. The findings make a significant contribution to a better understanding of sedimentary processes and the paleontological content within this region during the Upper Cretaceous period.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Benmansour, Sana</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Upper Cretaceous bivalves from Northeastern Algeria: Description and paleobiogeography</style></title><secondary-title><style face="normal" font="default" size="100%">Journal of African Earth Sciences</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2023</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.1016/j.jafrearsci.2022.104787</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">198</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	The systematic study of bivalves collected from the Cenomanian-Turonian succession of the Bellezma-Batna Mountains (northeastern Algeria) led identification of nine species belonging to eight genera, three of which,&amp;nbsp;&lt;em&gt;Nicaisolopha nicaisei&lt;/em&gt;&amp;nbsp;(Coquand)&lt;em&gt;, Pterotrigonia&lt;/em&gt;&amp;nbsp;(&lt;em&gt;Scabrotrigonia&lt;/em&gt;)&amp;nbsp;&lt;em&gt;scabra&lt;/em&gt;&amp;nbsp;(Lamarck), and&amp;nbsp;&lt;em&gt;Agelasina plenodonta&lt;/em&gt;&amp;nbsp;Riedel, were recorded for the first time from the study area. Particular attention was paid to the rudist fauna, including&amp;nbsp;&lt;em&gt;Vaccinites praegiganteus&lt;/em&gt;&amp;nbsp;(Toucas),&amp;nbsp;&lt;em&gt;Vaccinites rousseli&lt;/em&gt;&amp;nbsp;(Douvillé), and&amp;nbsp;&lt;em&gt;Sauvagesia nicaisei&lt;/em&gt;&amp;nbsp;(Coquand), occurring in very large numbers within composite&amp;nbsp;biostromes&amp;nbsp;(5 to 10 m-thick) composed of both hippuritids and radiolitids. A distribution map of Cenomanian-Turonian bivalves is established based on data from Algeria and other localities.
&lt;/p&gt;

&lt;p style=&quot;text-align: justify;&quot;&gt;
	The map shows that the most bivalve genera are widely distributed and some of them are probably cosmopolitan. They are present in&amp;nbsp;northern Africa, Middle East, south and northern Europe,&amp;nbsp;western Africa, and South America, with some taxa are also known from the south-eastern coast of Africa (Madagascar and South Africa) and India.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Benmansour, Sana</style></author><author><style face="normal" font="default" size="100%">Kherchouche, Rima</style></author><author><style face="normal" font="default" size="100%">Bouterfaa, Abdellatif</style></author><author><style face="normal" font="default" size="100%">Garah,  Abdelmoumen</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Quantitative analysis and paleoenvironmental reconstruction of the middle Cenomanian deposits from southern Bellezma-Batna Mountains (northeastern Algeria)</style></title><secondary-title><style face="normal" font="default" size="100%">A Journal of the Brazilian Society of Paleontology</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2023</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://d1wqtxts1xzle7.cloudfront.net/120770104/190-libre.pdf?1736657213=&amp;response-content-disposition=inline%3B+filename%3DQuantitative_analysis_and_paleoenvironme.pdf&amp;Expires=1772447085&amp;Signature=UurT22eV3jCrpNUxYZ3e~lg93VuDbTEmGJHUunYgfR7AeHxm-Z-phfzuF</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">26</style></volume><pages><style face="normal" font="default" size="100%">183–196</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	The middle Cenomanian deposits of the southern part of the Bellezma-Batna Mountains, northeastern Algeria, have been investigated to evaluate the response of Foraminifera to variations of paleo-bathymetry, oxygen, and salinity. The Djebel Azeb section, with a thickness of 40 m, is composed of a clay-marl mass interspersed with lumachellic limestone layers. It makes up the middle part of the ‘’Marnes de Smail’’ Formation. The Turrilites acutus Subzone of the upper part of the Acanthoceras rhotomagense Zone corresponds to the Aspidiscus cristatus Total Range Zone, and the Rotalipora cushmani Zone was recognized based on the study of ammonites, scleractinian and planktic foraminifera in this section. The statistical analysis of the foraminifera yielded only one assemblage of planktic foraminifera with globular chambers and trochospiral test belonging to the Cenomanian–Turonian; no association is typically restricted to the middle Cenomanian. The benthic foraminifera are poorly represented, belonging to the orders Textulariina, Lituolina, Trochamminina, Verneuilinina, Loftusiina, Orbitolinina, Miliolina, and Rotaliina. These foraminifera assemblages indicate that the bottom-water conditions during the middle Cenomanian were characterized by periodic changes in the oxygen and salinity. All planktic foraminifera species are opportunists related to poorly oxygenated, eutrophic conditions interspersed by a short interval of well-oxygenated environment with Planolites. The maximum abundance of Whiteinella and Muricohedbergella and the minimum amount of Planoheterohelix species within the Cenomanian of Djebel Azeb reflect dwindling palaeosalinity during this time, except for a slight increase in the middle of the section.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">3</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Nahnah, Raouia</style></author><author><style face="normal" font="default" size="100%">Benmansour, Sana</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Mixed marine, brackish water, non-marine, and subaerial microfaunal association in the Red Marls Formation of the Western Aurès Basin (Upper Paleocene)</style></title><secondary-title><style face="normal" font="default" size="100%">Revista Brasileira de Paleontologia </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2023</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.4072/rbp.2023.3.05</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">26</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	In the western part of the Aurès Basin (northeastern Algeria), the Red Marls of El Kantara Formation records a mixed microfaunal association of non-marine-brackish ostracoda, marine foraminifera, lacustrine charophytes, and subaerial&amp;nbsp;&lt;em&gt;Microcodiums&lt;/em&gt;. Based on the recovered biotic component, it is considered that the Red Marls of El-Kantara Formation date from the upper Paleocene (Thanetian). Seven species of brackish water (&lt;em&gt;Neocyprideis raoi&lt;/em&gt;) and non-marine ostracoda (&lt;em&gt;Frambocythere tumiensis anjarensis&lt;/em&gt;,&amp;nbsp;&lt;em&gt;Paracypretta jonesi&lt;/em&gt;,&amp;nbsp;&lt;em&gt;Paracypretta verruculosa&lt;/em&gt;,&amp;nbsp;&lt;em&gt;Limnocythere deccanensis&lt;/em&gt;,&lt;em&gt;&amp;nbsp;Darwinula torpedo&lt;/em&gt;&amp;nbsp;and&amp;nbsp;&lt;em&gt;Zonocypris spirula&lt;/em&gt;), have been discovered for the first time in Algeria and on the south Tethyan margin. Paleoenvironmentally, the overall biotic assemblage recovered indicates the presence of a freshwater palustrine/lacustrine depositional system connected to a low energy stream/river. This indicates that marginal marine conditions were prevalent in northeastern Algeria’s far inland regions. Paleobiogeographically, the seven known ostracod species have limited distributions that are until now common only with India. However, this disproved the theory that these species are endemic to the Indian Subcontinent, which is confirmed by their association with cosmopolitan charophytes.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">3</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Athamena, Ali</style></author><author><style face="normal" font="default" size="100%">Gaagai, Aissam</style></author><author><style face="normal" font="default" size="100%">Aouissi, Hani-Amir</style></author><author><style face="normal" font="default" size="100%">Burlakovs, Juris</style></author><author><style face="normal" font="default" size="100%">Bencedira, Selma</style></author><author><style face="normal" font="default" size="100%">Zekker, Ivar</style></author><author><style face="normal" font="default" size="100%">E. Krauklis, Andrey</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Chemometrics of the Environment: Hydrochemical Characterization of Groundwater in Lioua Plain (North Africa) Using Time Series and Multivariate Statistical Analysis</style></title><secondary-title><style face="normal" font="default" size="100%">Sustainability</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2023</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.3390/su15010020</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">15</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	This study aims to analyze the chemical composition of Lioua’s groundwater in order to determine the geological processes influencing the composition and origin of its chemical elements. Therefore, chemometrics techniques, such as multivariate statistical analysis (MSA) and time series methods (TSM) are used. Indeed, MSA includes a component analysis (PCA) and a cluster analysis (CA), while autocorrelation analysis (AA), supplemented by a simple spectral density analysis (SDA), is used for the TMS. PCA displays three main factors explaining a total variance (TV) of 85.01 %. Factors 1, 2, and 3 are 68.72%, 11.96%, and 8.89 % of TV, respectively. In the CA, total dissolved solids (TDS) and electrical conductivity (EC) controlled three groups. The elements SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2−&lt;/sup&gt;, K&lt;sup&gt;+&lt;/sup&gt;, and Ca&lt;sup&gt;2+&lt;/sup&gt;&amp;nbsp;are closely related to TDS, the elements Na&lt;sup&gt;+&lt;/sup&gt;, Cl&lt;sup&gt;−&lt;/sup&gt;, and Mg&lt;sup&gt;2+&lt;/sup&gt;&amp;nbsp;are closely related to CE, while HCO&lt;sup&gt;3−&lt;/sup&gt;&amp;nbsp;and NO&lt;sup&gt;3−&lt;/sup&gt;&amp;nbsp;indicate the dissociation of other chemical elements. AA shows a linear interrelationship of EC, Mg&lt;sup&gt;2+&lt;/sup&gt;, Na&lt;sup&gt;+&lt;/sup&gt;, K&lt;sup&gt;+&lt;/sup&gt;, Cl&lt;sup&gt;−&lt;/sup&gt;, and SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2−&lt;/sup&gt;. However, NO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;−&lt;/sup&gt;&amp;nbsp;and HCO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;−&lt;/sup&gt;&amp;nbsp;indicate uncorrelated characteristics with other parameters. For SDA, the correlograms of Mg&lt;sup&gt;2+&lt;/sup&gt;, Na&lt;sup&gt;+&lt;/sup&gt;, K&lt;sup&gt;+&lt;/sup&gt;, Cl&lt;sup&gt;−&lt;/sup&gt;, and SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2−&lt;/sup&gt;&amp;nbsp;have a similar trend with EC. Nonetheless, pH, Ca&lt;sup&gt;2+&lt;/sup&gt;, HCO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;−&lt;/sup&gt;&amp;nbsp;and NO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;−&lt;/sup&gt;&amp;nbsp;exhibit multiple peaks related to the presence of several distinct cyclic mechanisms. Using these techniques, the authors were able to draw the following conclusion: the geochemical processes impacting the chemical composition are (i) dissolution of evaporated mineral deposits, (ii) water–rock interaction, and (iii) evaporation process. In addition, the groundwater exhibits two bipolar characteristics, one recorded with negative and positive charges on pH and Ca&lt;sup&gt;+&lt;/sup&gt;&amp;nbsp;and another recorded only with negative charges on HCO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;−&lt;/sup&gt;&amp;nbsp;and NO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;−&lt;/sup&gt;. On the other hand, SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2−&lt;/sup&gt;, K&lt;sup&gt;+&lt;/sup&gt;, Ca&lt;sup&gt;2+&lt;/sup&gt;, and TDS are the major predominant elements in the groundwater’s chemical composition. Chloride presence mainly increases the electrical conductivity of water. The lithological factor is dominant in the overall mineralization of the Plio Quaternary surface aquifer waters. The origins of HCO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;−&lt;/sup&gt;&amp;nbsp;and NO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;−&lt;/sup&gt;&amp;nbsp;are as follows: HCO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;−&lt;/sup&gt;&amp;nbsp;has a carbonate origin, whereas NO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;–&lt;/sup&gt;&amp;nbsp;has an anthropogenic origin. The salinity was affected by Mg&lt;sup&gt;2+&lt;/sup&gt;, SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2−&lt;/sup&gt;, Cl&lt;sup&gt;−&lt;/sup&gt;, Na&lt;sup&gt;+&lt;/sup&gt;, K&lt;sup&gt;+&lt;/sup&gt;, and EC. Ca&lt;sup&gt;2+&lt;/sup&gt;, HCO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;−&lt;/sup&gt;, and NO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;−&lt;/sup&gt;&amp;nbsp;result from human activity such as the usage of fertilizers, the carbonate facies outcrops, and domestic sewage.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">1</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Gaagai, Aissam</style></author><author><style face="normal" font="default" size="100%">Aouissi, Hani-Amir</style></author><author><style face="normal" font="default" size="100%">Bencedira, Selma</style></author><author><style face="normal" font="default" size="100%">Hinge, Gilbert</style></author><author><style face="normal" font="default" size="100%">Athamena, Ali</style></author><author><style face="normal" font="default" size="100%">Heddam, Salim</style></author><author><style face="normal" font="default" size="100%">Gad, Mohamed</style></author><author><style face="normal" font="default" size="100%">Elsherbiny, Osama</style></author><author><style face="normal" font="default" size="100%">Elsayed, Salah</style></author><author><style face="normal" font="default" size="100%">Eid, Mohamed-Hamdy</style></author><author><style face="normal" font="default" size="100%">Ibrahim, Hekmat</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Application of Water Quality Indices, Machine Learning Approaches, and GIS to Identify Groundwater Quality for Irrigation Purposes: A Case Study of Sahara Aquifer, Doucen Plain, Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">Water</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2023</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.3390/w15020289</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">15</style></volume><pages><style face="normal" font="default" size="100%">289</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	In order to evaluate and project the quality of groundwater utilized for irrigation in the Sahara aquifer in Algeria, this research employed irrigation water quality indices (IWQIs), artificial neural network (ANN) models, and Gradient Boosting Regression (GBR), alongside multivariate statistical analysis and a geographic information system (GIS), to assess and forecast the quality of groundwater used for irrigation in the Sahara aquifer in Algeria. Twenty-seven groundwater samples were examined using conventional analytical methods. The obtained physicochemical parameters for the collected groundwater samples showed that Ca&lt;sup&gt;2+&lt;/sup&gt;&amp;nbsp;&amp;gt; Mg&lt;sup&gt;2+&lt;/sup&gt;&amp;nbsp;&amp;gt; Na&lt;sup&gt;+&lt;/sup&gt;&amp;nbsp;&amp;gt; K&lt;sup&gt;+&lt;/sup&gt;, and Cl&lt;sup&gt;−&lt;/sup&gt;&amp;nbsp;&amp;gt; SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2−&lt;/sup&gt;&amp;nbsp;&amp;gt; HCO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;−&lt;/sup&gt;&amp;nbsp;&amp;gt; NO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;−&lt;/sup&gt;, owing to the predominance of limestone, sandstone, and clay minerals under the effects of human activity, ion dissolution, rock weathering, and exchange processes, which indicate a Ca-Cl water type. For evaluating the quality of irrigation water, the IWQIs values such as irrigation water quality index (IWQI), sodium adsorption ratio (SAR), Kelly index (KI), sodium percentage (Na%), permeability index (PI), and magnesium hazard (MH) showed mean values of 47.17, 1.88, 0.25, 19.96, 41.18, and 27.87, respectively. For instance, the IWQI values revealed that 33% of samples were severely restricted for irrigation, while 67% of samples varied from moderate to high restriction for irrigation, indicating that crops that are moderately to highly hypersensitive to salt should be watered in soft soils without any compressed layers. Two-machine learning models were applied, i.e., the ANN and GBR for IWQI, and the ANN model, which surpassed the GBR model. The findings showed that ANN-2F had the highest correlation between IWQI and exceptional features, making it the most accurate prediction model. For example, this model has two qualities that are critical for the IWQI prediction. The outputs’ R&lt;sup&gt;2&lt;/sup&gt;&amp;nbsp;values for the training and validation sets are 0.973 (RMSE = 2.492) and 0.958 (RMSE = 2.175), respectively. Finally, the application of physicochemical parameters and water quality indices supported by GIS methods, machine learning, and multivariate modeling is a useful and practical strategy for evaluating the quality and development of groundwater.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">2</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Hammadi, A</style></author><author><style face="normal" font="default" size="100%">Brinis, Nafaa</style></author><author><style face="normal" font="default" size="100%">Djidel, M</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Hydrodynamic Characteristics of the &amp;ldquo;Complex Terminal&amp;rdquo; aquifer in the Region of Oued Righ North (Algerian Sahara).</style></title><secondary-title><style face="normal" font="default" size="100%">Algerian Journal of Environmental Science and Technology</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2023</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.aljest.net/index.php/aljest/article/view/879</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">9</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	Accessibility of fresh water, the nature's gift wheels the foremost part of the world economy. The sufficient supplies of water are essential for agriculture, human intake, industry as well as regeneration.&amp;nbsp;The Oued Righ region is located in Algeria's South-East, specifically in the North-East of the Sahara, on the Northern edge of the Grand Erg Oriental and the Southern border of the Aures massif. This area appears as a lower Sahara synclinal basin and is part of a broad North-South trending ditch.
&lt;/p&gt;

&lt;p style=&quot;text-align: justify;&quot;&gt;
	It is famous for its date palms, the development of the date culture in this region is attributed not only to the population’s efforts, but above all to the particular climatic conditions, the favorable soil characteristics and the existence of significant groundwater. The aim of this study is to understand the&amp;nbsp;results obtained from using different approaches of water&amp;nbsp;&amp;nbsp; hydrodynamics in&amp;nbsp;&amp;nbsp; the Complex Terminal aquifer.&amp;nbsp;The aquifer’s hydrodynamic characterization was carried out using hydrodynamic parameters and piezometry. As a result, the transmissivity and permeability obtained data using traditional Cooper-Jacob method&amp;nbsp;showed&amp;nbsp;that the flow capacities of the aquifer environment and the productivities of the structures are important in the studied zone where, the highest value of transmissivity equal&amp;nbsp;2.36× 10&lt;sup&gt;2-&lt;/sup&gt;m&lt;sup&gt;2&lt;/sup&gt;/s&lt;sup&gt;&amp;nbsp;&lt;/sup&gt;is found in the central part of the study area in El-Meghair. The establishment of piezometric maps reveals a flow direction oriented toward the chott.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">2</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Khadri, Rahma</style></author><author><style face="normal" font="default" size="100%">Abdelhamid, Khedidja</style></author><author><style face="normal" font="default" size="100%">Brinis, Nafaa</style></author><author><style face="normal" font="default" size="100%">Kharroubi, Maha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Geophysical and geological contribution to determining the neritic limestone aquifer structure of Hammam Bradaa &amp;ndash; El Fedjoudj (Seybouse medium), Northeastern Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">Mining of Mineral Deposits</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2023</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.researchgate.net/profile/Abdelhamid-Khedidja/publication/369638762_Geophysical_and_geological_contribution_to_determining_the_neritic_limestone_aquifer_structure_of_Hammam_Bradaa_-El_Fedjoudj_Seybouse_medium_Northeastern_Algeria/links/648d9aad</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">17</style></volume><pages><style face="normal" font="default" size="100%">67-73</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	&lt;strong&gt;Purpose. &lt;/strong&gt;The neritic aquifer that extends between Hammam Bradaa and El Fedjoudj, despite its faulted and in places karstified structure, due toits capacity and lateral extension represent a strategic resource for the region. Its waters are used for drinking water supply in the neighboring towns: Heliopolis, Guelaat Bousbaa, Nechmaya and El Fedjoudj, as well as in part of the Annaba wilaya. These neritic limestones outcrop at Djebel Debagh and Bouzitoune.
&lt;/p&gt;

&lt;p style=&quot;text-align: justify;&quot;&gt;
	&lt;strong&gt;Methods.&lt;/strong&gt; In order to better study the potential of this aquifer, it is essential to identify its geometry and structure by ana lyzing the geological data, mechanical drilling data and geophysical data analysis through an electrical survey campaign. Findings. The main results indicate that the study area has identified two important aquifer formations: a formation in the Mio-Plio-Quaternary alluvium consisting of clays, marls, gravel and sand; the second is a deep carbonate aquifer composed of fissured and karstified neritic limestone of the Cretaceous age of variable depth ranging within 50 and 350 m.
&lt;/p&gt;

&lt;p style=&quot;text-align: justify;&quot;&gt;
	&lt;strong&gt;Originality.&lt;/strong&gt; The originality of the study is in the fact that the studied area is characterized by the presence of thick, frac tured and karstified carbonate formations, which are intensively tectonized and have significant aquifer potential.
&lt;/p&gt;

&lt;p style=&quot;text-align: justify;&quot;&gt;
	&lt;strong&gt;Practical implications. &lt;/strong&gt;The correlation of geological data with geophysical data made it possible to conclude that the stu died area is a sedimentary basin bounded by faults predominantly oriented to the south-west and north-east, forming a highly fractured unit consisting of horsts and grabens. The significant water potential reservoir is formed essentially by carbonate geological formations, highly fractured with the presence of karst forms represented by resistant horizons.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">1</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Tafrount, Assia</style></author><author><style face="normal" font="default" size="100%">Drias, Tarek</style></author><author><style face="normal" font="default" size="100%">Chenaf,  Djaouida</style></author><author><style face="normal" font="default" size="100%">Brinis, Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Hydrogeochemical evolution and mineralization origin in a semi-arid shallow aquifer: a case study of the Barika area in northeast Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">Acque Sotterranee - Italian Journal of Groundwater </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2023</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.acquesotterranee.net/acque/article/download/624/495</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">12</style></volume><pages><style face="normal" font="default" size="100%">19-34</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	Most Middle Eastern and North African regions are characterized by an arid and semi-arid climate. As such, the drinking water supply and management have become a challenging task for local and regional authorities. The Mio-Plio Quaternary aquifer of the Barika area is the only drinking and irrigation water reservoir in the region. The objective of this paper is to identify the origin and evolution process of the groundwater mineralization of this aquifer using major elements as indicators. To achieve this objective water samples were collected, from several boreholes drilled in the aquifer, in June 2018 and March 2019, and subsequently analyzed. The results obtained in terms of Gibbs plot, Piper, chemical correlation, and statistical analysis of chemical data identified the origins of groundwater mineralization. The dissolution of evaporated minerals, precipitation of carbonates, evapotranspiration, and ion exchange reactions have been identified as the primary processes of mineralization. The results of the physicochemical analysis showed that these waters consisted mainly of chloride, calcium sulfate, and magnesium facies types with a slight change of facies in some boreholes during the two sampling periods. This is due to the interactions with the-aquifer geology and to the water scarcity caused by climate change.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">2</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Khadri, Rahma</style></author><author><style face="normal" font="default" size="100%">Abdelhamid Khedidja</style></author><author><style face="normal" font="default" size="100%">Boubaya, Djamel</style></author><author><style face="normal" font="default" size="100%">Brinis, Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Integrated gravity and resistivity investigations of the deep Hammam Bradaa aquifer, Northeast Algeria: Implications for groundwater exploration</style></title><secondary-title><style face="normal" font="default" size="100%">Journal of African Earth Sciences</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2023</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%"> https://doi.org/10.1016/j.jafrearsci.2023.10501</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">205</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Recently, the Guelma region, located northeast of Algeria, has been facing an unusual water shortage. To bypass this situation, a geophysical study using gravity and resistivity has been initiated to enhance the understanding of the&amp;nbsp;geology&amp;nbsp;and&amp;nbsp;hydrogeology&amp;nbsp;of the deep structures of the study area. In order to accomplish this, a residual&amp;nbsp;gravity anomaly&amp;nbsp;map has been constructed by removing from the&amp;nbsp;Bouguer anomaly&amp;nbsp;map a regional gravity gradient using the upward continuation technique. For the purpose of validating the Vertical Electrical Sounding(VES) interpretation, two soundings were conducted near boreholes with known&amp;nbsp;lithology. The Hammam Bradaa deep aquifer of the Guelma region is composed of limestones that belong to the Constantine neritic domain. The Constantine neritic domain is covered by thrust nappes and outcrops in some places of the study area as tectonic windows. The exact geometry such as depth and lateral extent of the aquifer are not well known. Since limestones are characterized by high densities and resistivities relative to the host rock, the combining of gravity and VES was able to accurately map their extension among the other lithologies composing the geological section. Multiscale edge detection of gravity data known as &quot;worms&quot; made it possible to highlight the principal lineaments across the study area which may contribute to the recharge of the Hammam Bradaa aquifer. The 3D Gravity inversion enabled the mapping of the spatial configuration of limestones that are characterized by positive gravity contrast relative to the host rocks. A vertical density slice extracted from the 3D gravity inversion, running from north to south, reveals a significant thickness of limestone beneath Hammam Bradaa which suggests a strong potential for groundwater resources. The geo-electric section, constructed from the interpretation of VES data and calibrated with well&amp;nbsp;lithology, enabled the mapping of the depth to the top of limestone beneath conductive alluvium and marls.</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Athamena,Malika</style></author><author><style face="normal" font="default" size="100%">Athamena, Ali</style></author><author><style face="normal" font="default" size="100%">Menani, Mohamed-Redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Study of the thermal sources of the Bellezmamounts, eastern Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">Algerian Journal of Environmental Science and Technology </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2023</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">Algerian Journal of Environmental Science and Technology</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">9</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	The Bellezma Mounts, located in the northeast of Algeria, present cases of hydrothermalism with temperatures ranging between 30° C and 63° C. For the evaluation of the thermal potential of this dissymmetrical mountains chains (often rectified in the South, where Cretaceous and Jurassic limestones emerge), we used a multidisciplinary approach, notably geology, geophysics, hydrogeology, hydrochemistry and the isotopic tool. Hydrogeological investigations have shown that these carbonate formations can offer an important aquifer potential. From the hydrochemical point of view, the warm waters of the Bellezma mounts are characterized by the presence of three different chemical facies: the sulfated-sodium, the bicarbonate-calcium and the chloride-calcium. Evaporite terrigenous origin is attributed to sodium, chlorides and sulphates of these waters. The thermal waters circulation in this region, at great depths in the crystallophyllian formations and the carbonate ones, in contact with terrigenous salt formations, could be responsible of the salinity characterizing these waters, in some places. Geothermometry has shown that these thermal waters acquire a high temperature in their original tanks coming from a depth ranging from 1100 to 2600 m through a fault system that affects the basement. The use of the isotopic tool has shown that the thermal waters of this region are ancient and that their recharge is weak or non-existent.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">3</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Saadali, Badreddine</style></author><author><style face="normal" font="default" size="100%">Zerrouki,  Hichem</style></author><author><style face="normal" font="default" size="100%">Drias, Tarek</style></author><author><style face="normal" font="default" size="100%">Abdelhamid Khedidja</style></author><author><style face="normal" font="default" size="100%">Haoues,  Cherif</style></author><author><style face="normal" font="default" size="100%">Moufida Belloula</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Hydrogeochemical assessment to characterize the water quality for agricultural use in Mexanna and Bougous dams in the province of El Tarf, Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">Euro-Mediterranean Journal for Environmental Integration </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2022</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://link.springer.com/article/10.1007/s41207-022-00291-w?utm_source=researchgate.net&amp;utm_medium=article</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">7</style></volume><pages><style face="normal" font="default" size="100%">79–88</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	The Mexa and Bougous dams were built to control river floods and supply crop-irrigation and drinking water. This study aimed to characterize the hydrogeochemical state in the region containing the dams, which influences the quality of the waters and thus their suitability for agricultural use, given the extent of the river networks that naturally transport sediments and pollutants into the reservoirs via streams. Thus, some physicochemical and organic parameters, including electrical conductivity, calcium, magnesium, sodium, potassium, chloride, bicarbonate, sulfate, biological oxygen demand, nitrite, ammonium, and phosphate, were used as benchmarks to examine the stiffness of the water pollution. Sampling was carried out during May and September of 2011 and 2012. The obtained results showed that, according to the Stiff diagram, the dominant hydrogeochemical facies is calcium bicarbonate in waters that do not have calcium levels in excess of 3 meq/l and bicarbonate levels in excess of 2.4 meq/l. The organic pollution index disclosed that the waters have evolved from a moderate to a high degree of organic pollution due to the accumulation of pollutants and nutrients from waste disposal and fertilizers. The samples fell into the C2-S1 class in the Richards diagram; this implies that the waters are suitable for plants that are salt tolerant, but that the use of these waters can cause problems for clay soils. However, in the long term, irrigation with the dam waters may pose difficulties for agriculture due to the resulting increase in the electrical conductivity of the soil. This study concludes that water salinity and alkalinity affect crop suitability, meaning that the temporal monitoring of water quality is needed to avoid adverse consequences for crop production.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Abdelhamid Khedidja</style></author><author><style face="normal" font="default" size="100%">Dib, Imen</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Effect of the agriculture on the quality of groundwater in the alluvial aquifer of the Tadjenanet area (eastern Algeria)</style></title><secondary-title><style face="normal" font="default" size="100%">  Geomatics, Landmanagement and Landscape</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2022</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://gll.urk.edu.pl/Effect-of-the-agriculture-on-the-quality-of-groundwater-in-the-alluvial-aquifer-of,153518,0,2.html</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">3</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	The region of Tadjenanet is in eastern Algeria in the high plains, characterized by a varied age detritus Mio-Plio-Quaternary. Some geological formations can be an important source of groundwater (alluvial sand, shell limestone, gravel). Its location in semi-arid area involves evaporation pronounced even tilt the balance in a chronic deficit, excluding periods characterized by rainfall events. Agriculture in the study area is the first socio-economic activity and the largest consumer of water resources. It is therefore necessary to consider for effective water management. Indeed, the combination of hydrogeological and hydro chemical geological mapping, geophysics, harvested from field data and their interpretations can be an excellent tool for deciding the suitability of water for irrigation. The analysis of the physicochemical data shows an increase in the concentration of nitrates reaching 200 mg · l–1, as well as the analysis by the Richards SAR parameter shows that most groundwater samples are generally suitable for agricultural purposes with 33%, belong characterizing poor quality. Indeed, the groundwater in the region generally requires prior treatment before consumption and use depending on the type of crop. The assessment of the quality of the water in the region and its consequences on the soil and the types of crops has enabled the authorities concerned to manage the water supply adequately to preserve and protect this vital source for the future from any risk of contamination.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Dib, Imane</style></author><author><style face="normal" font="default" size="100%">Abdelhamid Khedidja</style></author><author><style face="normal" font="default" size="100%">Chettah, Wahid</style></author><author><style face="normal" font="default" size="100%">Hadji, Riheb</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Multivariate statistical-based approach to the physical-chemical behavior of shallow groundwater in a semiarid dry climate: The case study of the Gadaïne-Ain Yaghout plain NE Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">Mining of Mineral Deposits</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2022</style></year></dates><volume><style face="normal" font="default" size="100%">16</style></volume><pages><style face="normal" font="default" size="100%">38-47</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	&lt;strong&gt;Purpose.&lt;/strong&gt; Several natural and anthropogenic factors control the hydro-geochemical behavior of groundwater. These factors influence on the quality, even the suitability of this resource for drinking. The main purpose of our study is the application of multivariate statistical methods to compile the mechanisms of mineralization acquisition in confined aquifers. Methods. The adopted method measures the chemical evolution of Ca+2, Mg+2, Na+, K+, HCO-3, Cl-, SO4-2, NO-3, NO-2, NH+4, and PO4-3 using an atomic-absorption spectrometer. The content of nitrogen and dissolved oxygen is measured using a spectrophotometer. Temperature (T°), electrical conductivity (EC), pH and dissolved oxygen are determined using a multi-parameter system. Findings. The main results show that 28 water samples from the Mio-Plio-Quaternary aquifer of the Gadaïne-Ain Yaghout plain have chemical facies of chloride, sulfate-calcium and chloride-magnesium types. Originality. The originality of the study is in the demonstration that water acquires its carbonate mineralization at the supply limits. Whereas it acquires its chloride, sodium and sulfate mineralization in contact with terrigenous saliferous formations, as well as in its interaction with the salt chotts formations. The results show a significant variation in the concentrations of chemical elements, in some cases exceeding drinkability standards. Mineralization is mainly caused by the dissolution of evaporitic minerals such as gypsum, halite and epsomite.
&lt;/p&gt;

&lt;p style=&quot;text-align: justify;&quot;&gt;
	&lt;strong&gt;Practical implications. &lt;/strong&gt;The practical implications of this study could be resumed in terms of the convenience of multiva-riate statistical evaluation of complex physical-chemical databases in identifying pollution sources and understanding temporal variations for effective groundwater quality management in semiarid regions.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">3</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Abdelhamid Khedidja</style></author><author><style face="normal" font="default" size="100%">Lecheheb, Brahim</style></author><author><style face="normal" font="default" size="100%">Reghais, Azzeddine</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Landslide of the RN 77, PK 23+100, commune of Texenna (Wilaya of Jijel, Algeria): stability and comfort</style></title><secondary-title><style face="normal" font="default" size="100%">THE SECOND EDITION OF THE SEMINAR ON GEOHAZARDS IN ALGERIA</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2022</style></year></dates><pub-location><style face="normal" font="default" size="100%">Mila, Algeria</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	The landslide studied is located on RN 77 at PK 23+100 in the municipality of Texenna, 25 km southeast of the wilaya of Jijel. The faults observed in the study area are the result of the combination of several factors: the slope of the slope, the lithology of the soil and the strong pluviometry. The project studied consists in the design and analysis of the stability and reinforcement by backfill reinforced with geotextiles. A visual survey was carried out to clarify the probable causes of the impairments, followed by a geological and geotechnical reconnaissance campaign to determine the lithological nature and the physical and mechanical properties of the different formations that make up the soil. The study continued with a backfill reinforced with geotextiles. The analysis of stability and reinforcement was carried out using the finite element method and Plaxis 2D software. According to the results obtained, which give satisfactory values for the coefficient of safety for different combinations of loads, the choice of installing the geotextile wall at the foot of the road is a technical and economic solution aimed at ensuring stability and restoring the collapsed part of the roadway Keywords: Stability; Reinforced embankment; Coefficient of safety.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Saadali, Badreddine</style></author><author><style face="normal" font="default" size="100%">Zerrouki, Hamza</style></author><author><style face="normal" font="default" size="100%">Drias, Tarek</style></author><author><style face="normal" font="default" size="100%">Abdelhamid Khedidja</style></author><author><style face="normal" font="default" size="100%">Haoues,  Cherif</style></author><author><style face="normal" font="default" size="100%">Moufida Belloula</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Hydrogeochemical assessment to characterize the water quality for agricultural use in Mexanna and Bougous dams in the province of El Tarf, Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">Euro-Mediterranean Journal for Environmental Integration</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2022</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://link.springer.com/article/10.1007/s41207-022-00291-w</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">7</style></volume><pages><style face="normal" font="default" size="100%">79–88</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	The Mexa and Bougous dams were built to control river floods and supply crop-irrigation and drinking water. This study aimed to characterize the hydrogeochemical state in the region containing the dams, which influences the quality of the waters and thus their suitability for agricultural use, given the extent of the river networks that naturally transport sediments and pollutants into the reservoirs via streams. Thus, some physicochemical and organic parameters, including electrical conductivity, calcium, magnesium, sodium, potassium, chloride, bicarbonate, sulfate, biological oxygen demand, nitrite, ammonium, and phosphate, were used as benchmarks to examine the stiffness of the water pollution. Sampling was carried out during May and September of 2011 and 2012. The obtained results showed that, according to the Stiff diagram, the dominant hydrogeochemical facies is calcium bicarbonate in waters that do not have calcium levels in excess of 3 meq/l and bicarbonate levels in excess of 2.4 meq/l. The organic pollution index disclosed that the waters have evolved from a moderate to a high degree of organic pollution due to the accumulation of pollutants and nutrients from waste disposal and fertilizers. The samples fell into the C2-S1 class in the Richards diagram; this implies that the waters are suitable for plants that are salt tolerant, but that the use of these waters can cause problems for clay soils. However, in the long term, irrigation with the dam waters may pose difficulties for agriculture due to the resulting increase in the electrical conductivity of the soil. This study concludes that water salinity and alkalinity affect crop suitability, meaning that the temporal monitoring of water quality is needed to avoid adverse consequences for crop production.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Boufekane, Abdelmadjid</style></author><author><style face="normal" font="default" size="100%">Moufida Belloula</style></author><author><style face="normal" font="default" size="100%">Busico, Gianluigi</style></author><author><style face="normal" font="default" size="100%">Drias, Tarek</style></author><author><style face="normal" font="default" size="100%">Reghais, Azzeddine</style></author><author><style face="normal" font="default" size="100%">Maizi, Djamel</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Hybridization of DRASTIC Method to Assess Future GroundWater Vulnerability Scenarios: Case of the Tebessa-Morsott Alluvial Aquifer (Northeastern Algeria)</style></title><secondary-title><style face="normal" font="default" size="100%">Applied Sciences</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2022</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.3390/app12189205</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">12</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	In this study, a new approach integrating a groundwater vulnerability method and a numerical model for predicting groundwater resource sustainability under actual and future conditions of exploitation (2010–2030) is proposed in the semi-arid region of the Tebessa-Morsott alluvial aquifer (northeastern Algeria). The groundwater vulnerability method-based DRASTIC model was used to evaluate and delineate the vulnerable areas using a GIS technique. The MODFLOW code, on the other hand, was used to calculate the dynamics of groundwater level under actual and future conditions of exploitation considering two scenarios. The results of the application of the DRASTIC method to the reference year conditions (year 2010) showed that the high and average vulnerability classes covered a wide zone of the study area, about 97%. These results were validated based on the nitrate concentration values (R&lt;sup&gt;2&lt;/sup&gt;&amp;nbsp;= 0.955). However, the results for predicting future groundwater vulnerability showed that groundwater vulnerability variation over time (period 2010–2030) was closely related to groundwater depth variation caused by the pumping rate, since the decreases in the piezometric level produce a worsening of groundwater vulnerability. To achieve better groundwater management, an experimental site for artificial recharge supplemented by hydro-chemical monitoring of the groundwater could be an effective remediation strategy.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">18</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Boumaiza, Lamine</style></author><author><style face="normal" font="default" size="100%">Walter, Julien</style></author><author><style face="normal" font="default" size="100%">Chesnaux, Romain</style></author><author><style face="normal" font="default" size="100%">Zahi, Faouzi</style></author><author><style face="normal" font="default" size="100%">Huneau, Frédéric</style></author><author><style face="normal" font="default" size="100%">Garel, Emilie</style></author><author><style face="normal" font="default" size="100%">Stotler, Randy-L</style></author><author><style face="normal" font="default" size="100%">Bordeleau, Geneviève</style></author><author><style face="normal" font="default" size="100%">Johannesson, Karen-H</style></author><author><style face="normal" font="default" size="100%">Vystavna, Yuliya</style></author><author><style face="normal" font="default" size="100%">Drias, Tarek</style></author><author><style face="normal" font="default" size="100%">Re,  Viviana</style></author><author><style face="normal" font="default" size="100%">Knöller, Kay</style></author><author><style face="normal" font="default" size="100%">Stumpp, Christine</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Combined effects of seawater intrusion and nitrate contamination on groundwater in coastal agricultural areas: A case from the Plain of the El-Nil River (North-Eastern Algeria)</style></title><secondary-title><style face="normal" font="default" size="100%">Science of The Total Environment</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2022</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.1016/j.scitotenv.2022.158153</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">851</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	This study focuses on&amp;nbsp;coastal aquifers&amp;nbsp;subject to uncontrolled land use development by investigating the combined effects of seawater intrusion and nitrate contamination. The research is undertaken in a Mediterranean coastal agricultural area (Plain of the El-Nil River, Algeria), where water resources are heavily impacted by anthropogenic activities. A multi-tracer approach, integrating hydrogeochemical and isotopic tracers (δ&lt;sup&gt;2&lt;/sup&gt;H&lt;sub&gt;H2O&lt;/sub&gt;, δ&lt;sup&gt;18&lt;/sup&gt;O&lt;sub&gt;H2O&lt;/sub&gt;, δ&lt;sup&gt;15&lt;/sup&gt;N&lt;sub&gt;NO3&lt;/sub&gt;&amp;nbsp;and δ&lt;sup&gt;18&lt;/sup&gt;O&lt;sub&gt;NO3&lt;/sub&gt;), is combined with a hydrochemical facies evolution diagram, and a Bayesian isotope mixing model (MixSIAR) to assess seawater contamination with its inland intrusion, and distinguish the nitrate sources and their apportionment. Results show that seawater intrusion is circumscribed to the sector neighboring the Mediterranean Sea, with two influencing functions including classic inland intrusion through the aquifer, and upstream seawater impact through the river mouth connected to the Mediterranean Sea. Groundwater and surface water samples reveal nitrate concentrations above the natural baseline threshold, suggesting anthropogenic influence. Results from nitrate&amp;nbsp;isotopic composition, NO&lt;sub&gt;3&lt;/sub&gt;&amp;nbsp;and Cl concentrations, and the MixSIAR model show that nitrate concentrations chiefly originate from sewage and manure sources. Nitrate derived from the sewage is related to wastewater discharge, whereas nitrate derived from the manure is attributed to an excessive use of animal manure to fertilise agricultural areas. The dual negative impact of seawater intrusion and nitrate contamination degrades water quality over a large proportion of the study area. The outcomes of this study are expected to contribute to effective and sustainable&amp;nbsp;water resources management&amp;nbsp;in the Mediterranean coastal area. Furthermore, this study may improve scientists' ability to predict the combined effect of various anthropogenic stressors on coastal environments and help decision-makers elsewhere to prepare suitable environmental strategies for other regions currently undergoing an early stage of water resources deterioration.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Slami, Rafika</style></author><author><style face="normal" font="default" size="100%">Bruno Ferré</style></author><author><style face="normal" font="default" size="100%">Benkherouf-Kechid, Fatiha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Cenomanian ostracods (Crustacea) of Djebel Sabaoune (Batna, Algeria): Specific assemblage and significance</style></title><secondary-title><style face="normal" font="default" size="100%">Journal of African Earth Sciences</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2022</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.1016/j.jafrearsci.2022.104604</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">193</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	The&amp;nbsp;Cenomanian&amp;nbsp;‘Marnes de Smail’ Formation in Djebel Sabaoune (Batna, Algeria) contains many&amp;nbsp;fossil&amp;nbsp;ostracods&amp;nbsp;with 73 species taxa that are identified for the first time from this area. The ostracod assemblages are consistent with the&amp;nbsp;Cenomanian&amp;nbsp;age formerly assigned by means of invertebrate macrofossils:&amp;nbsp;ammonites, corals, bivalves, echinoids and gastropods. The diverse ostracofaunal assemblages allowed us to reconstruct the palaeoenvironmental parameters that prevailed during the Cenomanian. Both qualitative and quantitative analyses of ostracod assemblages, along with foraminiferal associations and&amp;nbsp;lithofacies, documented progressive environmental change from a relatively deep marine or outer distal platform (at the base of this series) to a middle, inner platform and, finally, to a reefal environment (at the top). The ostracod taxa are mostly&amp;nbsp;endemic species. However, the occurrences of species already known from North and&amp;nbsp;West Africa, the Middle East and the Atlantic clearly demonstrate that migrations still occurred during the Cenomanian.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>5</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Chairat, Imen</style></author><author><style face="normal" font="default" size="100%">Fouad Djaiz</style></author><author><style face="normal" font="default" size="100%">Mabrouk Boughdiri</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">The Cenomano-Turonian Facies Through the Algerian-Tunisian Confines (Region of Tebessa): Correlations, Subsidence and Source Rock</style></title><secondary-title><style face="normal" font="default" size="100%"> Advances in Geophysics, Tectonics and Petroleum Geosciences</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2022</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	The Algero-Tunisian confines (Tebessa region) belong to the southern Tethyan domain and the Monts Mellegue. This region is partly composed of Cenomano-Turonian carbonate outcrops; therefore, the investigated sections&amp;nbsp;highlight the black shale levels reported over a short period, around the Cenomanian-Turonian boundary. The lithostratigraphic study designated a depositional environment that emphasized a relatively deep, calm, and often confined ocean environment significantly shallower on the northern part of the study area. The facies lithology and distribution leads&amp;nbsp; to underline the pelagic influences during the upper Cretaceous and neritic throughout&amp;nbsp;the lower Cretaceous period. The&amp;nbsp;maximum thickness of the Cenomano-Turonian (1000&amp;nbsp;m) was recorded&amp;nbsp;in the southern zones and the&amp;nbsp;minimum (100&amp;nbsp;m) occurred&amp;nbsp; further north. This palaeogeographic organization persists&amp;nbsp;laterally in Tunisia as&amp;nbsp;the extension of the Constantine mole. The geochemical analyses reveal&amp;nbsp;that the maturity of the Cenomanian source rock is variable. Nevertheless,&amp;nbsp;the Turonian source rock &amp;nbsp;seems to be&amp;nbsp;at the beginning of the oil phase.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Bachir Lamouri</style></author><author><style face="normal" font="default" size="100%">Labadi, Abdellah-Seddik</style></author><author><style face="normal" font="default" size="100%">Boukoffa, Machati</style></author><author><style face="normal" font="default" size="100%">Chouaf, Ibtissem</style></author><author><style face="normal" font="default" size="100%">Djouder, Hocine</style></author><author><style face="normal" font="default" size="100%">Fouad Djaiz</style></author><author><style face="normal" font="default" size="100%">Bouabsa, Lakhdar</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">A preliminary mineralogical and physicochemical characterization of the Neogene clays from the Timgad Basin (Massif of Aurès, NE Algeria): potential use in the manufacturing of bricks and ceramic industry</style></title><secondary-title><style face="normal" font="default" size="100%"> SN Applied Sciences</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2022</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://link.springer.com/article/10.1007/s42452-022-05029-5?utm_source=researchgate.net&amp;utm_medium=article</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">4</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	This study aims at the mineralogical and physicochemical characterization of the clay formations of the Miocene age from the Timgad Basin (Massif of Aurès, NE Algeria), in order to evaluate their possible valorization, notably for their potential use in the manufacturing of bricks and ceramic industry. For this purpose, four samples were taken from a clay-dominated formation that outcrops 5&amp;nbsp;km east of the Timgad city. Each sample was collected, prepared, and analyzed by the appropriate analytical methods of characterization such as X-ray diffraction, X-ray fluorescence, and scanning electron microscopy. Moreover, other complementary analyses are performed in this study such as laser granulometry and geotechnical tests. The results of the different tests revealed that the clay formations of the Timgad Basin are non-refractory clays and characterized by medium plasticity. These clays are constituted of more than 50% of fine fraction, mainly represented by kaolinite in association with non-negligible proportions of illite, chlorite, mixed-layer clay minerals, and traces of smectite. Besides, this clayey assemblage is accompanied by some proportion of quartz and calcite, as well as traces of hematite, feldspar, and gypsum. In the light of these results and in combination with the particle size distribution, as well as the results of geotechnical tests, it is concluded that the Neogene clays of the Timgad Basin present high limits of Atterberg. Consequently, their use in the field of manufacturing of bricks and terra cotta ‘Terre Cuite’ products is subordinated to a preliminary treatment with addition of a degreasing agent, in the form of coarse sand, in order to improve their plasticity.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">149</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Marred, Manal</style></author><author><style face="normal" font="default" size="100%">Naimi, Mohammed-Nadir</style></author><author><style face="normal" font="default" size="100%">Fouad Djaiz</style></author><author><style face="normal" font="default" size="100%">Kherchouche, Adila</style></author><author><style face="normal" font="default" size="100%">Boushaba, Abdellah</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Gastrochaenolites ornatus Kelly and Bromley and other trace fossils on a Middle Miocene omission surface from the Aures Massif, Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">Proceedings of the Geologists' Association</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2022</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.1016/j.pgeola.2022.04.004</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">133</style></volume><pages><style face="normal" font="default" size="100%">218-226</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	Trace fossils provide detailed palaeoenvironmental and palaeoecological information of both ancient and modern sedimentary systems. During middle Miocene times the Aures Massif located in the northeastern part of Algeria, was affected by, at least, one marine transgression. The latter led to the installation of a carbonate platform, which is placed, for the first time, in a Mediterranean context. In the Rhassira basin, the Middle Miocene marine succession is characterised by carbonate platform deposits dominated by rhodolith beds, typical of those known throughout the Mediterranean area. This succession can be divided into many units separated by discontinuities interpreted here as omission surfaces. The Djebel Arhane section shows two omission surfaces characterised by a pre-omission suite (firmground) represented by Balanoglossites burrows for the first surface and Gastrochaenolites ornatus burrows/borings for the second one, and an omission suite (hardground) as evidenced by the bioerosive structures Trypanites and Caulostrepsis, in both surfaces, respectively. Gastrochaenolites ornatus traces were formed and preserved in firm, compact, semi-lithified and fine-grained substrates (firm- to hardground), indicating the Glossifungites ichnofacies. They show bioglyphs which have been formed during contraction of the posterior adductor muscles. These suggest that their tracemakers were represented by suspension-feeding bivalves, most probably Pholadidae or Mytilidae, which rotated during penetration. The fill of these traces is composed of marine deposits related to a transgressive lag. The omission suite is divided into two ichnocoenoses: (i) pre-lithification burrows/borings, and (ii) post-lithification borings. This is the first report of the ichnotaxon G. ornatus from Algeria.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">3</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Cherif,  Ichrak</style></author><author><style face="normal" font="default" size="100%">Touansa, Rachid</style></author><author><style face="normal" font="default" size="100%">Mabrouk Boughdiri</style></author><author><style face="normal" font="default" size="100%">Fouad Djaiz</style></author><author><style face="normal" font="default" size="100%">Bahrouni, Nejib</style></author><author><style face="normal" font="default" size="100%">Sallouhi, Houaïda</style></author><author><style face="normal" font="default" size="100%">Yahiaoui,  Abdelwaheb</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Updated calpionellid zonation around the Jurassic&amp;ndash;Cretaceous boundary in NE Algeria (&amp;ldquo;Ravin Bleu&amp;rdquo; site, Batna Mountains): A potential regional stratotype for the North Africa Maghrebian Ranges</style></title><secondary-title><style face="normal" font="default" size="100%">Geologica Carpathica</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2022</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">10.31577/GeolCarp.73.5.3</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">73</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	In NE Algeria and the Tunisia–Algeria border chains, detailed stratigraphic investigations across the Jurassic– Cretaceous boundary (JKB) are scarce and this important stratigraphic interval remains poorly known. This work attempts fulfilling this gap of our knowledge on the JKB successions in this area. It represents unpublished data on calpionellid zonations, based on bed-by-bed sampling, of two sections from the “Ravin Bleu” site of Batna Mountains. In the Jebel Kasserou and J. Bou Merzoug study sections, most of the standard Upper Tithonian–lowermost Valanginian calpionellid zones and subzones are first identified here. Their limits correspond to main calpionellid bioevents allowing to recognize a new Alpelliptica Subzone of the Calpionella Zone in the Lower–Middle Berriasian; subsidiary bioevents being useful to delimit six horizons in the Upper Tithonian Crassicollaria Zone and two others in the Middle Berriasian Elliptica Subzone. All these biostratigraphic units are correlated with their lateral equivalents in other Tethyan sections, mainly from Morocco, Tunisia, SE France, Spain, the Carpathian Ranges and the Balkanides. Chitinoidellid and most of the calpionellid species from Eastern Algeria are first illustrated here. In addition to their easy access and good outcrops, the continuous, complete and thick marine study successions are devoid of strong diagenetic alteration, synsedimentary features and tectonic effects. The “Ravin Bleu” site is proposed herein as a potential reference section for the JKB interval in the North Africa Maghrebian Ranges of the SW Tethys Margin.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">5</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Gaagai, Aissam</style></author><author><style face="normal" font="default" size="100%">Aouissi, Hani-Amir</style></author><author><style face="normal" font="default" size="100%">E. Krauklis, Andrey</style></author><author><style face="normal" font="default" size="100%">Burlakovs, Juris</style></author><author><style face="normal" font="default" size="100%">Athamena, Ali</style></author><author><style face="normal" font="default" size="100%">Zekker, Ivar</style></author><author><style face="normal" font="default" size="100%">Boudoukha, Abderahmane</style></author><author><style face="normal" font="default" size="100%">Benaabidate, Lahcen</style></author><author><style face="normal" font="default" size="100%">Haroun Chenchouni</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Modeling and Risk Analysis of Dam-Break Flooding in a Semi-Arid Montane Watershed: A Case Study of the Yabous Dam, Northeastern Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">Algerian Journal of Environmental Science and Technology</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2022</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.3390/w14050767</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">14</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	The risk related to embankment dam breaches needs to be evaluated in order to prepare emergency action plans. The physical and hydrodynamic parameters of the flood wave generated from the dam failure event correspond to various breach parameters, such as width, slope, and formation time. This study aimed to simulate the dam breach failure scenario of the Yabous dam (northeast Algeria) and analyze its influence on the related areas (urban and natural environments) downstream of the dam. The simulation was completed using the sensitivity analysis method to assess the impact of breach parameters and flooding on the dam break scenario. The flood wave propagation associated with the dam break was simulated using the one-dimensional HEC-RAS hydraulic model. This study applied a sensitivity analysis of three breach parameters (slope, width, and formation time) on five sites selected downstream of the embankment dam. The simulation showed that the maximum flow of the flood wave recorded at the level of the breach was 8768 m&lt;sup&gt;3&lt;/sup&gt;/s, which gradually attenuated along the river course to reach 1972.7 m&lt;sup&gt;3&lt;/sup&gt;/s at about 8.5 km downstream the dam. This study established the map of flood risk areas that illustrated zones threatened by the flooding wave triggered by the dam failure due to extreme rainfall events. The sensitivity analysis showed that flood wave flow, height, and width revealed positive and similar changes for the increases in adjustments (±25% and ±50%) of breach width and slope in the five sites. However, flood wave parameters of breach formation time showed significant trends that changed in the opposite direction compared to breach slope and width. Meanwhile, the adjustments (±25% and ±50%) of the flood hydrograph did not significantly influence the flood parameters downstream of the dam. In the present study, the HEC-RAS 1-D modeling demonstrated effectiveness in simulating the propagation of flood waves downstream of the dam in the event of dam failure and highlighted the impact of the breach parameters and the flood hydrographical pattern on flood wave parameters.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">5</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Halima Belalite</style></author><author><style face="normal" font="default" size="100%">Menani, Mohamed-Redha</style></author><author><style face="normal" font="default" size="100%">Athamena, Ali</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Calculation of water needs of the main crops and water resources available in a semi-arid climate, case of Zana-Gadaïne plain, Northeastern Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">Algerian Journal of Environmental Science and Technology</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2022</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.aljest.net/index.php/aljest/article/view/570</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">8</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	The relative scarcity of water resources in Algeria and their unequal distribution induce a rational use of available resources. The Zana-Gadaïne plain appears as an exemplary case study, where the difficulties posed by the problem of crop water needs versus the availability of water resources appear. This article, based on field surveys and in-situ measurements, aims to identify the pressure of irrigation on water resources and the optimization of their use in an agricultural area, where irrigated agriculture represents 85% of the water consumption of the Zana-Gadaïne plain. The piezometric study in correlation with hydrogeological data reveals that groundwater resources are limited, aggravated by wastage resulting in a consequent drawdown of 24 meters over 11 years. The analysis of interannual climate variability has enabled us to draw rainfall maps characteristic of the evolution of rainfall over the past decades where we observe a net deficit in precipitation. We calculated the evapotranspiration and the requirements in irrigation water for each crop in order to compare them with the available hydric resources and the establishment of irrigation schedules for the principal irrigated crops. The analysis of interannual climate variability has enabled us to draw rainfall maps characteristic of the evolution of rainfall over the past decades where we observe a net deficit in precipitation. We calculated the evapotranspiration and the requirements in irrigation water for each crop in order to compare them with the available hydric resources and the establishment of irrigation schedules for the principal irrigated crops.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">2</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Gaagai, Aissam</style></author><author><style face="normal" font="default" size="100%">Aouissi, Hani-Amir</style></author><author><style face="normal" font="default" size="100%">E. Krauklis, Andrey</style></author><author><style face="normal" font="default" size="100%">Burlakovs, Juris</style></author><author><style face="normal" font="default" size="100%">Burlakovs, Juris</style></author><author><style face="normal" font="default" size="100%">Zekker, Ivar</style></author><author><style face="normal" font="default" size="100%">Boudoukha, Abderahmane</style></author><author><style face="normal" font="default" size="100%">Benaabidate, Lahcen</style></author><author><style face="normal" font="default" size="100%">Haroun Chenchouni</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Modeling and Risk Analysis of Dam-Break Flooding in a Semi-Arid Montane Watershed: A Case Study of the Yabous Dam, Northeastern Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">Water</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2022</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.3390/w14050767</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">14</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	The risk related to embankment dam breaches needs to be evaluated in order to prepare emergency action plans. The physical and hydrodynamic parameters of the flood wave generated from the dam failure event correspond to various breach parameters, such as width, slope, and formation time. This study aimed to simulate the dam breach failure scenario of the Yabous dam (northeast Algeria) and analyze its influence on the related areas (urban and natural environments) downstream of the dam. The simulation was completed using the sensitivity analysis method to assess the impact of breach parameters and flooding on the dam break scenario. The flood wave propagation associated with the dam break was simulated using the one-dimensional HEC-RAS hydraulic model. This study applied a sensitivity analysis of three breach parameters (slope, width, and formation time) on five sites selected downstream of the embankment dam. The simulation showed that the maximum flow of the flood wave recorded at the level of the breach was 8768 m&lt;sup&gt;3&lt;/sup&gt;/s, which gradually attenuated along the river course to reach 1972.7 m&lt;sup&gt;3&lt;/sup&gt;/s at about 8.5 km downstream the dam. This study established the map of flood risk areas that illustrated zones threatened by the flooding wave triggered by the dam failure due to extreme rainfall events. The sensitivity analysis showed that flood wave flow, height, and width revealed positive and similar changes for the increases in adjustments (±25% and ±50%) of breach width and slope in the five sites. However, flood wave parameters of breach formation time showed significant trends that changed in the opposite direction compared to breach slope and width. Meanwhile, the adjustments (±25% and ±50%) of the flood hydrograph did not significantly influence the flood parameters downstream of the dam. In the present study, the HEC-RAS 1-D modeling demonstrated effectiveness in simulating the propagation of flood waves downstream of the dam in the event of dam failure and highlighted the impact of the breach parameters and the flood hydrographical pattern on flood wave parameters.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">5</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Hammadi, Aziza</style></author><author><style face="normal" font="default" size="100%">Brinis, Nafaa</style></author><author><style face="normal" font="default" size="100%">Djidel, Mohamed</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Hydrogeochemical behavior associated with a diverse etiology of high salinity in phreatic water along Oued Righ valley in Algerian Sahara</style></title><secondary-title><style face="normal" font="default" size="100%"> Arabian Journal of Geosciences</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2022</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://link.springer.com/article/10.1007/s12517-022-10402-0</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">15</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	In the northeastern Algerian Sahara, the Oued Righ region is one of the most prominent geothermal areas and it is defined by a hot arid climate. Water resources in Oued Righ valley are heterogeneous in terms of geological and environmental conditions; this is marked by multi-layer groundwater system through the formations of the Continental Intercalary aquifer, the Terminal Complex, and the Phreatic water. The Phreatic water is an important aquifer system used for public water supply and irrigation purposes. The main objective of this paper is to study the quality of Phreatic water through, the hydrogeochemistry characteristics in order to investigate how it mineralizes. Thirty water samples were collected in July 2019 and September 2020 and were analyzed for major dissolved chemical components. The water samples are characterized by conductivities ranged from 6360 to 193900 μS/cm (July 2019) and 6890 to 226400 μS/cm (September 2020). The water is mostly of sodium chlorinated, sodium, and magnesium sulfated types. Results of mineral equilibrium modeling showed that the Phreatic waters of Oued Righ are undersaturated with respect to evaporite minerals. Gibbs plot revealed that, the evaporations and crystallization dominance activities and oceanic tides are the primary causes of increased salinity in the Phreatic water of the studied area. The Phreatic water of Oued Righ perceived a change in its chemical characteristics during the tow sampling periods, caused by water-rock interactions and mixing processes.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Benfarhi, Farida</style></author><author><style face="normal" font="default" size="100%">Menani, Mohamed-Redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Risk assessment of irrigation with water contaminated by trace metals on the soil&amp;ndash;plant complex in the El Madher plain, north-east Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">JOURNAL OF WATER AND LAND DEVELOPMENT </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2022</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://jwld.pl/files/2022-01-JWLD-07.pdf</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">54</style></volume><pages><style face="normal" font="default" size="100%">59–67</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	Polluted water poses significant health risks when it is part of the water sources used for irrigation, leading to the contamination of soil and plants by various pollutants. This work aims, firstly, to assess the degree of pollution of Wadi El Gourzi water (Batna, Algeria), and then to verify the consequences on their use for the irrigation of market garden plants for everyday consumption (lettuce, cilantro, parsley and spinach), both in the aerial part (stems and leaves) and in the soil where they are grown. This study focuses on trace metals (Cr, Pb, Zn and Cd). Soil pollution was assessed by calculating the soil pollution index (PI), while the uptake of these elements by plants was monitored by the transfer factor (TF). The analyses of the Wadi El Gourzi water with the flame atomic absorption spectrophotometer (FAAS) show a maximum abnormal concentration of Cr (17.37 mg∙dm–3), Pb (0.71 mg∙dm–3) and Cd (0.45 mg∙dm–3). For the analysis of the soils irrigated by these waters, the results of the PI show that the soils used for the cultivation of parsley and lettuce are polluted by several metals (PI &amp;gt; 1). The concentrations of trace metals elements (TMEs) in the sampled plants show a significant accumulation of Zn, Cd, Pb and Cr by the vegetables (coriander, parsley, spinach and lettuce). These concentrations are above the permitted standards.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Dekakra, Mouna</style></author><author><style face="normal" font="default" size="100%">Menani, Mohamed-Redha</style></author><author><style face="normal" font="default" size="100%">Abdelhamid Khedidja</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">GROUNDWATER QUALITY ASSESSMENT: A CASE STUDY OF THE TELEGHMA PLAIN, ALGERIA</style></title><secondary-title><style face="normal" font="default" size="100%">Analele Universității din Oradea, Seria Geografie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2022</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.30892/auog.322104-890  </style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">32</style></volume><pages><style face="normal" font="default" size="100%">114-125</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	The Teleghma plain is located in northeastern Algeria, in the upper valley of Oued Rhumel. It is characterised by a semi-arid climate with average annual precipitation of 300 mm/ year. The shallow aquifer of Mio-Plio-Quaternary is powered mainly by carbonate formations of the Eocene surrounding the région. The uncontrolled use of groundwater for irrigation has caused water stress in the area which has threatened the degradation of water quality. On the other hand, the intense use of chemical fertilisers for agriculture aims has caused groundwater pollution by nitrates where concentrations exceeded the standard limit recommended by the world health organisation.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">2</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Halima Belalite</style></author><author><style face="normal" font="default" size="100%">Menani, Mohamed-Redha</style></author><author><style face="normal" font="default" size="100%">Athamena, Ali</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Calculation of water needs of the main crops and water resources available in a semi-arid climate, case of Zana-Gadaïne plain, Northeastern Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">Algerian Journal of Environmental Science and Technology</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2022</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.aljest.net/index.php/aljest/article/view/570</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">8</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	&amp;nbsp;The relative scarcity of water resources in Algeria and their unequal distribution induce a rational use of available resources. The Zana-Gadaïne plain appears as an exemplary case study, where the difficulties posed by the problem of crop water needs versus the availability of water resources appear. This article, based on field surveys and in-situ measurements, aims to identify the pressure of irrigation on water resources and the optimization of their use in an agricultural area, where irrigated agriculture represents 85% of the water consumption of the Zana-Gadaïne plain. The piezometric study in correlation with hydrogeological data reveals that groundwater resources are limited, aggravated by wastage resulting in a consequent drawdown of 24 meters over 11 years. The analysis of interannual climate variability has enabled us to draw rainfall maps characteristic of the evolution of rainfall over the past decades where we observe a net deficit in precipitation. We calculated the evapotranspiration and the requirements in irrigation water for each crop in order to compare them with the available hydric resources and the establishment of irrigation schedules for the principal irrigated crops. The analysis of interannual climate variability has enabled us to draw rainfall maps characteristic of the evolution of rainfall over the past decades where we observe a net deficit in precipitation. We calculated the evapotranspiration and the requirements in irrigation water for each crop in order to compare them with the available hydric resources and the establishment of irrigation schedules for the principal irrigated crops.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">2</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Zouaoui, Siham</style></author><author><style face="normal" font="default" size="100%">Menani, Mohamed-Redha</style></author><author><style face="normal" font="default" size="100%">Gaagai, Aissam</style></author><author><style face="normal" font="default" size="100%">Bouabid, Abdennasser</style></author><author><style face="normal" font="default" size="100%">Bencedira, Selma</style></author><author><style face="normal" font="default" size="100%">Zekker, Ivar</style></author><author><style face="normal" font="default" size="100%">Aouissi, Hani-Amir</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution of Stables Isotopes to the Study of the Groundwater Recharge in the Southern Foothills of the Saharan Atlas: The case of Tolga Region, North Eastern Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">Research Square</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2022</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.researchsquare.com/article/rs-1869669/v1</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	Tolga groundwater is one of Biskra's most important water supplies for both drinking and agriculture. The purpose of this study is to assess the hydrochemical and isotope (2H and 18O) signature of water in the Tolga area. To evaluate the hydrogeology of groundwater in the Tolga region, a chemical, piezometric, and isotopic research was employed. The results of the Piper diagram revealed that there is just one major hydrochemical facies in the research region, which corresponds to Ca–Mg–Cl–SO4. The piezometry of limestone sheets shows that as one goes westward, the turns become less substantial, with turns about 20 meters and a piezometric level of 140 m. For the rst time, the local meteoric water line (LMWL) was drawn for Complexe Teminal (CT) and Continental Intercalaire (CI) on Tolga groundwater. The Tolga area LMWL refers to the equation δ2H= 7,18 δ18O + 4.17 with R2 about 0.85. CI and CT measurement locations indicate deuterium excess values ranging from 8.35 to 12.57. Indeed, the majority of values were more than 10‰ (mean of 10.36 ± 2.01‰). Furthermore, waters from Eocene have an isotopic composition of-7.57 ± 0.68‰ in δ18O and − 49.04 ± 4.69‰ In δ2H. The results of the sample characterisation analysis show that the majority of the groundwater samples analysed are of the Ca-Mg-SO4 water type. In addition, the intense exploitation aquifer water and the region's arid climatic conditions resulted in a large decrease in the piezometric limestone level. Finely, the signature of 2H and 18O data indicate that water comes from local precipitation and recent water, and groundwater recharge is in uenced by quick in ltration.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">H. Belalite,</style></author><author><style face="normal" font="default" size="100%">Menani, Mohamed-Redha</style></author><author><style face="normal" font="default" size="100%">A. Athamena</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Calculation of water needs of the main crops and water resources available in a semi-arid climate, case of Zana-Gadaïne plain, Northeastern Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">Algerian Journal of Environmental Science and Technology ALJEST</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2022</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.aljest.net/index.php/aljest/article/view/570</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">8</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	The relative scarcity of water resources in Algeria and their unequal distribution induce a rational use of available resources. The Zana-Gadaïne plain appears as an exemplary case study, where the difficulties posed by the problem of crop water needs versus the availability of water resources appear. This article, based on field surveys and in-situ measurements, aims to identify the pressure of irrigation on water resources and the optimization of their use in an agricultural area, where irrigated agriculture represents 85% of the water consumption of the Zana-Gadaïne plain. The piezometric study in correlation with hydrogeological data reveals that groundwater resources are limited, aggravated by wastage resulting in a consequent drawdown of 24 meters over 11 years. The analysis of interannual climate variability has enabled us to draw rainfall maps characteristic of the evolution of rainfall over the past decades where we observe a net deficit in precipitation. We calculated the evapotranspiration and the requirements in irrigation water for each crop in order to compare them with the available hydric resources and the establishment of irrigation schedules for the principal irrigated crops. The analysis of interannual climate variability has enabled us to draw rainfall maps characteristic of the evolution of rainfall over the past decades where we observe a net deficit in precipitation. We calculated the evapotranspiration and the requirements in irrigation water for each crop in order to compare them with the available hydric resources and the establishment of irrigation schedules for the principal irrigated crops.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">2</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Boumaiza, Lamine</style></author><author><style face="normal" font="default" size="100%">Chesnaux, Romain</style></author><author><style face="normal" font="default" size="100%">Walter, Julien</style></author><author><style face="normal" font="default" size="100%">Drias, Tarek</style></author><author><style face="normal" font="default" size="100%">Huneau, Frédéric</style></author><author><style face="normal" font="default" size="100%">Garel, Emilie</style></author><author><style face="normal" font="default" size="100%">Vystavna, Yuliya</style></author><author><style face="normal" font="default" size="100%">Stumpp, Christine</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Reviewing the anthropogenic sources of groundwater contamination in the Plain of the El-Nil River, Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">74th Canadian Geotechnical Conference; 14th joint with IAH-CNC</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2021</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	&lt;br&gt;Located in northeast Algeria, the coastal aquifer of the Plain of the El-Nil River constitutes a significant source of groundwater. It contains many municipal and private wells used for several purposes, including agriculture irrigation and drinking water. This paper describes a review of potential anthropogenic sources of groundwater contamination over the Plain of the El-Nil River territory. Different potential sources are identified, including 1) cultivated fields, 2) old private sanitation systems, 3) seawater intrusion, 4) dumpsite, and 5) the contaminated rivers crossing the study area. The multi-sources of contamination in the coastal aquifer of the Plain of the El-Nil River could affect large sectors of the aquifer. However, the existing documentation of groundwater contamination of the Plain of the El-Nil River is still limited. Hence, a hydrogeochemical study, including the analyses of major chemical elements and certain stable isotopes, is proposed as the principal outcome of this site-review paper. If undertaken, this proposed study is expected to provide more accurate information on groundwater contamination and, subsequently, could help decision-makers to prepare a practical plan for protecting the local water resources.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Boumaiza, Lamine</style></author><author><style face="normal" font="default" size="100%">Chesnaux, Romain</style></author><author><style face="normal" font="default" size="100%">Drias, Tarek</style></author><author><style face="normal" font="default" size="100%">Walter, Julien</style></author><author><style face="normal" font="default" size="100%">Huneau, Frédéric</style></author><author><style face="normal" font="default" size="100%">Garel, Emilie</style></author><author><style face="normal" font="default" size="100%">Knöller, Kay</style></author><author><style face="normal" font="default" size="100%">Stumpp, Christine</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Hydrochemical and isotopic evidence for seawater intrusion into the coastal aquifer of Taleza, Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">74th Canadian Geotechnical Conference; 14th joint with IAH-CNC</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2021</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.cgsconferences.ca/fr/GEO2021/GEO2021_53.html</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	Located in north-east Algerian, the coastal aquifer of Taleza constitutes a significant source of groundwater. It contains hundreds of private wells installed by the population for several purposes including drinking water. Recently, the groundwater has become quite saline; in order to investigate this issue, hydrochemical and isotopic groundwater characterization is carried out, including the analyses of major elements and water stable isotopes d2H-H2O and d18O-H2O. Results confirmed a saltwater intrusion, and interestingly, the intrusion mechanism appears to be more complex than a direct intrusion from the Mediterranean Sea. During the high-water period, saltwater intrusion may also originate from the two rivers bordering the aquifer, via upstream migration of seawater through the river mouths. The heavier ratios in d2H-H2O and d18O-H2O of surface water collected from the rivers suggest that the Mediterranean Sea water is mixing with rivers water. The present study shows that seawater may exert deleterious impacts on groundwater quality and greatly limit conditions for the sustainable groundwater management.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Boumaiza, Lamine</style></author><author><style face="normal" font="default" size="100%">Chesnaux, Romain</style></author><author><style face="normal" font="default" size="100%">Drias, Tarek</style></author><author><style face="normal" font="default" size="100%">Walter, Julien</style></author><author><style face="normal" font="default" size="100%">Stumpp, Christine</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Using vadose-zone water stable isotope profiles for assessing groundwater recharge under different climatic conditions</style></title><secondary-title><style face="normal" font="default" size="100%">Hydrological Sciences Journal </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2021</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.1080/02626667.2021.1957479</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">10</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	Considering three sites under different climate conditions (arid, semi-arid, and subhumid), this study aims to use the vadose-zone water stable isotope profiles to estimate the groundwater recharge rate. High-resolution vertical subsurface soil sampling along the vadose zone of the investigated sites was conducted. The collected samples were analysed to determine their stable isotope ratios (δ&lt;sup&gt;2&lt;/sup&gt;H and δ&lt;sup&gt;18&lt;/sup&gt;O) that were used along with the piston displacement method to estimate recharge. Annual recharge rates of 0.2% (± 0.1%), 2.5%, and 18% of the total annual precipitation were obtained for the arid, semi-arid, and subhumid sites, respectively. Recharge rates at the semi-arid and subhumid sites are comparable to those previously estimated using water balance-based methods. The recharge rate at the arid site is lower than that previously estimated for that site using the water budget-based method, revealing difficulties in applying the piston displacement method under an arid regime.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">66</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Benyoucef,  Madani</style></author><author><style face="normal" font="default" size="100%">Bendella, Mohamed</style></author><author><style face="normal" font="default" size="100%">Brunetti, Mauro</style></author><author><style face="normal" font="default" size="100%">Bruno Ferré</style></author><author><style face="normal" font="default" size="100%">Koci, Tomas</style></author><author><style face="normal" font="default" size="100%">Bouchemla, Imad</style></author><author><style face="normal" font="default" size="100%">Slami, Rafika</style></author><author><style face="normal" font="default" size="100%">Ghenim,   Asma-Fethia</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Upper Pliocene bivalve shell concentrations from the Lower Chelif basin (NW Algeria): Systematics, sedimentologic and taphonomic frameworkConcentrations à coquilles de bivalves dans le Pliocène supérieur du bassin du Bas Chélif (NO Algérie) : systém</style></title><secondary-title><style face="normal" font="default" size="100%">Annales de Paléontologie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2021</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.1016/j.annpal.2021.102509 Get rights and content</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">107</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	Sedimentologic and palaeontological investigation of the Upper Pliocene Slama Formation in the Lower Chelif Basin (NW Algeria) led us to collect important bivalve assemblages for taxonomic and taphonomic purposes. A rather comprehensive inventory list of Upper Pliocene bivalves from northwestern Algeria is now available and consists of 30 species, 17 of which are extinct ones. Four principal taphonomic attributes were analysed: bioerosion, encrustation, fragmentation, and abrasion. Physical and biogenic sedimentary structures are used for palaeoenvironmental interpretations. The taphonomic, sedimentologic and ichnological characteristics of most of the deposits suggests they originated from discontinuous processes of winnowing and bypassing of sediments, probably due to the action of storms in shallow waters, mainly in the shoreface depositional environment. The bivalve assemblage is dominated by disarticulated valves and displays significant taphonomic alteration in the shells. Sclerobionts traces in shells particulary affect the oyster shells. Bioerosion traces are predominately those of clionid sponges (&lt;em&gt;Entobia&lt;/em&gt;&amp;nbsp;isp.), polychaetes (&lt;em&gt;Maeandropolydora&lt;/em&gt;&amp;nbsp;isp. and&amp;nbsp;&lt;em&gt;Caulostrepsis&lt;/em&gt;&amp;nbsp;isp.), bivalves (&lt;em&gt;Gastrochaenolites&lt;/em&gt;&amp;nbsp;isp.), and of predatory gastropods (&lt;em&gt;Oichnus&lt;/em&gt;&amp;nbsp;isp.). Among the sclerobionts, the identified encrusters were juvenile oyster recruits, barnacles, polychaetes (serpulid tubeworms), bryozoans (&lt;em&gt;Microporella&lt;/em&gt;&amp;nbsp;sp. and&amp;nbsp;&lt;em&gt;Acanthodesia&lt;/em&gt;&amp;nbsp;sp.), and vermetid gastropods (&lt;em&gt;Petaloconchus intortus&lt;/em&gt;).
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">4</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Benmansour, Sana</style></author><author><style face="normal" font="default" size="100%">Bernard, Andreu</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Répartition paléobiogéographique des ostracodes dans le Campanien-Maastrichtien du Bassin des Aurès, Algérie</style></title><secondary-title><style face="normal" font="default" size="100%">27e édition de la Réunion des Sciences de la Terre</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2021</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fouad Djaiz</style></author><author><style face="normal" font="default" size="100%">DEFAFLIA , Nabil</style></author><author><style face="normal" font="default" size="100%">Bachir Lamouri</style></author><author><style face="normal" font="default" size="100%">Boushaba, Abdellah</style></author><author><style face="normal" font="default" size="100%">Chairat, Imen</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Quaternary Fluviatile Terraces of the Oued El Gourzi (Batna, NE Algeria): Sedimentology and Characteristics of the Depositional Environment</style></title><secondary-title><style face="normal" font="default" size="100%">Science Technology and Innovation</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2021</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.researchgate.net/publication/351090687_Quaternary_Fluviatile_Terraces_of_the_Oued_El_Gourzi_Batna_NE_Algeria_Sedimentology_and_Characteristics_of_the_Depositional_Environment</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	Field observations and sedimentological analyses of alluvial terraces of the O. Gourzi (Batna, NE Algeria) lead us to consider sediments as dominated by clayey and silty-sandy fractions overlain by gravel and calcareous coarser fractions. Moderate CaO 3 contents would have resulted from the dissolution of the nearby carbonate relieves. They are mainly composed of Maastrichtian limestones. The distribution of the mineral fraction led us to identify 07 levels including horizons of coarse fractions alternating with layers rich in sand and silt with a roughly constant clay fraction through the stratigraphic column. Kurtosis values, frequency histograms of a prokurtic type, rarily mesokurtic, mark a constant power mode for the transport agent. Classification indices indicate poorly-to moderately sorted material, indicating a turbiditic depo-sitional environment. Quartz grain nature and mor-phoscopy refer to Miocene sandstones as a potential origin. The ferruginous coating is due to the initiating pedogenesis.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Hanini, Amine</style></author><author><style face="normal" font="default" size="100%">Houla, Yassine</style></author><author><style face="normal" font="default" size="100%">DJAIZ, Foued</style></author><author><style face="normal" font="default" size="100%">Chairat, Imen</style></author><author><style face="normal" font="default" size="100%">Mabrouk Boughdiri</style></author><author><style face="normal" font="default" size="100%">Maamri, Ridha</style></author><author><style face="normal" font="default" size="100%">Zagrarni,Mohamed-Faouzi</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Characterization of Cenomanian-Turonian oxic facies in Tunisia: sequence stratigraphy and correlation of recorded bioevents</style></title><secondary-title><style face="normal" font="default" size="100%">Arabian Journal of Geosciences </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2021</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">10.1007/s12517-021-07286-x</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">14</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	On the southwestern Tethyan Margin of Tunisia, the well-known anoxic black shale facies of the Cenomanian-Turonian transition contrasts with oxic fossiliferous carbonates, first characterized here as lateral equivalents. In terms of sequence stratigraphy, the analysis of four wisely sampled sections in Central and Southern Tunisia led to interpret these deposits as a transgressive interval (TST). This interval spans the&amp;nbsp;&lt;i&gt;Whiteinella archaeocretacea&lt;/i&gt;&amp;nbsp;Zone of foraminifera and is capped with a glauconite-rich highly bioturbated maximum flooding surface (MFS). In the reference section of Oued Bahloul and the Kalaat Senan area of North-Central Tunisia, these deposits overlay a Shelf Margin Wedge made of conglomeratic and bioclastic limestones. In South-Central and Southern Tunisia, the TST is characterized by the onset of oxic facies relaying laminated carbonates with local emergence surfaces. The analysis of both oxic and anoxic facies from the Cenomanian-Turonian transition allows identifying five successive bioevent markers, known elsewhere within the Tethyan domain: the extinction of the foraminifera genus&amp;nbsp;&lt;i&gt;Rotalipora&lt;/i&gt;&amp;nbsp;(or&amp;nbsp;&lt;i&gt;Thomasinella&lt;/i&gt;), the&amp;nbsp;&lt;i&gt;Heterohelix&lt;/i&gt;&amp;nbsp;shift, the&amp;nbsp;&lt;i&gt;Whiteinella&lt;/i&gt;&amp;nbsp;proliferation, the filament event, and the appearance of&amp;nbsp;&lt;i&gt;Helvetotruncana helvetica&lt;/i&gt;. Among these bioevents, the&amp;nbsp;&lt;i&gt;Heterohelix&lt;/i&gt;&amp;nbsp;shift coincides with the transgressive surface, while the filament event announces the maximal flooding surface. These Cenomanian-Turonian transition bioevents are of a particular relevance for regional and long-distance high-resolution correlations.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">11</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">RABAHI, Noureddine</style></author><author><style face="normal" font="default" size="100%">Fouad Djaiz</style></author><author><style face="normal" font="default" size="100%">DEFAFLIA , Nabil</style></author><author><style face="normal" font="default" size="100%">GUASTALDI, Enrico</style></author><author><style face="normal" font="default" size="100%">AMROUNE, Abdelouahab</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">THE VERTICAL DISTRIBUTION OF THE ALLUVIAL CHEMO-FACIES OF BOUMERZOUG WADI, CONSTANTINE, NORTHEASTERN ALGERIA: PALEOENVEROMENTAL SIGNIFICANCE AND CLIMATE EVOLUTION</style></title><secondary-title><style face="normal" font="default" size="100%">Analele Universităţii din Oradea, Seria Geografie </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2021</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.researchgate.net/deref/https%3A%2F%2Fdoi.org%2F10.30892%2Fauog.311108-865?_tp=eyJjb250ZXh0Ijp7ImZpcnN0UGFnZSI6InB1YmxpY2F0aW9uIiwicGFnZSI6InB1YmxpY2F0aW9uIiwicHJldmlvdXNQYWdlIjoicHJvZmlsZSJ9fQ</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">31</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	The authorities of Constantine city have been working on the redevelopment and calibration of the Rhumel and Boumerzoug wadis since 2015. The latter calebrage works caused great damage to the banks, thus affecting the Quaternary geological formations in place (alluvial terraces, flood plains). A multidisciplinary research project based on a geomorphological and sedimentological approach was quickly set up to create a scientific data base before their total destruction and loss of physical traces all along the wadis. The present study focuses on the sedimentological and geochemical analysis of the alluvial deposits of Boumerzoug wadi in order to describe the sediments, to reconstitute their nature, and to interpret both the climatic evolution and the paleo-environments of the region. Sedimentological and geochemical results confirm the succession of deposition cycles linked to progressive climate change.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">1</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis, Nafaa</style></author><author><style face="normal" font="default" size="100%">Brahmia, Ali</style></author><author><style face="normal" font="default" size="100%">Hamel, Ahmed</style></author><author><style face="normal" font="default" size="100%">Benhamida, Slimane</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Origin and dynamics of ions controlling the mineralisation of water&amp;rsquo;s spring of the upstream part of the Wady Labiod Valley, (W) BATNA, Algeria. Regions: Ichemoul, Arris, T&amp;rsquo;Kout and Ghassira</style></title><secondary-title><style face="normal" font="default" size="100%">Hydroscience Journal</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2021</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.tandfonline.com/doi/full/10.1080/27678490.2021.1974285#abstract</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">107</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	There are several springs in the “Aures”. They represent an opportunity for mountain populations where connection to the drinking water is difficult. They are used for human consumption, but mostly for agriculture. In this paper we try to classify about twenty perennial springs and identify the origin of the mineralisation by linking each class to a lithological context. These sources belong to several chemical groups whose apparent type do not necessarily reflect the lithological composition of the corresponding aquifers. Thus, a carbonated water passing through evaporitic formations can acquire a new facies, which further complicates the interpretations. The combination of thermodynamic simulation, statistics and hydrochemistry has given satisfactory results on the chemical identity of these waters. There are, in fact, two groups : one of the carbonated waters ; dominant with 63% of samples. The other gypsum with 37% of the samples checked. The rHCO3/rSO4 ratio often gives values superior than 1 which can reach the threshold of 5. The results indicate that : Ca, SO4, HCO3 and Mg control the mineralisation of the water. The phenomena that generated these two groups are multiple and mainly concern the lithological composition of aquifers as well as the mechanisms of mineralisation acquisition during the underground journey before reaching the surface.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">1</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Hamouda, Abida</style></author><author><style face="normal" font="default" size="100%">Benyahia, Lamia</style></author><author><style face="normal" font="default" size="100%">Brinis, Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">DECODING SPATIAL FRAMEWORK OF ROMAN-AFRICAN DOMUS, CASE OF CUICUL (DJEMILA) ALGERIA</style></title><secondary-title><style face="normal" font="default" size="100%">Mediterranean Archaeology and Archaeometry (MAA)</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2021</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.maajournal.com/index.php/maa/article/view/589</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">21</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	This article focuses on a type of habitat that existed in the Roman territories in North Africa and assumes that the domestic architecture of the domus is a reflection of the collective identity of culture buried for millennia and considers that house can be a carrier of cultural information in its spatial configuration. Space syntax, through its configurational analysis techniques, allows establishing a qualitative and quantitative analysis by reconstructing the ancestral way of life and the interactions between inhabitants and strangers. We here present and discusse the results of the syntactic analyzes applied to a set of large Roman-African residences or domus in the Roman site of Djemila (cuicul) in Algeria. Topics covered include the spatial organization of the domus and the potential for integration and control of shared activity areas within the residence, with an assessment of its relationship with human use of space and functioning of the domus with the public space through its permeability. It appears that the spatial and formal models created through buildings and the way they are connected and sequenced correspond to codes that govern the activities that take place there, those that need to be separated, and which categories of people have access to them. The domus is structured by the introduction of a multitude of transitional spaces which had two major effects: creating a hierarchy from the outside world to the interior of the building and inducing movement by creating circulation alternatives and help separate areas of unrelated function and areas dedicated to a specific function.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">3</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Mohamadi, Abderrahim</style></author><author><style face="normal" font="default" size="100%">Demdoum, Abdeslam</style></author><author><style face="normal" font="default" size="100%">Bouaicha, Foued</style></author><author><style face="normal" font="default" size="100%">Menani, Mohamed-Redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Evaluation of the quality of groundwater for its appropriateness for irrigation purposes using Water Quality Index (WQI), Mchira-Teleghma aquifer case study, northeastern Algeria</style></title><secondary-title><style face="normal" font="default" size="100%"> Sustainable Water Resources Management </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2021</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://link.springer.com/article/10.1007/s40899-021-00571-3</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">7</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	The Mio-Plio-Quaternary groundwater of Mchira-Teleghma suffers from an increasing rate of salinity especially in the northwestern part. To identify the reason for the water’s salinity and its aptitude for irrigation, physico-chemical analyses of 20 water samples, which were based on the different physical and chemical parameters (electric conductivity EC, pH, Ca&lt;sup&gt;2+&lt;/sup&gt;, Mg&lt;sup&gt;2+&lt;/sup&gt;, Na&lt;sup&gt;+&lt;/sup&gt;, K&lt;sup&gt;+&lt;/sup&gt;, HCO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;−&lt;/sup&gt;, Cl&lt;sup&gt;−&lt;/sup&gt;, SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2−&lt;/sup&gt;, NO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;−&lt;/sup&gt;&amp;nbsp;and Sr&lt;sup&gt;2+&lt;/sup&gt;), were carried out during the period of October 2015. This study showed disquieting anomalies of electric conductivity that reached the value of 4376.14 µS cm&lt;sup&gt;−1&lt;/sup&gt;. The statistical analyses, the multivariate statistics: the principal component analysis, Q-mode cluster analyses, Sr&lt;sup&gt;2+&lt;/sup&gt;/Ca&lt;sup&gt;2+&lt;/sup&gt;&amp;nbsp;ratio and water type showed that the hydrochemistry of Mchira-Teleghma groundwater is controlled by the dissolution of carbonate rocks and the leaching of evaporite processes, which proved that these anomalies of the MPQ groundwater’s salinity of Mchira-Teleghma are mainly determined by the leaching of Triassic gypsum formations process. This hydrogeochemical process generates an unsuitable quality of water based on Wilcox’s and Water Quality Index’s methods, whereas Richard’s method classifies all water samples to C3S1 and C4S1 classes as they are recommended to be used with salt-tolerant species in well-drained and leached soils.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">97</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Boumaiza, Lamine</style></author><author><style face="normal" font="default" size="100%">Chesnaux, Romain</style></author><author><style face="normal" font="default" size="100%">Drias, Tarek</style></author><author><style face="normal" font="default" size="100%">Walter, Julien</style></author><author><style face="normal" font="default" size="100%">Stumpp, Christine</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Using vadose-zone water stable isotope profiles for assessing groundwater recharge under different climatic conditions</style></title><secondary-title><style face="normal" font="default" size="100%">Hydrological Sciences Journal </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2021</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.tandfonline.com/doi/full/10.1080/02626667.2021.1957479</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">66</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	Considering three sites under different climate conditions (arid, semi-arid, and subhumid), this study aims to use the vadose-zone water stable isotope profiles to estimate the groundwater recharge rate. High-resolution vertical subsurface soil sampling along the vadose zone of the investigated sites was conducted. The collected samples were analysed to determine their stable isotope ratios (δ&lt;sup&gt;2&lt;/sup&gt;H and δ&lt;sup&gt;18&lt;/sup&gt;O) that were used along with the piston displacement method to estimate recharge. Annual recharge rates of 0.2% (± 0.1%), 2.5%, and 18% of the total annual precipitation were obtained for the arid, semi-arid, and subhumid sites, respectively. Recharge rates at the semi-arid and subhumid sites are comparable to those previously estimated using water balance-based methods. The recharge rate at the arid site is lower than that previously estimated for that site using the water budget-based method, revealing difficulties in applying the piston displacement method under an arid regime.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">10</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DEFAFLIA , Nabil</style></author><author><style face="normal" font="default" size="100%">Fouad Djaiz</style></author><author><style face="normal" font="default" size="100%">Fehdi, Chamseddine</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">paleoenvironmental study of oum ali region(tébessa, algeria) during quaternary, through the study of fluvial terrace of khenigue wadi</style></title><secondary-title><style face="normal" font="default" size="100%">ACTA GEOBALCANICA  </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2021</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.geobalcanica.org/wp-content/uploads/AGB/2021/AGB-2021-7-21.pdf</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">7</style></volume><pages><style face="normal" font="default" size="100%">151-157</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	Stratigraphic, sedimentological and magnetic study was performed on alluvial terraces, rich in archaeological tools, the region of OUM ALI, in north-eastern Algeria. The sedimentological points of view, the sediments are dominated by the sand fraction followed by the silt fraction; moderate concentrations of CaCO3 are the result of the dissolution of the surrounding limestone reliefs (Maastrichtian limestone). The morphoscopic observation of quartz grains with a dissecting microscope allows us to offer more or less significant changes, since they are often dull or sub-blunted. The results of the magnetic survey are consistent with those of the sedimentological study. The values of magnetic susceptibility are strong in the middle part of the stratigraphic section (just above the archaeological level) and decrease slightly at the top. Lower values are stored in the lower part. The dependence of frequency values of magnetic susceptibility (fd) are strong throughout the stratigraphic section and show the presence of a mixture of single-domain grain size (R), pseudo-single domain (PMD) and superparamagnetic (SP) (with a predominance of SP grains). The high concentration of SP grain size reveals the presence of significant soil formation during the implementation of the sediment
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">4</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Hanini, Amine</style></author><author><style face="normal" font="default" size="100%">Houla, Yassine</style></author><author><style face="normal" font="default" size="100%">DJAIZ, Foued</style></author><author><style face="normal" font="default" size="100%">Chairat, Imen</style></author><author><style face="normal" font="default" size="100%">Mabrouk Boughdiri</style></author><author><style face="normal" font="default" size="100%">Maamri, Ridha</style></author><author><style face="normal" font="default" size="100%">Zagrarni,Mohamed-Faouzi</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Characterization of Cenomanian-Turonian oxic facies in Tunisia: sequence stratigraphy and correlation of recorded bioevents</style></title><secondary-title><style face="normal" font="default" size="100%">Arabian Journal of Geosciences</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2021</style></year></dates><volume><style face="normal" font="default" size="100%">14</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	On the southwestern Tethyan Margin of Tunisia, the well-known anoxic black shale facies of the Cenomanian-Turonian transition contrasts with oxic fossiliferous carbonates, first characterized here as lateral equivalents. In terms of sequence stratigraphy, the analysis of four wisely sampled sections in Central and Southern Tunisia led to interpret these deposits as a transgressive interval (TST). This interval spans the&amp;nbsp;&lt;i&gt;Whiteinella archaeocretacea&lt;/i&gt;&amp;nbsp;Zone of foraminifera and is capped with a glauconite-rich highly bioturbated maximum flooding surface (MFS). In the reference section of Oued Bahloul and the Kalaat Senan area of North-Central Tunisia, these deposits overlay a Shelf Margin Wedge made of conglomeratic and bioclastic limestones. In South-Central and Southern Tunisia, the TST is characterized by the onset of oxic facies relaying laminated carbonates with local emergence surfaces. The analysis of both oxic and anoxic facies from the Cenomanian-Turonian transition allows identifying five successive bioevent markers, known elsewhere within the Tethyan domain: the extinction of the foraminifera genus&amp;nbsp;&lt;i&gt;Rotalipora&lt;/i&gt;&amp;nbsp;(or&amp;nbsp;&lt;i&gt;Thomasinella&lt;/i&gt;), the&amp;nbsp;&lt;i&gt;Heterohelix&lt;/i&gt;&amp;nbsp;shift, the&amp;nbsp;&lt;i&gt;Whiteinella&lt;/i&gt;&amp;nbsp;proliferation, the filament event, and the appearance of&amp;nbsp;&lt;i&gt;Helvetotruncana helvetica&lt;/i&gt;. Among these bioevents, the&amp;nbsp;&lt;i&gt;Heterohelix&lt;/i&gt;&amp;nbsp;shift coincides with the transgressive surface, while the filament event announces the maximal flooding surface. These Cenomanian-Turonian transition bioevents are of a particular relevance for regional and long-distance high-resolution correlations.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">RABAHI, Noureddine</style></author><author><style face="normal" font="default" size="100%">DJAIZ, Foued</style></author><author><style face="normal" font="default" size="100%">DEFAFLIA , Nabil</style></author><author><style face="normal" font="default" size="100%">GUASTALDI, Enrico</style></author><author><style face="normal" font="default" size="100%">AMROUNE, Abdelouahab</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">THE VERTICAL DISTRIBUTION OF THE ALLUVIAL CHEMO-FACIES OF BOUMERZOUG WADI, CONSTANTINE, NORTHEASTERN ALGERIA: PALEOENVEROMENTAL SIGNIFICANCE AND CLIMATE EVOLUTION</style></title><secondary-title><style face="normal" font="default" size="100%">Analele Universităţii din Oradea, Seria Geografie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2021</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://d1wqtxts1xzle7.cloudfront.net/84550251/auog.311108-865-libre.pdf?1650469151=&amp;response-content-disposition=inline%3B+filename%3DThe_Vertical_Distribution_of_the_Alluvia.pdf&amp;Expires=1663166053&amp;Signature=GgE6IslXDLa0uV9lBn--z69CxZVgU3Cu8BAoi2RqaTXm9w</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">31</style></volume><pages><style face="normal" font="default" size="100%">68-79</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	The authorities of Constantine city have been working on the redevelopment and calibration of the Rhumel and Boumerzoug wadis since 2015. The latter calebrage works caused great damage to the banks, thus affecting the Quaternary geological formations in place (alluvial terraces, flood plains). A multidisciplinary research project based on a geomorphological and sedimentological approach was quickly set up to create a scientific data base before their total destruction and loss of physical traces all along the wadis. The present study focuses on the sedimentological and geochemical analysis of the alluvial deposits of Boumerzoug wadi in order to describe the sediments, to reconstitute their nature, and to interpret both the climatic evolution and the paleo-environments of the region. Sedimentological and geochemical results confirm the succession of deposition cycles linked to progressive climate change.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">1</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Harizi, Khaled</style></author><author><style face="normal" font="default" size="100%">Menani, Mohamed-Redha</style></author><author><style face="normal" font="default" size="100%">Chabour, Nabil</style></author><author><style face="normal" font="default" size="100%">Labar, Sofiane</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Initial assessment of the groundwater flow and budget using Geographic Information System, MODFLOW-2005 and the FREEWAT modeling tool in Bouteldja coastal aquifer (Northern East of Algeria)</style></title><secondary-title><style face="normal" font="default" size="100%">Italian Journal of Groundwater ACQUE SOTTERRANEE</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2021</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.acquesotterranee.net/index.php/acque/article/view/511</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">10</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	The Bouteldja coastal aquifer is one of the most important groundwater resources in North eastern of Algeria. The region is under a sub-humid climate with an average rainfall of 600-880 mm/y. The unconfined aquifer is constituted of Quaternary sands formations. The hydrogeological characteristics were determined based on previous reports. A very important inflow recharges the sandy aquifer in the Southeastern boundary, in relation to a fault network system linking the aquifer and the Obeira Lake area. Another inflow is observed at the Southern boundary in relation to the exchanges with the alluvial aquifer of Bouteldja. The purpose of the present study is to provide an initial assessment of the groundwater flow and water budget of this aquifer. To achieve this goal, a one-layer groundwater flow numerical model was developed using the MODFLOW-2005 code and the FREEWAT software, using the available data. The model was run in steady state conditions. Calibration was achieved using the piezometric measurements of May 2018 as calibration target. After several trials of manual calibrations, the model successfully simulated the groundwater flows directions and heads. Calibration efforts lead to an acceptable concordance (for the purpose of this study) between the estimated and calculated hydraulic conductivity and piezometric heads, except at the Eastern border. The analyses of the simulated inflow budget shows that aside the rainfall infiltration, exchanges with surface water bodies, the adjoining alluvial aquifer and the fault system provide a relevant amount of water. This significant recharge needs additional investigations. This numerical modeling exercise using MODFLOW, the FREEWAT software and GIS reached the objective of a preliminary description of the groundwater flow and it represents an acceptable starting point for more thorough hydrodynamic characterization of the Bouteldja coastal aquifer.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">3</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Khadri, Rahma</style></author><author><style face="normal" font="default" size="100%">Brinis, Nafaa</style></author><author><style face="normal" font="default" size="100%">Abdelhamid Khedidja</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à l&amp;rsquo;étude des eaux souterraines exploitées dans la région deHammam Bradaa dans la wilaya de Guelma au Nord-Est Algérien.Géométrie de l&amp;rsquo;aquifère et suivi de la piézométrie</style></title><secondary-title><style face="normal" font="default" size="100%">The 3rd Integrated Water Resources Management Conference, GIRE’3 MOSTEFA BENBOULAID UNIVERSITY-BATNA 2- 15 DECEMBER</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2020</style></year></dates><pub-location><style face="normal" font="default" size="100%">Batna,Algeria</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Drias, Tarek</style></author><author><style face="normal" font="default" size="100%">Abdelhamid Khedidja</style></author><author><style face="normal" font="default" size="100%">Moufida Belloula</style></author><author><style face="normal" font="default" size="100%">Saadali, Badraddine</style></author><author><style face="normal" font="default" size="100%">Saibi, Hakim</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Groundwater modelling of the Tebessa-Morsott alluvial aquifer (northeasternAlgeria): A geostatistical approach</style></title><secondary-title><style face="normal" font="default" size="100%">Groundwater for Sustainable Development</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2020</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.1016/j.gsd.2020.100444</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">11</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	This paper studies aquifer's hydrodynamic behavior by combining a flow-simulation model with transmissivity optimization (cokriging) in order to provide an optimal management scheme for the groundwater aquifer. The use of a cokriging approach improves the transmissivity data which are insufficient for the database of the&amp;nbsp;groundwater flow&amp;nbsp;simulation model. The obtained results are then used to model the&amp;nbsp;groundwater flow&amp;nbsp;of the Tebessa-Morsott shallow aquifer, located in NE Algeria, under a steady and transient regime. The results of the model calibration for the steady-state (year 2010) show that the recharge by rainfall and leakage rate are similar compared to those calculated by the analytical approach, (84,354&amp;nbsp;m&lt;sup&gt;3&lt;/sup&gt;/day for the recharge and 36,986&amp;nbsp;m&lt;sup&gt;3&lt;/sup&gt;/day for pumped water flow rate). The results of the transient regime show the alluvial aquifer affected by large drawdowns reaching 40&amp;nbsp;m over 20 years (year 2030 scenario) due to increase in water exploitation from pumping wells to answer water needs of the Tebessa region.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Drias, Tarek</style></author><author><style face="normal" font="default" size="100%">Abdelhamid Khedidja</style></author><author><style face="normal" font="default" size="100%">Moufida Belloula</style></author><author><style face="normal" font="default" size="100%">Saadali, Badraddine</style></author><author><style face="normal" font="default" size="100%">Saibi, Hakim</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Groundwater modelling of the Tebessa-Morsott alluvial aquifer (northeastern Algeria): A geostatistical approach</style></title><secondary-title><style face="normal" font="default" size="100%">Groundwater for Sustainable Development</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2020</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.1016/j.gsd.2020.100444</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">11</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	This paper studies aquifer's hydrodynamic behavior by combining a flow-simulation model with transmissivity optimization (cokriging) in order to provide an optimal management scheme for the groundwater aquifer. The use of a cokriging approach improves the transmissivity data which are insufficient for the database of the&amp;nbsp;groundwater flow&amp;nbsp;simulation model. The obtained results are then used to model the&amp;nbsp;groundwater flow&amp;nbsp;of the Tebessa-Morsott shallow aquifer, located in NE Algeria, under a steady and transient regime. The results of the model calibration for the steady-state (year 2010) show that the recharge by rainfall and leakage rate are similar compared to those calculated by the analytical approach, (84,354&amp;nbsp;m&lt;sup&gt;3&lt;/sup&gt;/day for the recharge and 36,986&amp;nbsp;m&lt;sup&gt;3&lt;/sup&gt;/day for pumped water flow rate). The results of the transient regime show the alluvial aquifer affected by large drawdowns reaching 40&amp;nbsp;m over 20 years (year 2030 scenario) due to increase in water exploitation from pumping wells to answer water needs of the Tebessa region.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Boumaiza, Lamine</style></author><author><style face="normal" font="default" size="100%">Chesnaux, Romain</style></author><author><style face="normal" font="default" size="100%">Drias, Tarek</style></author><author><style face="normal" font="default" size="100%">Walter, Julien</style></author><author><style face="normal" font="default" size="100%">Huneau, Frédéric</style></author><author><style face="normal" font="default" size="100%">Garel, Emilie</style></author><author><style face="normal" font="default" size="100%">Knoeller, Kay</style></author><author><style face="normal" font="default" size="100%">Stumpp, Christine</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Identifying groundwater degradation sources in a Mediterranean coastal area experiencing significant multi-origin stresses</style></title><secondary-title><style face="normal" font="default" size="100%">Science of The Total Environment</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2020</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.1016/j.scitotenv.2020.141203</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">746</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	This study investigates the multiple contamination sources of a coastal Mediterranean aquifer in northeastern Algeria that is bordered by two rivers and neighboring densely populated areas. Hydrogeochemical and isotopic groundwater characterization is carried out, including the analyses of major elements, water stable isotopes δ&lt;sup&gt;2&lt;/sup&gt;H-H&lt;sub&gt;2&lt;/sub&gt;O and δ&lt;sup&gt;18&lt;/sup&gt;O-H&lt;sub&gt;2&lt;/sub&gt;O, and stable isotopes of nitrate δ&lt;sup&gt;15&lt;/sup&gt;N-NO&lt;sub&gt;3&lt;/sub&gt;&amp;nbsp;and δ&lt;sub&gt;18&lt;/sub&gt;O-NO&lt;sub&gt;3&lt;/sub&gt;, and then integrated into the history of land use over the study area. Groundwater nitrate concentrations ranging from 1.6 to 235&amp;nbsp;mg/L with a median value of 69&amp;nbsp;mg/L are evidence of the degradation of groundwater quality induced by&amp;nbsp;anthropogenic sources. The combined of δ&lt;sup&gt;15&lt;/sup&gt;N-NO&lt;sub&gt;3&lt;/sub&gt;&amp;nbsp;and δ&lt;sub&gt;18&lt;/sub&gt;O-NO&lt;sub&gt;3&lt;/sub&gt;&amp;nbsp;ratios showed that nitrate in groundwater is attributable to (i) the uncontrolled development of inadequate private sanitation systems over the study area, and (ii) the unsafe application of animal manure to fertilize crops. Very active&amp;nbsp;saltwater intrusion&amp;nbsp;is confirmed by several hydrogeochemical indicators. Interestingly, the intrusion mechanism appears to be more complex than a direct intrusion from the Mediterranean Sea. During the high-water period,&amp;nbsp;saltwater intrusion&amp;nbsp;may also originate from the two rivers bordering the aquifer, via upstream migration of seawater through the river mouths. The heavier ratios in δ&lt;sup&gt;2&lt;/sup&gt;H-H&lt;sub&gt;2&lt;/sub&gt;O and δ&lt;sup&gt;18&lt;/sup&gt;O-H&lt;sub&gt;2&lt;/sub&gt;O of surface water collected from the rivers suggest that water from the Mediterranean Sea is mixing with water in the rivers. Multi-source contamination not only contributes to complex chemical reactions within the aquifer, but also contributes, via the&amp;nbsp;cumulative effect&amp;nbsp;of the various sources, to affecting large parts of the study area. The present study may serve as a warning to the effect that historical land-use practices may exert seriously deleterious impacts on groundwater quality and greatly limit conditions for the sustainable management of Mediterranean coastal areas.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Hammadi, Aziza</style></author><author><style face="normal" font="default" size="100%">Brinis, Nafaa</style></author><author><style face="normal" font="default" size="100%">Djidel, Mohamed</style></author><author><style face="normal" font="default" size="100%">Chaa, Halima</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Hydrochemical assessment and groundwater quality using statistical approaches of the terminal complex aquifer in the region of Oued Righ (Algerian Sahara)</style></title><secondary-title><style face="normal" font="default" size="100%"> AGBIOL 2020. II International Agricultural, Biological &amp; Life Science Conference, 1-3 September 2020</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2020</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.cabidigitallibrary.org/doi/full/10.5555/20210298871</style></url></web-urls></urls><pub-location><style face="normal" font="default" size="100%"> Edirne, Turkey</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	Oued Righ valley is part of the northeastern Algerian Sahara, it is characterized by an arid desert climate with very high temperatures in summer. The Terminal Complex aquifer waters's in Oued Righ evoke serious problems related to the physical and the chemical quality; Larger variations in conductivity are observed that probably due to multiple geochemical processes; these waters which are highly mineralized and concentrated of some elements shown the higher value in recommended potable waters norms of Algeria.In this work, several hydrochemical and statistical approaches are using to demonstrate the correlation between the chemical composition of water of the Terminal Complex and lithology.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Drias, Tarek</style></author><author><style face="normal" font="default" size="100%">Abdelhamid Khedidja</style></author><author><style face="normal" font="default" size="100%">Moufida Belloula</style></author><author><style face="normal" font="default" size="100%">Badraddine, Saadali</style></author><author><style face="normal" font="default" size="100%">Saibi, Khedoudj</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Groundwater modelling of the Tebessa-Morsott alluvial aquifer (northeastern Algeria): A geostatistical approach</style></title><secondary-title><style face="normal" font="default" size="100%">Groundwater for Sustainable Development </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2020</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.sciencedirect.com/science/article/abs/pii/S2352801X1930311X</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">11</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">This paper studies aquifer's hydrodynamic behavior by combining a flow-simulation model with&amp;nbsp;&lt;a href=&quot;https://www.sciencedirect.com/topics/earth-and-planetary-sciences/transmissivity&quot; title=&quot;Learn more about transmissivity from ScienceDirect's AI-generated Topic Pages&quot;&gt;transmissivity&lt;/a&gt;&amp;nbsp;optimization (cokriging) in order to provide an optimal management scheme for the groundwater aquifer. The use of a cokriging approach improves the&amp;nbsp;&lt;a href=&quot;https://www.sciencedirect.com/topics/earth-and-planetary-sciences/transmissivity&quot; title=&quot;Learn more about transmissivity from ScienceDirect's AI-generated Topic Pages&quot;&gt;transmissivity&lt;/a&gt;&amp;nbsp;data which are insufficient for the database of the&amp;nbsp;&lt;a href=&quot;https://www.sciencedirect.com/topics/earth-and-planetary-sciences/groundwater-flow&quot; title=&quot;Learn more about groundwater flow from ScienceDirect's AI-generated Topic Pages&quot;&gt;groundwater flow&lt;/a&gt;&amp;nbsp;simulation model. The obtained results are then used to model the&amp;nbsp;&lt;a href=&quot;https://www.sciencedirect.com/topics/earth-and-planetary-sciences/groundwater-flow&quot; title=&quot;Learn more about groundwater flow from ScienceDirect's AI-generated Topic Pages&quot;&gt;groundwater flow&lt;/a&gt;&amp;nbsp;of the Tebessa-Morsott shallow aquifer, located in NE Algeria, under a steady and transient regime. The results of the model calibration for the steady-state (year 2010) show that the recharge by rainfall and&amp;nbsp;&lt;a href=&quot;https://www.sciencedirect.com/topics/earth-and-planetary-sciences/leakage&quot; title=&quot;Learn more about leakage from ScienceDirect's AI-generated Topic Pages&quot;&gt;leakage&lt;/a&gt;&amp;nbsp;rate are similar compared to those calculated by the analytical approach, (84,354&amp;nbsp;m&lt;sup&gt;3&lt;/sup&gt;/day for the recharge and 36,986&amp;nbsp;m&lt;sup&gt;3&lt;/sup&gt;/day for pumped water flow rate). The results of the transient regime show the alluvial aquifer affected by large drawdowns reaching 40&amp;nbsp;m over 20 years (year 2030 scenario) due to increase in water exploitation from pumping wells to answer water needs of the Tebessa region.</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Boumaiza, Lamine</style></author><author><style face="normal" font="default" size="100%">Chesnaux, Romain</style></author><author><style face="normal" font="default" size="100%">Drias, Tarek</style></author><author><style face="normal" font="default" size="100%">Walter, Julien</style></author><author><style face="normal" font="default" size="100%">Huneau, Frédéric</style></author><author><style face="normal" font="default" size="100%">Garel, Emilie</style></author><author><style face="normal" font="default" size="100%">Knoeller, Kay</style></author><author><style face="normal" font="default" size="100%">Stumpp, Christine</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Identifying groundwater degradation sources in a Mediterranean coastal area experiencing significant multi-origin stresses</style></title><secondary-title><style face="normal" font="default" size="100%">Science of The Total Environment </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2020</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.sciencedirect.com/science/article/abs/pii/S004896972034732X</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">746</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	This study investigates the multiple contamination sources of a coastal Mediterranean aquifer in northeastern Algeria that is bordered by two rivers and neighboring densely populated areas. Hydrogeochemical and isotopic groundwater characterization is carried out, including the analyses of major elements, water&amp;nbsp;&lt;a href=&quot;https://www.sciencedirect.com/topics/earth-and-planetary-sciences/stable-isotope&quot; title=&quot;Learn more about stable isotopes from ScienceDirect's AI-generated Topic Pages&quot;&gt;stable isotopes&lt;/a&gt;&amp;nbsp;δ&lt;sup&gt;2&lt;/sup&gt;H-H&lt;sub&gt;2&lt;/sub&gt;O and δ&lt;sup&gt;18&lt;/sup&gt;O-H&lt;sub&gt;2&lt;/sub&gt;O, and stable isotopes of nitrate δ&lt;sup&gt;15&lt;/sup&gt;N-NO&lt;sub&gt;3&lt;/sub&gt;&amp;nbsp;and δ&lt;sub&gt;18&lt;/sub&gt;O-NO&lt;sub&gt;3&lt;/sub&gt;, and then integrated into the history of land use over the study area. Groundwater nitrate concentrations ranging from 1.6 to 235&amp;nbsp;mg/L with a median value of 69&amp;nbsp;mg/L are evidence of the degradation of groundwater quality induced by&amp;nbsp;&lt;a href=&quot;https://www.sciencedirect.com/topics/earth-and-planetary-sciences/anthropogenic-source&quot; title=&quot;Learn more about anthropogenic sources from ScienceDirect's AI-generated Topic Pages&quot;&gt;anthropogenic sources&lt;/a&gt;. The combined of δ&lt;sup&gt;15&lt;/sup&gt;N-NO&lt;sub&gt;3&lt;/sub&gt;&amp;nbsp;and δ&lt;sub&gt;18&lt;/sub&gt;O-NO&lt;sub&gt;3&lt;/sub&gt;&amp;nbsp;ratios showed that nitrate in groundwater is attributable to (i) the uncontrolled development of inadequate private sanitation systems over the study area, and (ii) the unsafe application of animal manure to fertilize crops. Very active&amp;nbsp;&lt;a href=&quot;https://www.sciencedirect.com/topics/earth-and-planetary-sciences/saline-intrusion&quot; title=&quot;Learn more about saltwater intrusion from ScienceDirect's AI-generated Topic Pages&quot;&gt;saltwater intrusion&lt;/a&gt;&amp;nbsp;is confirmed by several hydrogeochemical indicators. Interestingly, the intrusion mechanism appears to be more complex than a direct intrusion from the Mediterranean Sea. During the high-water period, saltwater intrusion may also originate from the two rivers bordering the aquifer, via upstream migration of seawater through the river mouths. The heavier ratios in δ&lt;sup&gt;2&lt;/sup&gt;H-H&lt;sub&gt;2&lt;/sub&gt;O and δ&lt;sup&gt;18&lt;/sup&gt;O-H&lt;sub&gt;2&lt;/sub&gt;O of surface water collected from the rivers suggest that water from the Mediterranean Sea is mixing with water in the rivers. Multi-source contamination not only contributes to complex chemical reactions within the aquifer, but also contributes, via the&amp;nbsp;&lt;a href=&quot;https://www.sciencedirect.com/topics/earth-and-planetary-sciences/cumulative-effects&quot; title=&quot;Learn more about cumulative effect from ScienceDirect's AI-generated Topic Pages&quot;&gt;cumulative effect&lt;/a&gt;&amp;nbsp;of the various sources, to affecting large parts of the study area. The present study may serve as a warning to the effect that historical land-use practices may exert seriously deleterious impacts on groundwater quality and greatly limit conditions for the sustainable management of Mediterranean coastal areas.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Belgaid, Nassima</style></author><author><style face="normal" font="default" size="100%">Menani, Mohamed-Redha</style></author><author><style face="normal" font="default" size="100%">Bouhidel, Kamel-Eddine</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Elaboration of Bentonite layered double hydroxide composite (LDH-bentonite) to enhance adsorption of sulfide in water</style></title><secondary-title><style face="normal" font="default" size="100%">Séminaire International sur l′Hydrogéologie et l′Environnement SIHE 2019 Ouargla</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://dspace.univ-ouargla.dz/jspui/bitstream/123456789/24561/1/Belgaid%20Nassima.pdf</style></url></web-urls></urls><pub-location><style face="normal" font="default" size="100%">Ouargla, Algeria</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	Low cost bentonite clay was chemically modified using magnesium chloride in order to enhance its sulfide removal capacity. The incorporation of Co and Al into bentonite (MB). Batch adsorption experiments were conducted to study and optimize various operational parameters such as adsorbent dose, contact time, pH, and initial sulfide concentration. It was observed that the MB works effectively over wide range of pH and showed a maximum sulfide removal capacity of 2.26mgg−1 at an initial fluoride concentration of 5mg L−1, which is much better than the unmodified bentonite. Desorption study of MB suggest that almost all the loaded fluoride was desorbed (~97%) using 1M NaOH solution however maximum sulfide removal decreases from 95.47 to 73 (%) after regeneration. From the experimental results, it may be inferred that chemical modification enhances the sulfide removal efficiency of bentonite and it works as an effective
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Boudjema,  Abderrezak</style></author><author><style face="normal" font="default" size="100%">Guettaia, Sabrine</style></author><author><style face="normal" font="default" size="100%">Brinis, Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">STATISTICAL AND HYDROCHEMICAL CLASSIFICATION OF UNDERGROUND WATERS IN A MULTI-LAYER AQUIFER SYSTEM IN AN ARID ZONE :APPLICATION TO CHOTT EL GHARBI BASIN (EXTREME WEST OF ALGERIA)</style></title><secondary-title><style face="normal" font="default" size="100%">Journal of Fundamental and Applied Sciences</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.researchgate.net/profile/Nafaa-Brinis-2/publication/344543059_Statistical_and_hydrochemical_classification_of_underground_waters_in_a_multi-layer_aquifer_system_in_an_arid_zone_application_to_chott_el_gharbi_basin_extreme_west_of_algeria/links</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	The studied area, so called Chott El Gharbi shelters a multilayer aquifer system. The hydro-chemical tool shows that the results of the groundwater analyzes of the aquifer system of the Chott El Gharbi region revealed that they are sulphated-calcium and magnesian. Water infiltrated at the Bajo-Bathonian and Mio-Plio-Quaternary carbonate formations is enriched with HCO3- and SiO2 along its underground route. Also, the presence of a Triassic evaporitic formation or the Cenomano- Turonian argilo-gypsum formation enriches these waters with SO4 2- , Cl- , K+ , Mg2+, Na+ and Ca2+ . Thermodynamics has shown that these waters are under saturated evaporitic elements, which gives them a greater power of dissolution than that of carbonates which are in equilibrium or sometimes even supersaturated and tend to precipitate.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Kehiha Haifa</style></author><author><style face="normal" font="default" size="100%">Khetta Makhloufa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à l&amp;#39;étude géotechnique du viaduc de la penetrante Bir chouhada-Batnapénétrante Bir-Echouhada - Batna</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Zekiri Ahmed</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à l&amp;#39;étude géotechnique de la pénétrante  autoritière. Trançon Eleulma Djemila</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Basli Aleddine</style></author><author><style face="normal" font="default" size="100%">Aksa Nasreddine</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Cartographie de vulnérabilité de l&amp;#39;aquifère superficiel de Biska</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Mekhloufi Nadjet</style></author><author><style face="normal" font="default" size="100%">Bastal Dhaouia</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Suivi piézométrique et hydrochique de l&amp;#39;aquifère alluvionnaire de Ain Djasser</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Aichaoui Billal</style></author><author><style face="normal" font="default" size="100%">Abid Belgacem</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Le Turonien de Dj Boukezzez (ChaabetOuledChelih) : Caractérisation lithobiostratigraphique et interprétation paléoenvironnementale.</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Bessariani tahar</style></author><author><style face="normal" font="default" size="100%">Guettaoui Imed</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Coupe de Dj BouArif : Etude lithostratigraphique, sédimentologique et réflexions paléoenvironnementales à partir de l&amp;rsquo;étude de la faune et de la microfaune (Aurès, Batna).</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Slami Rafika</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Mise en Evidence de l&amp;#39;évènement anoxique océanique 2 (EAO-2) dans la région de Batna (NE, Algérie)</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://biblio.univ-annaba.dz/wp-content/uploads/2019/11/These-Slami-Rafika.pdf</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;div class=&quot;textLayer&quot; style=&quot;width:992px;height:1403px;&quot;&gt;
	&lt;span style=&quot;left:837.167px;top:63.6px;18.4px;sans-serif;transform:scaleX(0.949474);&quot;&gt;Résumé&lt;/span&gt;&lt;span style=&quot;left:141.84px;top:119.013px;20px;sans-serif;transform:scaleX(0.967493);&quot;&gt;Résumé&lt;/span&gt;&lt;span style=&quot;left:214.433px;top:119.013px;20px;sans-serif;&quot;&gt;:&lt;/span&gt;&lt;span style=&quot;left:177.433px;top:165.011px;20px;sans-serif;transform:scaleX(0.907355);&quot;&gt;La présente étude s’intéresse aux dépôts cénomano&lt;/span&gt;&lt;span style=&quot;left:591.717px;top:165.013px;20px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:598.317px;top:165.013px;20px;sans-serif;transform:scaleX(0.912758);&quot;&gt;turoniens, observables dans la région &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:188.013px;20px;sans-serif;transform:scaleX(0.916738);&quot;&gt;de Batna&lt;/span&gt;&lt;span style=&quot;left:213.033px;top:188.013px;20px;sans-serif;&quot;&gt;,&lt;/span&gt;&lt;span style=&quot;left:223.833px;top:188.011px;20px;sans-serif;transform:scaleX(0.934847);&quot;&gt;afin de définir la mise en évidence de l’évènement anoxique océanique 2 (EAO&lt;/span&gt;&lt;span style=&quot;left:869.367px;top:188.013px;20px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:875.967px;top:188.013px;20px;sans-serif;transform:scaleX(1.01227);&quot;&gt;2). &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:211.013px;20px;sans-serif;transform:scaleX(0.900573);&quot;&gt;Cette &lt;/span&gt;&lt;span style=&quot;left:192.433px;top:211.013px;20px;sans-serif;transform:scaleX(0.922909);&quot;&gt;région couvre deux domaines &lt;/span&gt;&lt;span style=&quot;left:458.483px;top:211.013px;20px;sans-serif;transform:scaleX(0.912445);&quot;&gt;paléogéographiques et structuraux : le préatlasique&lt;/span&gt;&lt;span style=&quot;left:141.84px;top:234.013px;20px;sans-serif;transform:scaleX(0.931316);&quot;&gt;(Monts de Bellezma&lt;/span&gt;&lt;span style=&quot;left:314.833px;top:234.013px;20px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:321.833px;top:234.013px;20px;sans-serif;transform:scaleX(0.911454);&quot;&gt;Batna) au N&lt;/span&gt;&lt;span style=&quot;left:426.683px;top:234.013px;20px;sans-serif;&quot;&gt;O&lt;/span&gt;&lt;span style=&quot;left:449.083px;top:234.013px;20px;sans-serif;transform:scaleX(0.910447);&quot;&gt;et l'atlasique &lt;/span&gt;&lt;span style=&quot;left:563.117px;top:234.013px;20px;sans-serif;transform:scaleX(0.907985);&quot;&gt;(Monts de l'Aurès) au SE. &lt;/span&gt;&lt;span style=&quot;left:789.167px;top:234.013px;20px;sans-serif;transform:scaleX(0.892962);&quot;&gt;Pour le faire,&lt;/span&gt;&lt;span style=&quot;left:141.84px;top:257.013px;20px;sans-serif;transform:scaleX(0.902415);&quot;&gt;une analyse sédimentologique, biostratigraphique et géochimique est réalisée sur deux coupes &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:280.013px;20px;sans-serif;transform:scaleX(0.945864);&quot;&gt;Thénièt El Manchar et Firmet Riche «&lt;/span&gt;&lt;span style=&quot;left:482.283px;top:280.013px;20px;sans-serif;transform:scaleX(1.00822);&quot;&gt;Dj Bou Arif&lt;/span&gt;&lt;span style=&quot;left:594.917px;top:280.013px;20px;sans-serif;transform:scaleX(0.918216);&quot;&gt;». Basées sur les ammonites et les &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:303.013px;20px;sans-serif;transform:scaleX(0.875237);&quot;&gt;foraminifères planctoniques, deux formations ont été définies&lt;/span&gt;&lt;span style=&quot;left:649.917px;top:303.013px;20px;sans-serif;transform:scaleX(0.893969);&quot;&gt;: (1) la Formati&lt;/span&gt;&lt;span style=&quot;left:777.567px;top:303.013px;20px;sans-serif;&quot;&gt;o&lt;/span&gt;&lt;span style=&quot;left:787.567px;top:303.013px;20px;sans-serif;transform:scaleX(0.855427);&quot;&gt;n des Marnes &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:326.013px;20px;sans-serif;transform:scaleX(0.929617);&quot;&gt;de Smail, subdivisée en quatre unités litho&lt;/span&gt;&lt;span style=&quot;left:517.883px;top:326.013px;20px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:524.483px;top:326.013px;20px;sans-serif;transform:scaleX(0.973285);&quot;&gt;stratigraphiques (IA, IB, IC, ID), datée du &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:349.011px;20px;sans-serif;transform:scaleX(0.929831);&quot;&gt;Cénomanien et (2) la base de la Formation des Dolomies de l’Oued Skhoun (unité, IIA) datée &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:372.011px;20px;sans-serif;transform:scaleX(0.948156);&quot;&gt;du Turonien inférieur. L’analyse qualitative et quantitative d&lt;/span&gt;&lt;span style=&quot;left:642.717px;top:372.013px;20px;sans-serif;&quot;&gt;e&lt;/span&gt;&lt;span style=&quot;left:651.517px;top:372.013px;20px;sans-serif;transform:scaleX(0.927028);&quot;&gt;s foraminifères (planctoniques &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:395.061px;20px;sans-serif;transform:scaleX(0.888316);&quot;&gt;et/ou benthiques), des ostracodes, l’étude du microfaciès et des marqueurs géochimiques, &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:418.061px;20px;sans-serif;transform:scaleX(0.974375);&quot;&gt;permet de reconstituer l’évolution du paléo&lt;/span&gt;&lt;span style=&quot;left:541.717px;top:418.063px;20px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:548.317px;top:418.063px;20px;sans-serif;transform:scaleX(0.91466);&quot;&gt;environnement et les variations paléo&lt;/span&gt;&lt;span style=&quot;left:890.967px;top:418.063px;20px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:141.84px;top:441.061px;20px;sans-serif;transform:scaleX(0.914609);&quot;&gt;bathymétriques au cours de l’intervalle stratigraphiq&lt;/span&gt;&lt;span style=&quot;left:562.317px;top:441.063px;20px;sans-serif;&quot;&gt;u&lt;/span&gt;&lt;span style=&quot;left:572.317px;top:441.063px;20px;sans-serif;transform:scaleX(0.951664);&quot;&gt;e concerné. Ainsi, les unités IA&lt;/span&gt;&lt;span style=&quot;left:824.767px;top:441.063px;20px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:831.567px;top:441.063px;20px;sans-serif;transform:scaleX(1.16068);&quot;&gt;IB&lt;/span&gt;&lt;span style=&quot;left:851.367px;top:441.063px;20px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:858.167px;top:441.063px;20px;sans-serif;transform:scaleX(0.973938);&quot;&gt;IC et &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:464.061px;20px;sans-serif;transform:scaleX(0.9502);&quot;&gt;la partie inférieure de l’unité ID (Cénomanien) sont dominées par des associations de fora&lt;/span&gt;&lt;span style=&quot;left:891.167px;top:464.063px;20px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:141.84px;top:487.061px;20px;sans-serif;transform:scaleX(0.907777);&quot;&gt;minifères benthiques agglutinés et des carapaces entières d’ostracodes, témoignant d’un &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:510.063px;20px;sans-serif;transform:scaleX(0.908447);&quot;&gt;milieu de plate&lt;/span&gt;&lt;span style=&quot;left:260.633px;top:510.063px;20px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:267.233px;top:510.061px;20px;sans-serif;transform:scaleX(0.916132);&quot;&gt;forme et d’un faib&lt;/span&gt;&lt;span style=&quot;left:412.483px;top:510.063px;20px;sans-serif;&quot;&gt;l&lt;/span&gt;&lt;span style=&quot;left:418.083px;top:510.061px;20px;sans-serif;transform:scaleX(0.928217);&quot;&gt;e hydrodynamisme. Les calcaires supérieurs de l’unité IC et &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:533.061px;20px;sans-serif;transform:scaleX(0.929366);&quot;&gt;inférieurs de l’unité ID sont marqués par la présence de rudistes traduisant une reduction&lt;/span&gt;&lt;span style=&quot;left:877.767px;top:533.063px;20px;sans-serif;transform:scaleX(0.880933);&quot;&gt;du &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:556.061px;20px;sans-serif;transform:scaleX(0.921854);&quot;&gt;milieu de sédimentation et une augmentation de l’hydrodynamisme. Dans ces dépôts, les &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:579.063px;20px;sans-serif;transform:scaleX(0.894683);&quot;&gt;associations m&lt;/span&gt;&lt;span style=&quot;left:262.233px;top:579.063px;20px;sans-serif;&quot;&gt;o&lt;/span&gt;&lt;span style=&quot;left:272.233px;top:579.063px;20px;sans-serif;transform:scaleX(0.883442);&quot;&gt;ntrent une diversité spécifique faible à moy&lt;/span&gt;&lt;span style=&quot;left:637.317px;top:579.063px;20px;sans-serif;transform:scaleX(0.851944);&quot;&gt;enne et une abondance plus ou &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:602.063px;20px;sans-serif;transform:scaleX(0.912045);&quot;&gt;moins élevée de foraminifères benthiques, témoignant de conditions trophiques et &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:625.061px;20px;sans-serif;transform:scaleX(0.917098);&quot;&gt;d’oxygénation considérées comme normales. Les termes sommitaux de l’unité ID (sommet du &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:648.063px;20px;sans-serif;transform:scaleX(0.917778);&quot;&gt;Cénomanien)&lt;/span&gt;&lt;span style=&quot;left:255.233px;top:648.061px;20px;sans-serif;transform:scaleX(0.930604);&quot;&gt;et l’unité IIA (base du Turonien) marquent, quant à eux, une évolution vers des &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:671.097px;20px;sans-serif;transform:scaleX(0.893131);&quot;&gt;conditions plus profondes, comme le montre la succession stan&lt;/span&gt;&lt;span style=&quot;left:679.917px;top:671.097px;20px;sans-serif;transform:scaleX(0.878418);&quot;&gt;dard des événements déjà &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:694.094px;20px;sans-serif;transform:scaleX(0.917714);&quot;&gt;reconnus en Afrique du nord, à savoir : l’abondance de foraminifères planctoniques, la &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:717.097px;20px;sans-serif;&quot;&gt;p&lt;/span&gt;&lt;span style=&quot;left:151.84px;top:717.097px;20px;sans-serif;&quot;&gt;r&lt;/span&gt;&lt;span style=&quot;left:158.44px;top:717.094px;20px;sans-serif;transform:scaleX(0.90375);&quot;&gt;ésence de ‘filaments’ et une réduction drastique de la faune d’ostracodes. &lt;/span&gt;&lt;span style=&quot;left:177.433px;top:763.094px;20px;sans-serif;transform:scaleX(0.936151);&quot;&gt;D’une manière générale, la sédimentation des deux formations dans les deux domaines &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:786.094px;20px;sans-serif;transform:scaleX(0.897595);&quot;&gt;représente une séquence qui évolue d’un environnement de plate&lt;/span&gt;&lt;span style=&quot;left:662.917px;top:786.097px;20px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:669.517px;top:786.097px;20px;sans-serif;transform:scaleX(0.918249);&quot;&gt;forme externe distale à celui &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:809.097px;20px;sans-serif;&quot;&gt;d&lt;/span&gt;&lt;span style=&quot;left:151.84px;top:809.094px;20px;sans-serif;&quot;&gt;’&lt;/span&gt;&lt;span style=&quot;left:158.44px;top:809.097px;20px;sans-serif;transform:scaleX(0.876958);&quot;&gt;une plate&lt;/span&gt;&lt;span style=&quot;left:235.633px;top:809.097px;20px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:242.233px;top:809.094px;20px;sans-serif;transform:scaleX(0.902523);&quot;&gt;forme moyenne, avec une phase régressive. Cette séquence s’achève avec le &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:832.094px;20px;sans-serif;transform:scaleX(0.898618);&quot;&gt;retour aux conditions profondes concomitantes d’une hausse eustatique et dépôt de sédiments &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:855.094px;20px;sans-serif;transform:scaleX(0.905802);&quot;&gt;pélagiques caractérisant un intervalle transgressif (IT) et s’inscrit dans le c&lt;/span&gt;&lt;span style=&quot;left:774.967px;top:855.097px;20px;sans-serif;&quot;&gt;y&lt;/span&gt;&lt;span style=&quot;left:784.567px;top:855.097px;20px;sans-serif;transform:scaleX(0.886885);&quot;&gt;cle eustatique &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:878.094px;20px;sans-serif;transform:scaleX(0.909097);&quot;&gt;majeur téthysien de troisième ordre. L’évolution séquentielle et paléogéographique des &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:900.897px;20px;sans-serif;transform:scaleX(0.860378);&quot;&gt;dépôts cénomaniens et turoniens inférieurs de la région de Batna dépendent intimement du &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:923.947px;20px;sans-serif;transform:scaleX(0.90297);&quot;&gt;contexte structural de la région.&lt;/span&gt;&lt;span style=&quot;left:167.033px;top:969.947px;20px;sans-serif;transform:scaleX(0.909695);&quot;&gt;En outre, les courbes isotop&lt;/span&gt;&lt;span style=&quot;left:389.083px;top:969.947px;20px;sans-serif;&quot;&gt;i&lt;/span&gt;&lt;span style=&quot;left:394.683px;top:969.947px;20px;sans-serif;transform:scaleX(0.897402);&quot;&gt;ques du, carbone (&lt;/span&gt;&lt;span style=&quot;left:541.517px;top:969.944px;20px;sans-serif;&quot;&gt;Δ&lt;/span&gt;&lt;span style=&quot;left:554.317px;top:968.227px;13.4px;sans-serif;transform:scaleX(0.971429);&quot;&gt;13&lt;/span&gt;&lt;span style=&quot;left:567.717px;top:969.944px;20px;sans-serif;transform:scaleX(0.94237);&quot;&gt;C) et de l’oxygène (&lt;/span&gt;&lt;span style=&quot;left:727.917px;top:969.944px;20px;sans-serif;&quot;&gt;Δ&lt;/span&gt;&lt;span style=&quot;left:740.717px;top:968.227px;13.4px;sans-serif;transform:scaleX(0.971429);&quot;&gt;18&lt;/span&gt;&lt;span style=&quot;left:754.367px;top:969.947px;20px;sans-serif;transform:scaleX(0.898125);&quot;&gt;O) des carbonates &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:992.947px;20px;sans-serif;transform:scaleX(0.922887);&quot;&gt;mettent en évidence des anomalies isotopiques relatives aux modifications paléo&lt;/span&gt;&lt;span style=&quot;left:891.167px;top:992.947px;20px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:141.84px;top:1015.95px;20px;sans-serif;transform:scaleX(0.917037);&quot;&gt;environnementales. Les données du &lt;/span&gt;&lt;span style=&quot;left:457.883px;top:1015.94px;20px;sans-serif;&quot;&gt;Δ&lt;/span&gt;&lt;span style=&quot;left:470.683px;top:1014.23px;13.4px;sans-serif;transform:scaleX(0.971429);&quot;&gt;13&lt;/span&gt;&lt;span style=&quot;left:484.283px;top:1015.95px;20px;sans-serif;transform:scaleX(0.940311);&quot;&gt;C et celles du COT indiquent une productivité &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:1038.95px;20px;sans-serif;transform:scaleX(0.87944);&quot;&gt;primaire faible. Les données d&lt;/span&gt;&lt;span style=&quot;left:393.083px;top:1038.95px;20px;sans-serif;&quot;&gt;u&lt;/span&gt;&lt;span style=&quot;left:410.283px;top:1038.94px;20px;sans-serif;&quot;&gt;Δ&lt;/span&gt;&lt;span style=&quot;left:423.083px;top:1037.23px;13.4px;sans-serif;transform:scaleX(0.971429);&quot;&gt;18&lt;/span&gt;&lt;span style=&quot;left:436.683px;top:1038.95px;20px;sans-serif;transform:scaleX(0.851647);&quot;&gt;O, quant à elles, indiquent une augmentation des paléo&lt;/span&gt;&lt;span style=&quot;left:891.167px;top:1038.95px;20px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:141.84px;top:1061.94px;20px;sans-serif;transform:scaleX(0.912284);&quot;&gt;températures, cause principale du déclenchement de l’EAO 2. Ces interprétations paléo&lt;/span&gt;&lt;span style=&quot;left:890.967px;top:1061.95px;20px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:141.84px;top:1084.94px;20px;sans-serif;transform:scaleX(0.906523);&quot;&gt;environnementales s’accordent avec les données con&lt;/span&gt;&lt;span style=&quot;left:590.317px;top:1084.95px;20px;sans-serif;transform:scaleX(0.886902);&quot;&gt;nues du contexte paléogéographique &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:1107.95px;20px;sans-serif;transform:scaleX(0.879169);&quot;&gt;régional et mettent en e&lt;/span&gt;&lt;span style=&quot;left:329.483px;top:1107.95px;20px;sans-serif;&quot;&gt;x&lt;/span&gt;&lt;span style=&quot;left:339.683px;top:1107.95px;20px;sans-serif;transform:scaleX(0.911768);&quot;&gt;ergue les spécificités téthysiennes. &lt;/span&gt;
&lt;/div&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Bouhadeb Chamsseddine</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Evaluation du transport solide au niveau du bassin versant d&amp;#39;Oued Bounamoussa et ses incidences sur l&amp;#39;envasement du barrage de Chefia</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Djenba Samir</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caracterisation hydrochimiques des eaux du continental intercalaire et complexe terminal et les problèmes d&amp;rsquo;irrigationà la vallée d&amp;rsquo;oued Righ  </style></title><secondary-title><style face="normal" font="default" size="100%">Second International Symposium Water Resources and Environmental Impact Assessment  in North Africa (WREIANA 2019) March 25 -27 , 2019-Sousse, Tunisia</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Dekakra Mouna</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">Abdelhamid Khedidja</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Impact de la pollution agricole sur la qualité des eaux de l&amp;#39;aquifère de Teleghma</style></title><secondary-title><style face="normal" font="default" size="100%">Second International Symposium Water Resources and Environmental Impact Assessment  in North Africa (WREIANA 2019) March 25 -27 , 2019-Sousse, Tunisia</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">B. Saadali</style></author><author><style face="normal" font="default" size="100%">H. Zerouk</style></author><author><style face="normal" font="default" size="100%">Drias Tarek</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Physicochemical and organic quality assessment of Mexa and Bougous waters and its suitability for agricultural use</style></title><secondary-title><style face="normal" font="default" size="100%">Second International Symposium Water Resources and Environmental Impact Assessment  in North Africa (WREIANA 2019) March 25 -27 , 2019-Sousse, Tunisia</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Drias Tarek</style></author><author><style face="normal" font="default" size="100%">Abdelhamid Khedidja</style></author><author><style face="normal" font="default" size="100%">Belloula Moufida</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Assessment of the capacitive function of Shallow aquifer using probabilistic and deterministic approaches (geostatistics - 3D model)</style></title><secondary-title><style face="normal" font="default" size="100%">Second International Symposium Water Resources and Environmental Impact Assessment  in North Africa (WREIANA 2019) March 25 -27 , 2019-Sousse, Tunisia</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.wreiana2019.com</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Boumaiza Lamine</style></author><author><style face="normal" font="default" size="100%">Chabour Nabil</style></author><author><style face="normal" font="default" size="100%">Drias Tarek</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Reviewing the potential anthropogenic sources of groundwater contamination - Case study of the expanding urban area of Taleza in Algeria.</style></title><secondary-title><style face="normal" font="default" size="100%">the 72nd Canadian Geotechnical Conference, St-John’s, (September 29 to October 02, 2019)Newfoundland, Canada</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.iaeg.info › Congresses</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Boumaiza Lamine</style></author><author><style face="normal" font="default" size="100%">Chabour Nabil</style></author><author><style face="normal" font="default" size="100%">Drias Tarek</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">there still a chance to save the groundwater in Taleza aquifer ?</style></title><secondary-title><style face="normal" font="default" size="100%">AGC-AMC-AIH - GAC-MAC-IAH Conference | Quebec City</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://gacmac-quebec2019.ca</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Abdelhamid Khedidja</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderrahmane</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Quality assessment of shallow groundwater for irrigation purposes in Tadjenanet &amp;ndash; Chelghoum Laid area (Eastern Algeria) ISSN / e-ISSN 1571-5124 / 1814-2060</style></title><secondary-title><style face="normal" font="default" size="100%">International Journal of River Basin Management</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.researchgate.net/publication/333708795_Quality_Assessment_of_Shallow_Groundwater_for_irrigation_purposes_in_Tadjenanet_-_Chelghoum_Laid_area_Eastern_Algeria</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">The groundwater quality of Tadjenanet- Chelghoum Laid Semi-arid region was assessed for irrigation suitability; where the intensity of salinization process depends on soil characteristics, water quality, irrigation practices and in particular the inefficiency of the drainage system. The drought of the last decade has created an agricultural deficit due to high evapotranspiration, influencing the water salinity. To achieve this assessment, thirty groundwater samples were collected at identical locations from deeper wells. The physicochemical parameters such as, pH, electrical conductivity (EC), total hardness (TH), Ca²⁺, Mg²⁺, Na⁺, K⁺, HCO3⁻, SO4²⁻, Cl⁻ and NO3⁻ have been studied. Obtained results were measured and interpreted with different irrigation indexes like EC, sodium percentage (SP), sodium adsorption ratio (SAR), residual sodium carbonate (RSC), permeability index (PI) and Kelly’s ratio (KR). These parameters combined allowed to conclude that the quality of groundwater was roughly suitable for irrigation.</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Benmansour Sana</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Les carbonates marins campano-maastrichtiens dans les gorges d&amp;#39;El Kantara, Aurès occidental, Algérie : control sur la biodiversité, les types de microfaciès et l&amp;#39;architecture des dépôts</style></title><secondary-title><style face="normal" font="default" size="100%">Premier Colloque sur la géologie des Bassins Sédimentaires Maghrébins FSTGAT-USTHB 01 au 03-10-2019</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Benmansour Sana</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à l&amp;#39;étude du Crétacé supérieur- Tertiaire : cas de Dj. Arhane, bassin decGhassira (Aurès central, NE Algérien)</style></title><secondary-title><style face="normal" font="default" size="100%">Premier Colloque sur la géologie des Bassins Sédimentaires Maghrébins FSTGAT-USTHB 01 au 03-10-2019</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Benmansour Sana</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude lithostratigraphique et analyse séquentielle de la région de Maafa- synclinal de Béni Fedhala (Aurès, Atlas Saharien Oriental)</style></title><secondary-title><style face="normal" font="default" size="100%">Premier Colloque sur la géologie des Bassins Sédimentaires Maghrébins FSTGAT-USTHB 01 au 03-10-2019</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">Lamouri Bachir</style></author><author><style face="normal" font="default" size="100%">A. Bousahaba</style></author><author><style face="normal" font="default" size="100%">Belalite Halima</style></author><author><style face="normal" font="default" size="100%">Touansa Rachid</style></author><author><style face="normal" font="default" size="100%">Khanfer Soumia</style></author><author><style face="normal" font="default" size="100%">Marred Manal</style></author><author><style face="normal" font="default" size="100%">Chairat Imen</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation géologique et apport de la géophysique pour la mobilisation des ressources hydriques dans le  bassin de Gadaine (Ain Yagout, Algérie NE)</style></title><secondary-title><style face="normal" font="default" size="100%">1st  National Seminar on GeoSciences and Environment SGSE 19 October 23-24, Tamanrasset, </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Marred Manal</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Boushaba Abdellah</style></author><author><style face="normal" font="default" size="100%">Lamouri Bachir</style></author><author><style face="normal" font="default" size="100%">Kherchouche Adila</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Essai de caracterisation lithostratigraphiques et paléoenvironnementdes formations Eocène du bassin de Ghassira : Coupe  du Kef El-Arous (Aurès Central, NE Algérien)</style></title><secondary-title><style face="normal" font="default" size="100%">1st  National Seminar on GeoSciences and Environment SGSE 19 October 23-24, Tamanrasset</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Khanfer Soumia</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à l&amp;rsquo;étude du basin Néogène Batna-ain Touta, limite aurès-Monts de Belezma</style></title><secondary-title><style face="normal" font="default" size="100%">1st  National Seminar on GeoSciences and Environment SGSE 19 October 23-24, Tamanrasset</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Chairat Imen</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Boughdiri Mabrouk</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Reconsideration of the Cenomanian-Turonian stratigraphics units in the Tebessa region (Algero-TunisienConfines): Petroleum implications</style></title><secondary-title><style face="normal" font="default" size="100%">1st  National Seminar on GeoSciences and Environment SGSE 19 October 23-24, Tamanrasset</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">MENNANI Mohamed Redha</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Hydrochemical Characteristics under current condition exploitation usingstatistics methods : case of the Zana- Roknia plain, North east of Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">1st  National Seminar on GeoSciences and Environment SGSE 19 October 23-24, Tamanrasset</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Lamouri Bachir</style></author><author><style face="normal" font="default" size="100%">Boughdiri Mabrouk</style></author><author><style face="normal" font="default" size="100%">Touansa Rachid</style></author><author><style face="normal" font="default" size="100%">Boushaba Abdellah</style></author><author><style face="normal" font="default" size="100%">Mrred Manel</style></author><author><style face="normal" font="default" size="100%">Khaner Soumia</style></author><author><style face="normal" font="default" size="100%">Chairat Imen</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Les terrasses fluviatiles quaternaires de Oued El Gourzi et oued El Hay (Batna, NE Algérie) : Sédimentologie Caractéristiques de l&amp;rsquo;Environnement</style></title><secondary-title><style face="normal" font="default" size="100%">1st  National Seminar on GeoSciences and Environment SGSE 19 October 23-24, Tamanrasset</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Defaflia Nabil</style></author><author><style face="normal" font="default" size="100%">A. Benkhedda</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">A. Cerif</style></author><author><style face="normal" font="default" size="100%">M. Djerab-Ruault</style></author><author><style face="normal" font="default" size="100%">L. Gouadia</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Les dépots Miocène de la région de Tébessa (Nord-est Algérien) : Analyses sédimentologiques, Micropaléontologiques et Paléoenvironnement </style></title><secondary-title><style face="normal" font="default" size="100%">Premier Colloque sur la géologie des Bassins Sédimentaires Maghrébins FSTGAT-USTHB 01 au 03-10-2019</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Nadji Hocine</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">M. Hmmimed</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation géologique et apport de la géophysique pour la mobilisation des ressources hydriques dans le bassin d&amp;rsquo;El Mather.</style></title><secondary-title><style face="normal" font="default" size="100%">Premier Colloque sur la géologie des Bassins Sédimentaires Maghrébins FSTGAT-USTHB 01 au 03-10-2019</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">R. Touansa</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Boughdiri Mabrouk</style></author><author><style face="normal" font="default" size="100%">I. Cherif</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">La lithostratigraphie de l&amp;rsquo;Ammonitico Rosso de Djebel Kasserou (Monts de Batna)</style></title><secondary-title><style face="normal" font="default" size="100%">Premier Colloque sur la géologie des Bassins Sédimentaires Maghrébins FSTGAT-USTHB 01 au 03-10-2019</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">M. Marred</style></author><author><style face="normal" font="default" size="100%">A. Kherchouche</style></author><author><style face="normal" font="default" size="100%">Benmansour Sana</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à l&amp;rsquo;étude du crétacé supérieur-Tertiaire: Cas de Djebel Arhane, bassin de Ghassira (Aurès Central, NE Algérien.</style></title><secondary-title><style face="normal" font="default" size="100%">Premier Colloque sur la géologie des Bassins Sédimentaires Maghrébins FSTGAT-USTHB 01 au 03-10-2019</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">S. Khanfer</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Lamouri Bachir</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Evolution tectono-sédimentaire du bassin néogène de Batna-Ain Touta, limite Aurès-Monts de Belezma</style></title><secondary-title><style face="normal" font="default" size="100%">Premier Colloque sur la géologie des Bassins Sédimentaires Maghrébins FSTGAT-USTHB 01 au 03-10-2019</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Benmansour Sana</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">The Campanian-Maastrichtian series of Dj. Gaâga (Tebessa, NE of Algeria) : quantitative and qualitative analysis and palaeoenvironmental interpretation</style></title><secondary-title><style face="normal" font="default" size="100%">7. INTERNANATIONAL EARTH SCIENCE COLLOQUIUM ON THE AEGEAN REGION. Izmir/ Turkiye. 7-11 october 2019</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Benmansour Sana</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Lithostratigraphical and sedimentological characterization of the Aptian formation on the Northern flank of Dj Bou Arif (NE of Algeria)</style></title><secondary-title><style face="normal" font="default" size="100%">7. INTERNANATIONAL EARTH SCIENCE COLLOQUIUM ON THE AEGEAN REGION. Izmir/ Turkiye. 7-11 october 2019</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fouad Djaiz</style></author><author><style face="normal" font="default" size="100%">Defaflia Nabil</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">Bachir Lamouri</style></author><author><style face="normal" font="default" size="100%">Mabrouk Boughdiri</style></author><author><style face="normal" font="default" size="100%">Halima Belalite</style></author><author><style face="normal" font="default" size="100%">Boushaba Abdellah</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Geological Characterization and contibution of Geophysics to the mobilization of water resources in the Ain Djasser basin (South-Sétifien, Algeria NE), ISSN 2052-3408</style></title><secondary-title><style face="normal" font="default" size="100%">The Euro-arab Organization for Environment and Water  and Desert Researches, International Journal of Environment and Water </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.researchgate.net/publication/330104660_Caracterisation_geologique_et_apport_de_la_geophysique_pour_la_mobilisation_des_ressources_hydriques_dans_le_bassin_d'Ain_Djasser_Sud-Setifien_Algerie_NE_Geological_Characterization_and_contribution_o</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Vol. 8</style></volume><pages><style face="normal" font="default" size="100%">pp. 66-77</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Le bassin d'Ain Djasser fait partie de l'ensemble Sud-Sétifien. Ce dernier est représenté par une plaine inter-montagneuse appartenant au bassin des hauts plateaux constantinois. Il est caractérisé par un climat de type méditerranéen. L'hydrologie tributaire du relief est la conséquence directe des eaux de surface et de la fonte des neiges. La synthèse géologique montre un domaine allochtone résultant d'une histoire polyphasée associant les tectoniques atlasique et alpine. Ce dernier est caractérisé par des séries sédimentaires carbonatées colmaté par d'abondantes formations terrigènes. L'alimentation de l'eau souterraine des différentes nappes profondes à semi-profondes provient essentiellement de l'infiltration des eaux de pluies. Ce cortège de roche forme une nappe libre et captive, par endroit recoupée par des forages à des profondeurs de 178 à 330 m, fournissant un débit moyen de 15 l/s. L'interprétation des coupes géoélectriques du bassin montrent, (i) des formations alluvionnaires du mio-plio-quaternaire de quelques dizaines de mètres qui forment un bon aquifère superficiel, (ii) des calcaires fissurés du jurassico-crétacé dont le toit est atteint à des profondeurs variables est un aquifère captif. L'influence d'accidents entre les différents blocs rend possible une éventuelle alimentation des aquifères entres eux. L'analyse litho-stratigraphique montre que le substratum et la couverture sédimentaire ne présentent pas de grandes variations latérales. Par contre, nous observons au niveau des sondages une variation dans l'épaisseur et la lithologie des couches, essentiellement au niveau de la formation du remplissage mio-plio-quaternaire. L'objectif de cette étude réside pour l'essentiel, dans la mobilisation des ressources en eaux superficielles et souterraine pour leurs exploitations dans les domaines agricoles et l'élevage, en vue d'une utilisation rationnelle et planifiée de cet élément vital qu'est l'eau</style></abstract><issue><style face="normal" font="default" size="100%">Issue3</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Analyse statistique des paramètres hydrochimiques du continental intercalaire de la région de biskra - sud-est algérien</style></title><secondary-title><style face="normal" font="default" size="100%">1st national seminar on geosciences and environment SGSE'19, Tamanrasset, Algérie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Chafou Nasereddine</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation hydrochimique et aptitude à l&amp;#39;irrigation des eaux du (CI) dans la région de Touggourt -ouargla- Oued Righ au sud algérien</style></title><secondary-title><style face="normal" font="default" size="100%">1st national seminar on geosciences and environment SGSE'19, Tamanrasset, Algérie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Chafou Nasereddine</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Analyse statistique des paramètres hydrochimiques du continental intercalaire de la région de biskra - sud-est algérien</style></title><secondary-title><style face="normal" font="default" size="100%">1st national seminar on geosciences and environment SGSE'19, Tamanrasset, Algérie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation hydrochimique et aptitude à l&amp;#39;irrigation des eaux du (CI) dans la région de Touggourt -ouargla- Oued Righ au sud algérien</style></title><secondary-title><style face="normal" font="default" size="100%">1st national seminar on geosciences and environment SGSE'19, Tamanrasset, Algérie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Mekoussi Adel</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Identification des paramètres responsables de la minéralisation des sources d&amp;#39;eau utilisées pour l&amp;#39;irrigation dans le synclinal de BOUZINA, Nord est algérien</style></title><secondary-title><style face="normal" font="default" size="100%">Seminaire international sur l'hydrogéologie et l'environnement , Ouargla Algerie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Identification des paramètres responsables de la minéralisation des sources d&amp;#39;eau utilisées pour l&amp;#39;irrigation dans le synclinal de BOUZINA, Nord est algérien</style></title><secondary-title><style face="normal" font="default" size="100%">Seminaire international sur l'hydrogéologie et l'environnement , Ouargla Algerie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Identification des aquifères par les méthodes géophysiques. Cas du système aquifère de hammam bradaa nord-est de guelma. Algérie</style></title><secondary-title><style face="normal" font="default" size="100%">Colloque sur le géologie des bassins sédimentaires Maghrebins Alger, Algérie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Azizi Yacine</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">Boucenna Fatih</style></author><author><style face="normal" font="default" size="100%">Ag Maatallah Lamine</style></author><author><style face="normal" font="default" size="100%">Bouaam Med Lamine</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation de potentialité aquifère du socle cristallin par les apports de la télédétection et de SIG (région de Tamanrasset)</style></title><secondary-title><style face="normal" font="default" size="100%">1er Séminaire National sur les géosciences et l'environnement SGSE'2019</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Azizi Yacine</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">Boumazbeur Abderrahmane</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Collapse susceptibility mapping for Karst sinkholes in Cheria area, NE Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">1er Séminaire National sur les géosciences et l'environnement SGSE'2019</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Rihani Abla</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Hydrogeology of montain basin, cas of O. Labiod, North Eastern of Algreia</style></title><secondary-title><style face="normal" font="default" size="100%">15 th ICWRE - Antalya, Turkey, 25-28 Oct </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Boudjema A</style></author><author><style face="normal" font="default" size="100%">Guettaia Sabrine</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">statistical and hydrochemical classification of underground waters in a multi-layer aquifer system in an arid zone: application to chott el gharbi basin (extreme west of algeria), ISSN: 1112-9867 </style></title><secondary-title><style face="normal" font="default" size="100%">Journal of Fundamental and Applied Sciences</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><volume><style face="normal" font="default" size="100%">volume 11</style></volume><pages><style face="normal" font="default" size="100%">pp.786-803</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><issue><style face="normal" font="default" size="100%">issue 2</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Belouanas Hamza</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Characterization on Contentinetal Intercalaire Aquifer (CI) in the Tinrhert East Area-Illizi basin on the Algerian-Libyan Border, June, ISSN / e-ISSN: 2305 - 7068 / 1674-6767 </style></title><secondary-title><style face="normal" font="default" size="100%">Journal of groundwater science and engineering. </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://gwse.iheg.org.cn/EN/abstract/abstract367.shtml</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">vol 7</style></volume><pages><style face="normal" font="default" size="100%">pp.115-132</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">This paper addresses the characterization of the Continental Intercalaire aquifer (CI) in the Tinrhert-East area of Illizi Basin on the Algerian-Libyan border, which belongs to the SASS1 system, one of the biggest transboundary aquifers in the world. This study concerns a superficies of 4 300 km2. On the basis of Mud Logging borehole data conducted in this part of the aquifer, a realistic characterization of the aquifer was done. The thickness of the CI aquifer varies from 300 m in the south to 700 m in the north, and the depth ranges from 180 m to 320 m. The interpretation of the logs showed that the aquifer is characterized by a maximum net thickness in its southwestern part (more than 600 m), the porosity is very high, ranging from 30% in the west to 24% at the Libyan borders, the permeability is low to medium around 10-5 m/s, and the maximum transmissivity values of about 8×10-3 m2/s were recorded at the center of the study area. The depth of water varies from 235 m to 312 m, and the water flows from south to north, in accordance with the general direction observed in the CI aquifer in the Northern Sahara Aquifer System (SASS). The porosity values obtained from the interpretation of the sonic and density logs permit to estimate the water reserves of this aquifer considered fossil, at thresholds much higher than what was considered until now.</style></abstract><issue><style face="normal" font="default" size="100%">n°2</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Baaguigui  Samra</style></author><author><style face="normal" font="default" size="100%">Rahmoun Aicha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">La limite Crétacé/ Tertiaire dans la région de Menaa : caractérisation paléontologique et sédimentologique</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Khouaked Khadidja</style></author><author><style face="normal" font="default" size="100%">Rahmoune Amar</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Le Cénomanien de Chaabet Ouled Chelih : Sédimentologie et paléoenvironnements (L&amp;rsquo;ensemble Aurès-Bellezma).</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Benabbes.L</style></author><author><style face="normal" font="default" size="100%">Beda.S</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à l&amp;rsquo;étude hydrogéologique de la vallée de Manaa. W Batna</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Labed.E</style></author><author><style face="normal" font="default" size="100%">Harrouz.A</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à l&amp;rsquo;étude hydrogéologique de la région de Djamaa (W) El-Oued</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Reghais.A</style></author><author><style face="normal" font="default" size="100%">Maachi.F</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à l&amp;rsquo;étude du dimensionnement des périmètres de protection du lac du barrage de fontaine des gazelles (Wilaya de Biskra).</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Djemmal Samir</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude des sources thermominérales de la région de Sétif dans leur contexte structural</style></title><secondary-title><style face="normal" font="default" size="100%">Département des Sciences de la Terre</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.pnst.cerist.dz/detail.php?id=49416/</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Dans ce contexte, la présente étude vient se greffer à d’autres travaux de recherche (mémoires de Magister et thèses de Doctorat), et ce pour compléter les travaux entrepris déjà dans ce domaine à travers les sources thermominérales de la Wilaya de Sétif. Les premières recherches scientifiques menées sur les eaux thermales restent toujours d’actualité et présentent un intérêt indéniable à plus d’un titre. En effet ces études basées sur des apports scientifiques spécialisés, ont permis de comprendre le phénomène du thermalisme (qui a été jusqu’a un passé récent considéré par la population comme phénomène surnaturel) et de définir l’origine des eaux dites thermales ainsi que leurs zones d’alimentation et leurs processus d’acquisition de la température et de la minéralité. A signaler que la région d’étude a fait l’objet d’études géologiques par J.M Vila (1980) dans sa thèse de doctorat d’état “La chaine alpine d’Algérie orientale et les confins algéro-tunisiens”, où il a attribué le caractère d’allochtonie. Nous avons pensé alors qu’une étude des sources thermales de la région de Sétif pourra étayer les résultats de la géophysique et infirmer ou confirmer le caractère d’allochtonie attribué à cet ensemble. A partir de cela, nous allons essayer de mieux comprendre l’origine des eaux dites thermominérales (Froides et chaudes) ainsi que leurs zones d’alimentation et leurs processus d’acquisition de la température et de la minéralité et d’optimiser l'interprétation des analyses physico-chimiques en utilisant des moyens d’investigation appropriés. Le programme d’action pour la réalisation de ce travail doit répondre aux préoccupations suivantes : -Quel est l’état actuel de la qualité chimique des eaux souterraines de la région étudiée -Quels sont les mécanismes physico-chimiques régissant l’évolution des éléments chimiques dans le temps et dans l’espace (processus d’acquisition de la température et de la minéralité)? -Quels sont les processus d’acquisition des températures en profondeur des différents points d’eau chaude en utilisant des géothermomètres chimiques, comme indicateurs de la thermalité des gisements d’eaux. Afin de répondre à ces préoccupations, nous allons adopter la méthodologie suivante : -Etude du cadre naturel et hydrodynamique en relation avec le chimisme du milieu -Etude des paramètres physiques et chimiques de l'eau. -Etude des dépendances et relations entre les divers paramètres physico-chimiques de l'eau. -Etude des mécanismes d'acquisition de la température et de la minéralisation des eaux thermales et leurs origines. Pour concrétiser ce programme de travail, un suivi saisonnier des mesures physicochimiques sera effectué sur le terrain ainsi que des prélèvements d’échantillons d’eaux destinés aux analyses chimiques en éléments majeurs, mineurs. L’analyse des résultats ainsi obtenus sera développée à travers les deux parties constituant cette thèse. Première partie CHAPITRE I : Synthèse géologique de l’aire d’étude Elle reste d’une grande importance, dans le domaine du thermalisme nous décrirons les limites géographiques de la région de Sétif et nous examinerons ensuite la géologie et l’hydrogéologie qui portera sur l’étude des principales phases tectoniques, et plus particulièrement le système de la fracturation permettant l’émergence des eaux chaudes ; ainsi que la définition des différents aquifères dans le contexte lithostratigraphique, structural, géophysique et hydrogéologique. CHAPITRE II : hydroclimatologie Elle a pour objet d’étudier les facteurs importants comme la température de l’air pour définir les limites de la thermalité de la région et les précipitations qui conditionnent le bilan hydrologique et la recharge des aquifères. Elle permettra également la classification de la zone concernée sur la base d’indices climatiques et d’établir les principaux éléments du bilan hydrique qui est d’une importance capitale Deuxième partie CHAPITRE I : hydrochimie Cette partie essentielle dans notre travail de recherches, reposera sur le traitement des données des différentes analyses chimiques aussi bien les éléments majeurs que mineurs (fer, manganèse fluor, iode etc...) et la relation existante entre eux. En particulier la teneur en fer dans les eaux de Hammam Guergour. L’interprétation et l’exploitation de ces analyses permettront d’aboutir aux origines géologiques des eaux thermominérales (froides et chaudes), mais aussi d'avoir une idée sur la nature des formations lithologiques traversées par ces eaux et leur dynamique. CHAPITRE II : Géothermométrie Dans ce chapitre nous tenterons d’estimer les températures des eaux en profondeur des différentes sources thermales en utilisant divers géothermomètres chimiques, comme indicateurs des températures minimales et maximales au droit de l’aquifère. Sachant que la plupart des méthodes utilisées reposent sur les teneurs des eaux de certains éléments caractéristiques tels que : silice, calcium, sodium, potassium et carbonates</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Flux azoté : origine et devenir dans les eaux souterraines, cas de la région de Zana-est Algérien</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://docplayer.fr/66130950-Flux-azote-dans-les-eaux-souterraines-origine-et-devenir-cas-de-la-plaine-de-zana-est-algerien.html</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;span style=&quot;left:153.44px;top:886.724px;16.6px;sans-serif;transform:scaleX(0.930848);&quot;&gt;Nous avons essayé, par ce travail, d’apporter &lt;/span&gt;&lt;span style=&quot;left:461.683px;top:886.724px;16.6px;sans-serif;transform:scaleX(0.925995);&quot;&gt;une contribution à l’étudier les aquifères de la plaine de Zana, et &lt;/span&gt;&lt;span style=&quot;left:94.4px;top:905.724px;16.6px;sans-serif;transform:scaleX(0.930534);&quot;&gt;d’évaluer les risques de la pollution liée au flux azoté.&lt;/span&gt;&lt;span style=&quot;left:461.283px;top:905.726px;16.6px;sans-serif;transform:scaleX(0.916208);&quot;&gt;La plaine de Zana fait partie du bassin versant des hauts plateaux &lt;/span&gt;&lt;span style=&quot;left:94.4px;top:924.926px;16.6px;sans-serif;transform:scaleX(0.881629);&quot;&gt;constantinois et plus précisément du sous bassin versant Merdj&lt;/span&gt;&lt;span style=&quot;left:534.483px;top:924.924px;16.6px;sans-serif;transform:scaleX(0.993349);&quot;&gt;a Zana, qui s’étend sur une superficie de 369 Km² &lt;/span&gt;&lt;span style=&quot;left:94.4px;top:944.126px;16.6px;sans-serif;transform:scaleX(0.937879);&quot;&gt;environ.&lt;/span&gt;&lt;span style=&quot;left:154.24px;top:944.124px;16.6px;sans-serif;transform:scaleX(0.916627);&quot;&gt;L’étude de la géologie en association avec les données de la géophysique &lt;/span&gt;&lt;span style=&quot;left:653.917px;top:944.124px;16.6px;sans-serif;transform:scaleX(0.924105);&quot;&gt;met en évidence l’existence de deux &lt;/span&gt;&lt;span style=&quot;left:94.4px;top:963.324px;16.6px;sans-serif;transform:scaleX(0.930902);&quot;&gt;formations. La première formation, de surface d’âge Mio&lt;/span&gt;&lt;span style=&quot;left:478.883px;top:963.326px;16.6px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:484.283px;top:963.326px;16.6px;sans-serif;transform:scaleX(1.00029);&quot;&gt;Plio&lt;/span&gt;&lt;span style=&quot;left:511.483px;top:963.326px;16.6px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:516.883px;top:963.326px;16.6px;sans-serif;transform:scaleX(0.905731);&quot;&gt;Quaternaire formée par des&lt;/span&gt;&lt;span style=&quot;left:705.117px;top:963.326px;16.6px;sans-serif;transform:scaleX(0.932367);&quot;&gt;niveaux de sable, de gravier, &lt;/span&gt;&lt;span style=&quot;left:94.4px;top:982.526px;16.6px;sans-serif;transform:scaleX(0.897641);&quot;&gt;de calcaire lacustre et des intercalations argileuses. La deuxième formation, elle est carbonatée et formée &lt;/span&gt;&lt;span style=&quot;left:94.4px;top:1001.77px;16.6px;sans-serif;transform:scaleX(0.898747);&quot;&gt;essentiellement par des calcaires du Crétacé inférieur et du Jurassique supérieur de l’ensemble sud sétifien et du &lt;/span&gt;&lt;span style=&quot;left:94.4px;top:1020.78px;16.6px;sans-serif;transform:scaleX(0.871202);&quot;&gt;pa&lt;/span&gt;&lt;span style=&quot;left:110.2px;top:1020.78px;16.6px;sans-serif;transform:scaleX(0.884534);&quot;&gt;rautochtone aurésien. Le recouvrement de surface atteint dans &lt;/span&gt;&lt;span style=&quot;left:536.683px;top:1020.78px;16.6px;sans-serif;transform:scaleX(0.914269);&quot;&gt;certains&lt;/span&gt;&lt;span style=&quot;left:593.917px;top:1020.77px;16.6px;sans-serif;transform:scaleX(0.920676);&quot;&gt;endroits les 150m d’épaisseur notamment au &lt;/span&gt;&lt;span style=&quot;left:94.4px;top:1039.98px;16.6px;sans-serif;transform:scaleX(0.928527);&quot;&gt;milieu de la plaine et une faible épaisseur au voisinage des massifs. Quant aux formations carbonatées elles ont 350m &lt;/span&gt;&lt;span style=&quot;left:94.4px;top:1059.17px;16.6px;sans-serif;transform:scaleX(0.928288);&quot;&gt;d’épaisseur.&lt;/span&gt;&lt;span style=&quot;left:181.633px;top:1059.18px;16.6px;sans-serif;transform:scaleX(0.897404);&quot;&gt;La géomorph&lt;/span&gt;&lt;span style=&quot;left:273.633px;top:1059.18px;16.6px;sans-serif;transform:scaleX(0.876295);&quot;&gt;ologie, montre que notre bassin est allongé, il a une altitude moyenne de 935m et il est &lt;/span&gt;&lt;span style=&quot;left:94.4px;top:1078.38px;16.6px;sans-serif;transform:scaleX(0.911269);&quot;&gt;caractérisé par un relief modéré et de pente douce.&lt;/span&gt;&lt;span style=&quot;left:445.083px;top:1078.38px;16.6px;sans-serif;transform:scaleX(0.91083);&quot;&gt;Le réseau hydrographique est pe&lt;/span&gt;&lt;span style=&quot;left:664.317px;top:1078.38px;16.6px;sans-serif;transform:scaleX(0.8965);&quot;&gt;t développer et de type endoréique &lt;/span&gt;&lt;span style=&quot;left:94.4px;top:1097.58px;16.6px;sans-serif;transform:scaleX(0.912155);&quot;&gt;avec un écoulement temporaire.&lt;/span&gt;&lt;span style=&quot;left:314.833px;top:1097.57px;16.6px;sans-serif;transform:scaleX(0.948408);&quot;&gt;L’étude climatolo&lt;/span&gt;&lt;span style=&quot;left:434.483px;top:1097.57px;16.6px;sans-serif;transform:scaleX(0.925348);&quot;&gt;gique a montré que la région d’étude a un climat semi aride avec un &lt;/span&gt;&lt;span style=&quot;left:94.4px;top:1116.58px;16.6px;sans-serif;transform:scaleX(0.928126);&quot;&gt;bilan hydrologique déficitaire.&lt;/span&gt;&lt;span style=&quot;left:302.033px;top:1116.57px;16.6px;sans-serif;transform:scaleX(0.918641);&quot;&gt;L’aperçu hydrogéologique de la plaine montre que les formations du Crétacé inférieur et &lt;/span&gt;&lt;span style=&quot;left:94.4px;top:1135.78px;16.6px;sans-serif;transform:scaleX(0.938576);&quot;&gt;du Jurassique supérieur peuvent offrir des possibilités aquifères tr&lt;/span&gt;&lt;span style=&quot;left:579.517px;top:1135.78px;16.6px;sans-serif;transform:scaleX(0.926902);&quot;&gt;ès intéressantes de même que la formation &lt;/span&gt;&lt;span style=&quot;left:94.4px;top:1154.98px;16.6px;sans-serif;transform:scaleX(0.914193);&quot;&gt;superficielle, elle présente des potentialités aquifères non négligeables. La piézométrie montre une convergence vers les &lt;/span&gt;&lt;span style=&quot;left:94.4px;top:1174.18px;16.6px;sans-serif;transform:scaleX(0.899782);&quot;&gt;dépressions de Merdja de Zana et le Chott Saboun, qui représentent des exutoires naturels de&lt;/span&gt;&lt;span style=&quot;left:717.717px;top:1174.18px;16.6px;sans-serif;transform:scaleX(0.900906);&quot;&gt;la nappe.&lt;/span&gt;&lt;span style=&quot;left:94.4px;top:1193.37px;16.6px;sans-serif;transform:scaleX(0.945974);&quot;&gt;L’étude hydrochimique &lt;/span&gt;&lt;span style=&quot;left:261.033px;top:1193.37px;16.6px;sans-serif;transform:scaleX(0.965555);&quot;&gt;a permis d’attribuer l’origine évaporitique aux &lt;/span&gt;&lt;span style=&quot;left:591.317px;top:1193.38px;16.6px;sans-serif;transform:scaleX(0.888911);&quot;&gt;éléments Na&lt;/span&gt;&lt;span style=&quot;left:677.117px;top:1190.94px;10.8px;sans-serif;&quot;&gt;+&lt;/span&gt;&lt;span style=&quot;left:683.117px;top:1193.38px;16.6px;sans-serif;transform:scaleX(0.920956);&quot;&gt;, Mg&lt;/span&gt;&lt;span style=&quot;left:717.517px;top:1190.94px;10.8px;sans-serif;&quot;&gt;+&lt;/span&gt;&lt;span style=&quot;left:723.717px;top:1190.94px;10.8px;sans-serif;&quot;&gt;+&lt;/span&gt;&lt;span style=&quot;left:729.717px;top:1193.38px;16.6px;sans-serif;transform:scaleX(1.03688);&quot;&gt;, K&lt;/span&gt;&lt;span style=&quot;left:753.117px;top:1190.94px;10.8px;sans-serif;&quot;&gt;+&lt;/span&gt;&lt;span style=&quot;left:759.117px;top:1193.38px;16.6px;sans-serif;transform:scaleX(0.999074);&quot;&gt;, Cl&lt;/span&gt;&lt;span style=&quot;left:786.167px;top:1190.94px;10.8px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:789.767px;top:1193.38px;16.6px;sans-serif;&quot;&gt;,&lt;/span&gt;&lt;span style=&quot;left:800.967px;top:1193.38px;16.6px;sans-serif;transform:scaleX(0.991662);&quot;&gt;SO&lt;/span&gt;&lt;span style=&quot;left:822.167px;top:1201.14px;10.8px;sans-serif;&quot;&gt;4&lt;/span&gt;&lt;span style=&quot;left:827.567px;top:1190.94px;10.8px;sans-serif;transform:scaleX(0.9);&quot;&gt;--&lt;/span&gt;&lt;span style=&quot;left:834.767px;top:1193.38px;16.6px;sans-serif;transform:scaleX(0.865714);&quot;&gt;, quant à &lt;/span&gt;&lt;span style=&quot;left:94.4px;top:1212.57px;16.6px;sans-serif;transform:scaleX(0.971494);&quot;&gt;l’élément HCO&lt;/span&gt;&lt;span style=&quot;left:197.833px;top:1220.34px;10.8px;sans-serif;&quot;&gt;3&lt;/span&gt;&lt;span style=&quot;left:203.233px;top:1210.14px;10.8px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:206.833px;top:1220.34px;10.8px;sans-serif;transform:scaleX(0.933333);&quot;&gt;, &lt;/span&gt;&lt;span style=&quot;left:219.033px;top:1212.58px;16.6px;sans-serif;transform:scaleX(0.965818);&quot;&gt;il est &lt;/span&gt;&lt;span style=&quot;left:257.433px;top:1212.58px;16.6px;sans-serif;transform:scaleX(0.914006);&quot;&gt;issu des formations carbonatées&lt;/span&gt;&lt;span style=&quot;left:472.683px;top:1212.58px;16.6px;sans-serif;transform:scaleX(1.03067);&quot;&gt;. &lt;/span&gt;&lt;span style=&quot;left:487.683px;top:1212.57px;16.6px;sans-serif;transform:scaleX(0.927595);&quot;&gt;Les deux compagnes d’analyses effectuées montrent que les &lt;/span&gt;&lt;span style=&quot;left:94.4px;top:1231.57px;16.6px;sans-serif;transform:scaleX(0.886271);&quot;&gt;eaux issues de&lt;/span&gt;&lt;span style=&quot;left:202.833px;top:1231.57px;16.6px;sans-serif;transform:scaleX(0.980411);&quot;&gt;l’aquifère superficiel et de l’aquifère karstique ont le même faciès hydrochimique qui est de type &lt;/span&gt;&lt;span style=&quot;left:94.4px;top:1250.77px;16.6px;sans-serif;transform:scaleX(0.908723);&quot;&gt;chloruré et sulfaté magnésien, ce qui témoigne de l’existence d’une interaction probable entre les deux aquifères&lt;/span&gt;</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Drias Tarek</style></author><author><style face="normal" font="default" size="100%">Abdelhamid Khedidja</style></author><author><style face="normal" font="default" size="100%">Belloula Moufida</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Proposal for a new method for assessing the vulnerability of aquifers to contamination, ISSN 1737-3638</style></title><secondary-title><style face="normal" font="default" size="100%">3rd International Conference on Integrated Environmental Management for Sustainable Development &quot;ICIEM 2018&quot; , May 02 to 05, 2018.  Sousse, Tunisia</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%"> www.iciem-conference.com</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>47</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fouad Djaiz</style></author><author><style face="normal" font="default" size="100%">Defaflia Nabil</style></author><author><style face="normal" font="default" size="100%">Bachir Lamouri</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">Boushaba Abdellah</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">TERRASSES FLUVIATILES QUATERNAIRES DE L&amp;#39;OUED EL HAY (BATNA, NE ALGÉRIE): SÉDIMENTOLOGIE ET CARACTÉRISTIQUES DE L&amp;#39;ENVIRONNEMENT SÉDIMENTAIRE.</style></title><secondary-title><style face="normal" font="default" size="100%">4ème Colloque International les Géosciences au service du Développement durable (2018)  Tébessa, Algérie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.researchgate.net/publication/330038660_TERRASSES_FLUVIATILES_QUATERNAIRES_DE_L'OUED_EL_HAY_BATNA_NE_ALGERIE_SEDIMENTOLOGIE_ET_CARACTERISTIQUES_DE_L'ENVIRONNEMENT_SEDIMENTAIRE</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Une étude stratigraphique et sédimentologique a été réalisée sur une terrasse alluviale de la région d'Oued El Hay, au sud de Batna (NE Algérie). Les structures sédimentaires observées sont principalement des zones d'érosion, des zones inondables, des figures en biseau et des variations d'épaisseur associées à des joints de stratification. Du point de vue sédimentologique, les sédiments sont dominés par des fractions argilo-limono-sableuses, suivies par des fractions de gravier et de cailloux. Les teneurs modérées en CaCO3 résultent de la dissolution des reliefs calcaires à proximité (calcaire crétacé) associée à l'augmentation de la température et l'humidité du milieu. L'observation morphoscopique de grains de quartz avec une loupe binoculaire permet d'offrir une évolution plus ou moins importante, car ils sont souvent émoussés ou sous-arrondis. L'étude sédimentologique a été réalisée sur 16 échantillons prélevés systématiquement du haut vers le bas de la coupe stratigraphique. L'examen de la taille brute de la fraction inférieure à 2 mm a permis d'individualiser 03 niveaux dans des couches sédimentaires, certaines fractions grossières riches (gravier, cailloux et blocs) alternant avec des couches riches en sable et en limon. Le pourcentage de fraction d'argile est dominant et reste pratiquement constant presque tout au long de la section stratigraphique.</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Defaflia Nabil</style></author><author><style face="normal" font="default" size="100%">Lamouri Bachir</style></author><author><style face="normal" font="default" size="100%">Boushaba Abdellah</style></author><author><style face="normal" font="default" size="100%">Chairat. I</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Quaternary fluviatile terraces of the Oued El Gourzi (Batna, NE Algeria): sedimentology and characteristics of the depositional environment</style></title><secondary-title><style face="normal" font="default" size="100%">1ST CONFERENCES OF THE ARABIAN JOURNAL OF GEOSCIENCES (CAJC) (2018) Hammamet, Tunisie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Defaflia Nabil</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">Lamouri Bachir</style></author><author><style face="normal" font="default" size="100%">Boughdiri Mabrouk</style></author><author><style face="normal" font="default" size="100%">Belalite Halima</style></author><author><style face="normal" font="default" size="100%">Boushaba Abdellah</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Geological Characterization and contibution of Geophysics to the mobilization of water resources in the ain djasser basin (South-Sétifien, Algeria NE)</style></title><secondary-title><style face="normal" font="default" size="100%">The Euro-arab Organization for Environment,Water  and Desert Researches, (2018)   Antalya, Turquie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">Menani, Mohamed-Redha</style></author><author><style face="normal" font="default" size="100%">Fouad Djaiz</style></author><author><style face="normal" font="default" size="100%">Halima Belalite</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">The impact of the mobilization of water resources in semi-arid areas on sustainable development the case of Timgad Basin northeastern of Algeria</style></title><secondary-title><style face="normal" font="default" size="100%"> Advances in Sustainable and Environmental Hydrology, Hydrogeology, Hydrochemistry and Water Resources </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://link.springer.com/chapter/10.1007/978-3-030-01572-5_83</style></url></web-urls></urls><pages><style face="normal" font="default" size="100%">pp.355-357 </style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">A hill reservoir research project aims, among other perspectives, to improve the regional agriculture potential through irrigation of small areas. For such a project, the feasibility study for a given area is fundamental before the establishment of any related applied research works. This paper is of a socio-economic relevance for the Timgad region (NE Algeria) as the presented results consist of a contribution of both socio-economic operators and policy makers. In the study area, water resources are closely related to the regional geology and the main objectives of the establishment of the Foum-Toub hill reservoir is to promote the irrigation of its plain, regulate the flow of the Foum-Toub creek and minimize the silting of the Koudiet Lemdaour dam. The selected sites for the construction of this work are characterized by an impermeable bedrock. Loose material, favorable to serve as borrow areas, can be supplied from the surrounding depressions where sandstone can also be used for the dike construction.</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fouad Djaiz</style></author><author><style face="normal" font="default" size="100%">Defaflia Nabil</style></author><author><style face="normal" font="default" size="100%">Bachir Lamouri</style></author><author><style face="normal" font="default" size="100%">Boushaba Abdellah</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Quaternary fluviatile terraces of the Oued El Gourzi (Batna, NE Algeria): sedimentology and characteristics of the depositional</style></title><secondary-title><style face="normal" font="default" size="100%">Advances in Science, Technology &amp; Innovation </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://link.springer.com/chapter/10.1007/978-3-030-01452-0_79</style></url></web-urls></urls><pages><style face="normal" font="default" size="100%">pp 331-334 </style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Field observations and sedimentological analyses of alluvial terraces of the O. Gourzi (Batna, NE Algeria) lead us to consider sediments as dominated by clayey and silty-sandy fractions overlain by gravel and calcareous coarser fractions. Moderate CaO&lt;sub&gt;3&lt;/sub&gt; contents would have resulted from the dissolution of the nearby carbonate relieves. They are mainly composed of Maastrichtian limestones. The distribution of the mineral fraction led us to identify 07 levels including horizons of coarse fractions alternating with layers rich in sand and silt with a roughly constant clay fraction through the stratigraphic column. Kurtosis values, frequency histograms of a prokurtic type, rarily mesokurtic, mark a constant power mode for the transport agent. Classification indices indicate poorly- to moderately sorted material, indicating a turbiditic depositional environment. Quartz grain nature and morphoscopy refer to Miocene sandstones as a potential origin. The ferruginous coating is due to the initiating pedogenesis.</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Slami Rafika</style></author><author><style face="normal" font="default" size="100%">Salmi Laouar Sihem</style></author><author><style face="normal" font="default" size="100%">Bruno Ferré</style></author><author><style face="normal" font="default" size="100%">Riadh Aouissi</style></author><author><style face="normal" font="default" size="100%">Fatiha Kechid-Benkherouf</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Biostratigraphie, Géochimie et réponse des composantes microfauniques aux variations nvironnementales au passage Cénomanien-Turonien à Thniet El Manchar (Monts de Belezma, Batna, NE Algérie)</style></title><secondary-title><style face="normal" font="default" size="100%">Estudios Geológicos intitulé </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.researchgate.net/publication/326130603_Biostratigraphie_geochimie_et_reponse_des_composantes_microfauniques_aux_variations_environnementales_au_passage_Cenomanien-Turonien_a_Theniet_El_Manchar_Monts_de_Bellezma_Batna_NE_Algerie</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">74</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">[fr] La présente étude livre une analyse biostratigraphique et géochimique des dépôts cénomano-turoniens de la région Thénièt El Manchar, située dans les Monts de Bellezma-Batna, et leur évolution verticale. Une coupe (TM), épaisse de 180 m, est décrite dans ce secteur. Elle correspond à la Formation des Marnes de Smail, subdivisée en quatre unités litho-stratigraphiques (IA, IB, IC, ID), datée du Cénomanien grâce à la présence d’ammonites et de corail, et à la base de la Formation des Dolomies de l’Oued Skhoun (unité, IIA), datée de la base du Turonien au moyen de foraminifères planctoniques. L’analyse qualitative et quantitative des foraminifères (planctoniques et/ou benthiques), des ostracodes et des marqueurs géochimiques, permet de reconstituer l’évolution du paléo-environnement et les variations paléo-bathymétriques au cours de l’intervalle stratigraphique concerné. Ainsi, les unités IA-IB-IC et la partie inférieure de l’unité ID (Cénomanien) sont dominées par des associations de foraminifères benthiques agglutinés et des carapaces entières d’ostracodes, témoignant d’un milieu de plate-forme et d’un faible hydrodynamisme. Dans ces dépôts, les associations montrent une diversité spécifique faible à moyenne et une abondance plus ou moins élevée, témoignant de conditions trophiques et d’oxygénation considérées comme normales. Les derniers termes de l’unité ID (sommet du Cénomanien) et l’unité IIA (base du Turonien) marquent, quant à eux, une évolution vers des conditions plus profondes, comme le montre la succession standard des événements déjà reconnus en Afrique du nord, à savoir: l’abondance de foraminifères planctoniques, la présence de ‘filaments’ et une réduction drastique de la faune d’ostracodes. En outre, les courbes isotopiques du carbone (δ13C) et de l’oxygène (δ18O) des carbonates mettent en évidence des anomalies isotopiques relatives aux modifications paléo-environnementales. Les données du δ13C et celles du COT indiquent une productivité primaire faible. Les données du δ18O, quant à elles, indiquent une augmentation des paléo-températures, cause principale du déclenchement de l’EAO 2. Ces interprétations paléo-environnementales s’accordent avec les données connues du contexte paléogéographique régional et mettent en exergue les spécificités téthysiennes.</style></abstract><issue><style face="normal" font="default" size="100%">1</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Approche hydrogéologique des plaines de Gadaine et Zana-chott saboun (Wilaya de Batna, Nord est algérien)</style></title><secondary-title><style face="normal" font="default" size="100%">4eme colloque international : les géosciences au service du développement durable Tebessa, Algerie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Ait Mohand Said Meriem</style></author><author><style face="normal" font="default" size="100%">Bouhidel Kamel</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Le colmatage des membranes d&amp;#39;osmose inverse en dessalment d&amp;#39;eau : étude de l&amp;#39;ihibition de la précipitation de CaCO3 par Zn++</style></title><secondary-title><style face="normal" font="default" size="100%">Colloque International de Chimie CIC 5, Batna, Algérie, 04-06 décembre 2018</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Ait Mohand Said Meriem</style></author><author><style face="normal" font="default" size="100%">Bouhidel Kamel</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Coexistence effect of some ions on the nanofiltration quality</style></title><secondary-title><style face="normal" font="default" size="100%">5ème séminaire international sur l'eau et l'environnement, Chlef, 20-22 novembre 2018</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Belgaid Nassima</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">Bouhidel Kamel</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Synthetisis of  ZnO Bentonite as photocatalysis to degrade cationic yellow dye</style></title><secondary-title><style face="normal" font="default" size="100%">2nd International symposium on catalysis , Tlemcen, 1-3 Octobre 2018</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Belgaid Nassima</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">Bouhidel Kamel</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Valorisation de matériaux géologiques dans l&amp;#39;industrie de l&amp;#39;eau</style></title><secondary-title><style face="normal" font="default" size="100%">1er séminaire maghrébin sur  l'eau et l'environnement dans les zones arides, Ouargla, 23-25 avril 2018</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Belgaid Nassima</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">Bouhidel Kamel</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Synthetisis of Inorganic/organic modified Bentonite and its application for textile dye removal from water</style></title><secondary-title><style face="normal" font="default" size="100%">Colloque International de Chimie CIC 5, Batna, Algérie, 04-06 décembre 2018</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Belgaid Nassima</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Elaboration of Al-Bent, Fe-Bent, CTAB Bent,, AL-CTAB-Bent and Fe-CTAB-Bent from algerian Bentonite clay to adsorb cationic textiles dyes</style></title><secondary-title><style face="normal" font="default" size="100%">International Water Forum Conference, Hammamet, Tunisie, 19-21 Mars </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Rihani Abla</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Approche hydrogéologie et isotopique pour la connaissance de l&amp;#39;origine de la salinisation des eaux souterraines d&amp;#39;Oued Labiod, NE algérien </style></title><secondary-title><style face="normal" font="default" size="100%">4ème colloque international sur les géosciences et le développement durable, Tébessa,  Nov </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Belalit Halima</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Approche hydrogéologique des plaines de Gdaine et Zana-chott saboun, NE algérien.</style></title><secondary-title><style face="normal" font="default" size="100%">4ème colloque international sur les géosciences, Tébessa</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">The SASS transboundary water resources, joint management and risk of conflicts</style></title><secondary-title><style face="normal" font="default" size="100%">International Journal of arts and sciences UNLV, 12-16, 2018, USA</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://unlv2018.sched.com/</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Dekakra Mouna</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">Abdelhamid Khedidja</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Hydrogeological and hydrochemical study of Teleghma aquifer (NE Algeria)</style></title><secondary-title><style face="normal" font="default" size="100%">3rd International conference on Integrated environmental management for sustainable development, 2-5 mai 2018, Sousse, Tunisie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Adaptation de l&amp;#39;agriculture saharienne à la sécheresse - cas de la région d&amp;#39;Oued Souf (Algérie)</style></title><secondary-title><style face="normal" font="default" size="100%">16 ème Conférence Internationale EURO-RIOB, 17-20 Oct 2018, Séville, Espagne</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Lebchek Soumia</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Approche hydrogéologique du bassin miocène de Timgad(Wilaya de Batna -- nord-est algérien), ISSN: 1370 - 6071</style></title><secondary-title><style face="normal" font="default" size="100%">Geo-Eco-Trop </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://www.geoecotrop.be/uploads/publications/pub_421_03.pdf</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">volume 42</style></volume><pages><style face="normal" font="default" size="100%">pp.33-42</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Timgad Basin is a part of the North-East Algerian Saharan Atlas. It is located at the northern of the Aurès Mountain. It is bordered in the North by Bou Arif, Amrane and Tagratine mountains, while in the South it is limited by Chelia, Rdam and Nerdi Bouhmar mountains. It is shaped as a synclinal gutter oriented East-West and covers an area of about 1000 Km2 . The climate is semi-arid (cold winter and hot summer) with average annual rainfall not exceeding 350 mm. The basin is composed by varied lithology, showing large folded structures down sloping towards the center, which favor groundwater storage. The Miocene sandstone aquifer is the most important. It is characterized by a wavy shape, which form series of shale-marl filling depressions. Recent wells drilled in the basin edges and center, put in evidence its artesian character. The piezometric survey shows a groundwater convergent flow oriented towards the basin east (Bou el Freis), likewise the sandstone aquifer is marked by the presence of a West-East drainage axis which separates the basin northern part characterized by a low reservoirs hydraulic capacity from the southern part distinguished by the groundwater relative abundance.</style></abstract><issue><style face="normal" font="default" size="100%"> issue 1 </style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Lebchek Soumia</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">The influence of the aquifer geometry on the groundwater flows (Timgad Basin, North-East Algeria), ISSN / e-ISSN: 2220-6663 /2222-3045</style></title><secondary-title><style face="normal" font="default" size="100%">journal of Biodiversity and Environmental Sciences (JBES)</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://innspub.net/jbes/influence-aquifer-geometry-groundwater-flows-timgad-basin-north-east-algeria/</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Vol. 12</style></volume><pages><style face="normal" font="default" size="100%">pp. 354-360</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">The basin of Timgad belongs to the North-Eastern Algerian Saharan Atlas; it is located at the northern extension of the Aures Mountains. The basin is an asymmetrical syncline oriented East-West covering an area of 1000 Km2. The climate is semi-arid (cold winter and hot summer) with average annual rainfall not exceeding 400 mm. Recently, the increasing agricultural activities led to an excessive exploitation of groundwater resources. In order to meet this rising water supply demands, implementing a water resources management policy is a priority which should be based on a basin hydrogeological study. Effectively, the geological and geophysical studies have confirmed the presence of permeable Miocene and Cretaceous formations (sandstone and carbonate); relatively resistant affected by fractures network, which are probably forming a confined aquifers. Indeed, recent wells drilled in the basin center and their boundaries; show that the aquifers are artesian. The sandstone aquifer of the Miocene is the most important, it is characterized by significant thickness which can exceed 200m, its extension as well as its particular corrugated geometry, characterized by a wavy shape, which forming a series of shale-marl&amp;nbsp;filling depressions, influences the groundwater flow, actually, the piezometric surface illustrates groundwater convergent flow oriented to the east, towards Bou el freis, likewise the sandstone aquifer is marked by the presence of a West-East drainage axis which separates the basin northern part characterized by a low reservoirs hydraulic capacity from the southern part distinguished by the groundwater relative abundance. Groundwater is generally easily extracted, except the northern part of the basin where the top shale-marl layer is thickens to over 1000m.</style></abstract><issue><style face="normal" font="default" size="100%">No. 5</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Athamenani Ali</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Nitrogen flux and hydrochemical characteristics of the calcareous aquifer of the Zana plain, north east of Algeria, July, ISSN /e- ISSN: 1866-7511 / 1866-7538</style></title><secondary-title><style face="normal" font="default" size="100%">Arabian Journal of Geosciences</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.1007/s12517-018-3681-5</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Vol 11</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">The hydrochemical and multivariate statistical techniques such as the principal component analysis (PCA) and the cluster analysis (CA) were used to identify the hydrochemical processes and their relation with groundwater quality and also to get an insight into the hydrochemical Zana aquifer groundwater chemistry evaluation. Twenty-four samples during the wet season and even during the dry season are analyzed. The Piper diagram showed that water facies are magnesium bicarbonate on the sides of the western reliefs and magnesium chloride-sulfated at the north and the center of the plain. The PCA carried out on three factors revealed that on the factorial design F1-F3, nitrates negatively determine factor 3, indicating the presence of an agriculture pollution. On the factorial design F1-F2, HCO3− positively determine the factor 2, indicating the carbonated origin. However, the CA, based on variables, showed that the waters in the region can be classified into three groups according to flow direction while the CA, based on major ion contents, defined three groups, reflecting the same hydrochemical facies. The first group with dry residue varying between 360 and 1700 mg/l and characterized by Mg2+ and Cl−, HCO3−. Samples of this group are mostly located in the north and northeastern part of the region. The second group with highest dry residue (2080 to 3820 mg/l) characterized by Mg2+ and SO4−, Cl− is located near the Northwestern and western outcrops. The third group coincides with the central part, the lowest of the plain, with heightened dry residue (4140 to 13,950 mg/l), characterized by Mg2+ and SO4−. The hydrochemical study made it possible to allot the evaporitic origin to the elements Na+, Mg2+, K+, Cl−, and SO4−, while for element HCO3−, it results from the carbonated formations. These results showed that the presence of nitrates in the studied area is closely linked to the agricultural activity.</style></abstract><issue><style face="normal" font="default" size="100%">Issue 13</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Kechha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Étude géologique de la plaine Sud Sétifienne par une approche géophysique</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Douaflia Abdelkader</style></author><author><style face="normal" font="default" size="100%">Benour yahia</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Étude géologique de la plaine de Gadaine par une approche géophysique</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Drias Tarek</style></author><author><style face="normal" font="default" size="100%">Fehdi Chemseddine</style></author><author><style face="normal" font="default" size="100%">Belloula Moufida</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Hydrochemical Analysis and Evaluation of Groundwater Quality of an Alluvial Aquifer. Algeria.</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Bentahar Fahima</style></author><author><style face="normal" font="default" size="100%">Inal Ahmed</style></author><author><style face="normal" font="default" size="100%">Yahaoui Abedel Ouahab</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Evolution tectono-sedimentaires dans la serie aptienne de Telidjene-Tebessa (Algerie oreiental)</style></title><secondary-title><style face="normal" font="default" size="100%">4eme Colloque International, les Géosciences au service du Développement durable, université Larbi Tebessi,Tebessa, Alger 22 novembre.</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><pub-location><style face="normal" font="default" size="100%">Tebessa, Alger</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Bentahar Fahima</style></author><author><style face="normal" font="default" size="100%">Yahaoui Abedel Ouahab</style></author><author><style face="normal" font="default" size="100%">Inal Ahmed</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Lithostratigraphie de la serie Aptienne du DJ Bouroumane-Tebessa (Algerie oriental)</style></title><secondary-title><style face="normal" font="default" size="100%">4eme Colloque International, les Géosciences au service du Développement durable, université Larbi Tebessi,Tebessa, Alger 22 novembre.</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><pub-location><style face="normal" font="default" size="100%">Tebessa, Alger</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Zouaoui Siham</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">Bouabid Abd Ennasser</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Les ressources en eau du Nord Est Algerien region de Tolga, qualité des eaux  de la nappe des calcaires</style></title><secondary-title><style face="normal" font="default" size="100%">4eme Colloque International, les Géosciences au service du Développement durable, université Larbi Tebessi,Tebessa, Alger 22 novembre</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><pub-location><style face="normal" font="default" size="100%">Tebessa, Alger</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Zouaoui Siham</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">Bouabid Abd Ennasser</style></author><author><style face="normal" font="default" size="100%">Boukhenissa F</style></author><author><style face="normal" font="default" size="100%">Ahmadi L</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude de la qualité des eaux de la nappe superficielle dans la region de Tolga</style></title><secondary-title><style face="normal" font="default" size="100%">4eme Colloque International, les Géosciences au service du Développement durable, université Larbi Tebessi,Tebessa, Alger 22 novembre.</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><pub-location><style face="normal" font="default" size="100%">Tebessa, Alger</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brahmia Ali</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Use of mechanical drill data and vertical electrical soundings for the identification of aquifer geometry of lower Maestrichtian limestone M&amp;#39;Daourouch Drea plain Wilaya of Souk Ahras NE Algerian, ISSN / e-ISSN 2220-6663 / 2222-3045</style></title><secondary-title><style face="normal" font="default" size="100%">Journal of Biodiversity and Environmental Sciences (JBES)</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://innspub.net/jbes/use-mechanical-drill-data-vertical-electrical-soundings-identification-aquifer-geometry-lower-maestrichian-limestones-mdaourouch-drea-plain-wilaya-souk-ahras-ne-algerian/</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Volume 12</style></volume><pages><style face="normal" font="default" size="100%">pp 90-95</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">This paper was made in the region of M’daourouch-Dréa which is part of the high plains of northeastern Algeria, located southwest of the Souk-ahras Wilaya in eastern Algeria. It is a plain with agricultural vocation which requires for its development more water. Knowing that the rainfall is low (465mm/year) and not enough to meet the needs of farmers, the use of groundwater then becomes the only alternative to fill this lack of resources. Among the aquifers identified in this region is that contained in fissured limestones of lower Maestrichian age. In order to satisfy farmers and citizens in water it is necessary to have a good characterization of this aquifer. The objective of this paper is to improve the knowledge on the morphology and the extension of this aquifer and to locate its roof in space to help operators choose areas favorable to exploitation, so direct them to the nearest areas of the surface thus minimizing the cost of the drilling operation. To achieve this goal, we have exploited by exploiting several tools (geological map, logs of boreholes and geophysics survey), whose combination gave an idea on the geometry of the aquifer as well as the depth of its roof in different regions of the plain and shows by the occasion, the affectation of these limestones by several tectonic accidents generating thus a structure in collapsed blocks from where the very variable depth of the roof of these limestones of a place of the plain to other.</style></abstract><issue><style face="normal" font="default" size="100%">1</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution of statistical technique in the Characterization hydro-chimical of groundwater, case of the region Zana-Roknia, Eastern Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">13th International Conference on Water Resources organized by Al-Hussein Bin Talal University and the European Organization for Environmental, Water and Desert Research in Antalya, Turkey 25-27 novembre</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><pub-location><style face="normal" font="default" size="100%">Antalya, Turkey </style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Nitrogen flux and hydrochemical characteristics of the calcareous aquifer of the Zana plain, north east of Algeria, July, ISSN /e- ISSN: 1866-7511 / 1866-7538</style></title><secondary-title><style face="normal" font="default" size="100%">Arabian Journal of Geosciences</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.1007/s12517-018-3681-5</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%"> Vol 11</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">The hydrochemical and multivariate statistical techniques such as the principal component analysis (PCA) and the cluster analysis (CA) were used to identify the hydrochemical processes and their relation with groundwater quality and also to get an insight into the hydrochemical Zana aquifer groundwater chemistry evaluation. Twenty-four samples during the wet season and even during the dry season are analyzed. The Piper diagram showed that water facies are magnesium bicarbonate on the sides of the western reliefs and magnesium chloride-sulfated at the north and the center of the plain. The PCA carried out on three factors revealed that on the factorial design F1-F3, nitrates negatively determine factor 3, indicating the presence of an agriculture pollution. On the factorial design F1-F2, HCO3− positively determine the factor 2, indicating the carbonated origin. However, the CA, based on variables, showed that the waters in the region can be classified into three groups according to flow direction while the CA, based on major ion contents, defined three groups, reflecting the same hydrochemical facies. The first group with dry residue varying between 360 and 1700 mg/l and characterized by Mg2+ and Cl−, HCO3−. Samples of this group are mostly located in the north and northeastern part of the region. The second group with highest dry residue (2080 to 3820 mg/l) characterized by Mg2+ and SO4−, Cl− is located near the Northwestern and western outcrops. The third group coincides with the central part, the lowest of the plain, with heightened dry residue (4140 to 13,950 mg/l), characterized by Mg2+ and SO4−. The hydrochemical study made it possible to allot the evaporitic origin to the elements Na+, Mg2+, K+, Cl−, and SO4−, while for element HCO3−, it results from the carbonated formations. These results showed that the presence of nitrates in the studied area is closely linked to the agricultural activity.</style></abstract><issue><style face="normal" font="default" size="100%">Issue 13</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Kemoukh Sami</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Qualité des eaux de surface d&amp;#39;Oued Saf-Saf (Nord Est Algerien)</style></title><secondary-title><style face="normal" font="default" size="100%">4eme Colloque International, les Géosciences au service du Développement durable, université Larbi Tebessi,Tebessa, Alger 22 novembre</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><pub-location><style face="normal" font="default" size="100%">Tebessa, Alger</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">ATHAMENA Malika</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">The Evaluation of the Belezmamounts thermal potential: at the South-Eastern confinement of the South Setifian Set, Eastern Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">4eme Colloque International, les Géosciences au service du Développement durable, université Larbi Tebessi,Tebessa, Alger 22 novembre</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><pub-location><style face="normal" font="default" size="100%">Tebessa, Alger</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Bilalite Halima</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Approche hydrogéologique des plaines de Gadaine et Zana-Chott Saboun (wilaya de Batna, Nord-Est Algerienne)</style></title><secondary-title><style face="normal" font="default" size="100%">4eme Colloque International, les Géosciences au service du Développement durable, université Larbi Tebessi,Tebessa, Alger 22 novembre</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">Bilalite Halima</style></author><author><style face="normal" font="default" size="100%">Ghenima Z</style></author><author><style face="normal" font="default" size="100%">Teffaha S</style></author><author><style face="normal" font="default" size="100%">Kihel K</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Barrages et Envirennement, une relation développé, Cas du Barrage de Beni-Haroun, Mila, Est Algerie</style></title><secondary-title><style face="normal" font="default" size="100%">4eme Colloque International les Géosciences au service du Développement durable, université Larbi Tebessi,Tebessa, Alger 22 novembre</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><pub-location><style face="normal" font="default" size="100%">Tebessa, Alger</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Approche statistique dans la caractérisation physico-chimique des eaux souterraines, cas de Chott-Saboun, Est Algérie</style></title><secondary-title><style face="normal" font="default" size="100%">4eme Colloque International les Géosciences au service du Développement durable, université Larbi Tebessi,Tebessa, Alger 22 novembre</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><pub-location><style face="normal" font="default" size="100%">Tebessa, Alger</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">10&lt;sup&gt;ème &lt;/sup&gt;International Symposium on Cephalopods &amp;laquo; Present and Past &amp;raquo; organised by Sidi Mohamed Ben Abdellah University Fes and the Westfalische Wilhelms University, Muenster, 26&lt;sup&gt;th&lt;/sup&gt; March-3&lt;sup&gt;rd &lt;/sup&gt;April 2018.MAROC</style></title><secondary-title><style face="normal" font="default" size="100%">10th INTERNATIONAL SYMPOSIUM “CEPHALOPODS – PRESENT AND PAST</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><pub-location><style face="normal" font="default" size="100%">MAROC</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Drias Tarek</style></author><author><style face="normal" font="default" size="100%">Belloula Moufida</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Hydrogeochemical Assessment of an Alluvial Aquifer Under Semi-Arid Climat. Eastern Algeria, ISSN 2321 &amp;ndash;9009</style></title><secondary-title><style face="normal" font="default" size="100%">International Journal of Advances in Science, Engineering and Technology (IJASEAT)</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://www.iraj.in/journal/journal_file/journal_pdf/6-331-148853256927-32.pdf</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Volume-6</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;span style=&quot;left:187.2px;top:328px;15.1998px;sans-serif;transform:scaleX(0.9478);&quot;&gt;Th&lt;/span&gt;&lt;span style=&quot;left:204px;top:328px;15.1998px;sans-serif;transform:scaleX(0.878436);&quot;&gt;e study of the water quality in the alluvial aquifer &lt;/span&gt;&lt;span style=&quot;left:527.2px;top:328px;15.1998px;sans-serif;transform:scaleX(0.86389);&quot;&gt;of Tebessa&lt;/span&gt;&lt;span style=&quot;left:594.4px;top:327.9998488333333px;15.19983333333333px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:599.2px;top:328px;15.1998px;sans-serif;transform:scaleX(0.943096);&quot;&gt;Morsott &lt;/span&gt;&lt;span style=&quot;left:653.2px;top:328px;15.1998px;sans-serif;transform:scaleX(0.869563);&quot;&gt;basin&lt;/span&gt;&lt;span style=&quot;left:690.8px;top:328px;15.1998px;sans-serif;transform:scaleX(0.865705);&quot;&gt;was carried out &lt;/span&gt;&lt;span style=&quot;left:793.2px;top:328px;15.1998px;sans-serif;transform:scaleX(0.873079);&quot;&gt;to perform a &lt;/span&gt;&lt;span style=&quot;left:120px;top:345.2px;15.1998px;sans-serif;transform:scaleX(0.885536);&quot;&gt;preliminary assessment&lt;/span&gt;&lt;span style=&quot;left:266.4px;top:345.2px;15.1998px;sans-serif;transform:scaleX(0.913761);&quot;&gt;of the hydrochemical quality of same groundwater samples &lt;/span&gt;&lt;span style=&quot;left:637.2px;top:345.2px;15.1998px;sans-serif;transform:scaleX(0.858867);&quot;&gt;and &lt;/span&gt;&lt;span style=&quot;left:663.6px;top:345.2px;15.1998px;sans-serif;transform:scaleX(0.929801);&quot;&gt;their &lt;/span&gt;&lt;span style=&quot;left:695.6px;top:345.2px;15.1998px;sans-serif;transform:scaleX(0.939549);&quot;&gt;suitability for irrigation uses. &lt;/span&gt;&lt;span style=&quot;left:120px;top:362.4px;15.1998px;sans-serif;transform:scaleX(0.878021);&quot;&gt;The high salinity coupled&lt;/span&gt;&lt;span style=&quot;left:283.2px;top:362.4px;15.1998px;sans-serif;transform:scaleX(0.867104);&quot;&gt;with groundwater level decline pose serious problems for current irrigation and domestic water &lt;/span&gt;&lt;span style=&quot;left:120px;top:379.6px;15.1998px;sans-serif;transform:scaleX(0.905192);&quot;&gt;supplies as well as &lt;/span&gt;&lt;span style=&quot;left:239.6px;top:379.6px;15.1998px;sans-serif;transform:scaleX(0.956809);&quot;&gt;for &lt;/span&gt;&lt;span style=&quot;left:261.6px;top:379.6px;15.1998px;sans-serif;transform:scaleX(0.935955);&quot;&gt;future exploitation. &lt;/span&gt;&lt;span style=&quot;left:382.8px;top:379.6px;15.1998px;sans-serif;transform:scaleX(0.916073);&quot;&gt;The statistical treatment of hydrochemical data by principal component analysis &lt;/span&gt;&lt;span style=&quot;left:120px;top:396.8px;15.1998px;sans-serif;transform:scaleX(0.898354);&quot;&gt;revealed two components re&lt;/span&gt;&lt;span style=&quot;left:291.2px;top:396.8px;15.1998px;sans-serif;transform:scaleX(0.913495);&quot;&gt;lated to &lt;/span&gt;&lt;span style=&quot;left:341.2px;top:396.8px;15.1998px;sans-serif;transform:scaleX(0.942399);&quot;&gt;salinity and pollution.&lt;/span&gt;&lt;span style=&quot;left:478.8px;top:396.8px;15.1998px;sans-serif;transform:scaleX(0.919589);&quot;&gt;The US salinity diagram illustrates that most of the groundwater &lt;/span&gt;&lt;span style=&quot;left:120px;top:414px;15.1998px;sans-serif;transform:scaleX(0.900947);&quot;&gt;samples fall in C3S1&lt;/span&gt;&lt;span style=&quot;left:244.79999999999998px;top:413.99984883333343px;15.19983333333333px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:253.6px;top:414px;15.1998px;sans-serif;transform:scaleX(0.908158);&quot;&gt;C4S1 quality with high salinity hazard and low sodium hazard.&lt;/span&gt;</style></abstract><issue><style face="normal" font="default" size="100%">Issue-1</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>5</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Drias Tarek</style></author><author><style face="normal" font="default" size="100%">Chemseddine Fehdi</style></author><author><style face="normal" font="default" size="100%">Moufida Belloula</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Hydrochemical Analysis and Evaluation of Groundwater Quality of an Alluvial Aquifer. Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">Recent Advances in Environmental Science from the Euro-Mediterranean and Surrounding Regions</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.1007/978-3-319-70548-4_191</style></url></web-urls></urls><publisher><style face="normal" font="default" size="100%">Springer </style></publisher><pub-location><style face="normal" font="default" size="100%">Cham</style></pub-location><pages><style face="normal" font="default" size="100%"> 637-639</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">The study of the water quality in the shallow aquifer of Tebessa-Morsott was carried out to perform a preliminary assessment of the hydrochemical quality of same groundwater samples and their suitability for irrigation uses. The high salinity coupled with groundwater level decline pose serious problems for current irrigation and domestic water supplies as well as for future exploitation. The statistical treatment of hydrochemical data by principal component analysis revealed two components related to salinity and pollution. The US salinity diagram illustrates that most of the groundwater samples fall in C3S1- C4S1 quality with high salinity hazard and low sodium hazard.</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brahmia Ali</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Nouar Tahar</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Statistical and hydro-geochemical characteristics of the M&amp;rsquo;daourouch-Drea plain&amp;rsquo;s groundwater; North-east of Algeria, ISSN / e-ISSN 1429-7426 / 2083-4535</style></title><secondary-title><style face="normal" font="default" size="100%">Journal of Water and Land Development</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.degruyter.com/downloadpdf/j/jwld.2018.38.issue-1/jwld-2018-0038/jwld-2018-0038.pdf</style></url></web-urls></urls><pages><style face="normal" font="default" size="100%"> pp 19–26. (VII-IX) 2018 (promesse de publication).</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;span style=&quot;left:146.5px;top:687.918px;16.7px;serif;transform:scaleX(1.01679);&quot;&gt;This work was conducted on 23 samples distributed between sprin&lt;/span&gt;&lt;span style=&quot;left:597.798px;top:687.918px;16.7px;serif;transform:scaleX(1.01856);&quot;&gt;gs, wells and boreholes tapping the shal-&lt;/span&gt;&lt;span style=&quot;left:118.2px;top:707.118px;16.7px;serif;transform:scaleX(1.03235);&quot;&gt;low and deep aquifer in the M'Daourouch-Drea area located in ex&lt;/span&gt;&lt;span style=&quot;left:570.299px;top:707.118px;16.7px;serif;transform:scaleX(1.02727);&quot;&gt;treme northeast of Algeria. Ca&lt;/span&gt;&lt;span style=&quot;left:778.5px;top:704.876px;10.8px;serif;transform:scaleX(1.00066);&quot;&gt;2+&lt;/span&gt;&lt;span style=&quot;left:790px;top:707.118px;16.7px;serif;transform:scaleX(1.04393);&quot;&gt;, Mg&lt;/span&gt;&lt;span style=&quot;left:823px;top:704.876px;10.8px;serif;transform:scaleX(1.00066);&quot;&gt;2+&lt;/span&gt;&lt;span style=&quot;left:834.5px;top:707.118px;16.7px;serif;transform:scaleX(1.05444);&quot;&gt;, Na&lt;/span&gt;&lt;span style=&quot;left:863.7999999999998px;top:704.8754765625px;10.799999999999999px;serif;&quot;&gt;+&lt;/span&gt;&lt;span style=&quot;left:869.9px;top:707.118px;16.7px;serif;transform:scaleX(1.006);&quot;&gt;, &lt;/span&gt;&lt;span style=&quot;left:118.20237199999988px;top:726.217698203125px;16.7px;serif;&quot;&gt;K&lt;/span&gt;&lt;span style=&quot;left:130.3px;top:723.9754765624999px;10.799999999999999px;serif;&quot;&gt;+&lt;/span&gt;&lt;span style=&quot;left:136.4px;top:726.218px;16.7px;serif;transform:scaleX(1.01316);&quot;&gt;, Cl&lt;/span&gt;&lt;span style=&quot;left:160.79999999999998px;top:723.9754765624999px;10.799999999999999px;serif;&quot;&gt;–&lt;/span&gt;&lt;span style=&quot;left:166.2px;top:726.218px;16.7px;serif;transform:scaleX(1.00919);&quot;&gt;, SO&lt;/span&gt;&lt;span style=&quot;left:196.2px;top:733.9754765624999px;10.799999999999999px;serif;&quot;&gt;4&lt;/span&gt;&lt;span style=&quot;left:201.6px;top:723.976px;10.8px;serif;transform:scaleX(0.999999);&quot;&gt;2–&lt;/span&gt;&lt;span style=&quot;left:212.4px;top:726.218px;16.7px;serif;transform:scaleX(1.00141);&quot;&gt;, HCO&lt;/span&gt;&lt;span style=&quot;left:256.2px;top:733.9754765624999px;10.799999999999999px;serif;&quot;&gt;3&lt;/span&gt;&lt;span style=&quot;left:261.59999246666666px;top:723.9757565624999px;10.799999999999999px;serif;&quot;&gt;–&lt;/span&gt;&lt;span style=&quot;left:267px;top:726.218px;16.7px;serif;transform:scaleX(1.01348);&quot;&gt; and NO&lt;/span&gt;&lt;span style=&quot;left:324.09999999999997px;top:733.9754765624999px;10.799999999999999px;serif;&quot;&gt;3&lt;/span&gt;&lt;span style=&quot;left:329.49999246666664px;top:723.9757565624999px;10.799999999999999px;serif;&quot;&gt;–&lt;/span&gt;&lt;span style=&quot;left:334.9px;top:726.218px;16.7px;serif;transform:scaleX(1.00336);&quot;&gt; were analysed. The interpreta&lt;/span&gt;&lt;span style=&quot;left:537.399px;top:726.218px;16.7px;serif;transform:scaleX(1.00219);&quot;&gt;tion of the geological-geophysica&lt;/span&gt;&lt;span style=&quot;left:760.897px;top:726.218px;16.7px;serif;transform:scaleX(1.00361);&quot;&gt;l data allowed us &lt;/span&gt;&lt;span style=&quot;left:118.201px;top:745.418px;16.7px;serif;transform:scaleX(1.02106);&quot;&gt;to highlight two aquifers. The first consists of conglomerates,&lt;/span&gt;&lt;span style=&quot;left:537.799px;top:745.418px;16.7px;serif;transform:scaleX(1.02005);&quot;&gt; sandstones, gravels, sands, marls, limestones, la-&lt;/span&gt;&lt;span style=&quot;left:118.201px;top:764.618px;16.7px;serif;transform:scaleX(1.02594);&quot;&gt;custrine and alluvial deposits varying in thickness from a few &lt;/span&gt;&lt;span style=&quot;left:544.899px;top:764.618px;16.7px;serif;transform:scaleX(1.02638);&quot;&gt;tens to a few hundred meters, representing Neo-&lt;/span&gt;&lt;span style=&quot;left:118.201px;top:783.718px;16.7px;serif;transform:scaleX(0.998009);&quot;&gt;gene-Quaternary filling of the st&lt;/span&gt;&lt;span style=&quot;left:333px;top:783.718px;16.7px;serif;transform:scaleX(0.996796);&quot;&gt;udied basin. The second is mor&lt;/span&gt;&lt;span style=&quot;left:540.3px;top:783.718px;16.7px;serif;transform:scaleX(0.998671);&quot;&gt;e important localized in the cracked and karstified &lt;/span&gt;&lt;span style=&quot;left:118.202px;top:802.918px;16.7px;serif;transform:scaleX(1.01933);&quot;&gt;limestones of upper Cretaceous age; these limestones are outcro&lt;/span&gt;&lt;span style=&quot;left:554.1px;top:802.918px;16.7px;serif;transform:scaleX(1.03264);&quot;&gt;pped on the flanks of the syncline and the bor-&lt;/span&gt;&lt;span style=&quot;left:118.202px;top:822.118px;16.7px;serif;transform:scaleX(0.999164);&quot;&gt;ders of the basin. The first aqui&lt;/span&gt;&lt;span style=&quot;left:326.301px;top:822.118px;16.7px;serif;transform:scaleX(0.999189);&quot;&gt;fer sometimes rests directly o&lt;/span&gt;&lt;span style=&quot;left:522.8px;top:822.118px;16.7px;serif;transform:scaleX(0.999564);&quot;&gt;n the second which allows hydraulic communication &lt;/span&gt;&lt;span style=&quot;left:118.202px;top:841.217px;16.7px;serif;transform:scaleX(1.00093);&quot;&gt;between them. The hydogeochemical and statistical study, with t&lt;/span&gt;&lt;span style=&quot;left:549.8px;top:841.217px;16.7px;serif;transform:scaleX(0.997864);&quot;&gt;he combination of numerous tools, indicates that &lt;/span&gt;&lt;span style=&quot;left:118.202px;top:860.417px;16.7px;serif;transform:scaleX(1.01258);&quot;&gt;the chemistry of groundwater in t&lt;/span&gt;&lt;span style=&quot;left:344.101px;top:860.417px;16.7px;serif;transform:scaleX(1.00969);&quot;&gt;he M'Daourouch-Drea Plain is c&lt;/span&gt;&lt;span style=&quot;left:561.6px;top:860.417px;16.7px;serif;transform:scaleX(1.0143);&quot;&gt;ontrolled both by the dissolution of the miner-&lt;/span&gt;&lt;span style=&quot;left:118.202px;top:879.617px;16.7px;serif;transform:scaleX(0.998243);&quot;&gt;als of the evaporite formations and those of the carbonate form&lt;/span&gt;&lt;span style=&quot;left:537.4px;top:879.617px;16.7px;serif;transform:scaleX(0.999627);&quot;&gt;ations.&lt;/span&gt;</style></abstract><issue><style face="normal" font="default" size="100%">N°38</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brahmia Ali</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Use of mechanical drill data and vertical electrical soundings for the identification of aquifer geometry of lower Maestrichtian limestone M&amp;#39;Daourouch Drea plain Wilaya of Souk Ahras NE Algerian</style></title><secondary-title><style face="normal" font="default" size="100%">Journal of Biodiversity and Environmental Sciences (JBES)</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://innspub.net/jbes/use-mechanical-drill-data-vertical-electrical-soundings-identification-aquifer-geometry-lower-maestrichian-limestones-mdaourouch-drea-plain-wilaya-souk-ahras-ne-algerian/</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">12</style></volume><pages><style face="normal" font="default" size="100%">pp 90-95</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">This paper was made in the region of M’daourouch-Dréa which is part of the high plains of northeastern Algeria, located southwest of the Souk-ahras Wilaya in eastern Algeria. It is a plain with agricultural vocation which requires for its development more water. Knowing that the rainfall is low (465mm/year) and not enough to meet the needs of farmers, the use of groundwater then becomes the only alternative to fill this lack of resources. Among the aquifers identified in this region is that contained in fissured limestones of lower Maestrichian age. In order to satisfy farmers and citizens in water it is necessary to have a good characterization of this aquifer. The objective of this paper is to improve the knowledge on the morphology and the extension of this aquifer and to locate its roof in space to help operators choose areas favorable to exploitation, so direct them to the nearest areas of the surface thus minimizing the cost of the drilling operation. To achieve this goal, we have exploited by exploiting several tools (geological map, logs of boreholes and geophysics survey), whose combination gave an idea on the geometry of the aquifer as well as the depth of its roof in different regions of the plain and shows by the occasion, the affectation of these limestones by several tectonic accidents generating thus a structure in collapsed blocks from where the very variable depth of the roof of these limestones of a place of the plain to other.</style></abstract><issue><style face="normal" font="default" size="100%">01</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>5</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">La pollution des rejets liquides de la ville de Batna (Algérie). Impacts sur l&amp;rsquo;agriculture et sur les eaux destinées à l&amp;rsquo;usage domestique</style></title><secondary-title><style face="normal" font="default" size="100%">Eau et climat en Afrique du Nord et au Moyen-Orient</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><pages><style face="normal" font="default" size="100%">113-124</style></pages><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>5</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Évaluation du risque de conflit autour des eaux transfrontalières du système aquifère du Sahara septentrional (SASS)</style></title><secondary-title><style face="normal" font="default" size="100%">Eau et climat en Afrique du Nord et au Moyen-Orient</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><pages><style face="normal" font="default" size="100%">45-69</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;div&gt;
	&lt;p&gt;
		Le SASS couvre une superficie d’environ 1&amp;nbsp;000&amp;nbsp;000 km², il est partagé par l’Algérie, la Libye et la Tunisie. Il est situé dans une zone hyper aride avec une recharge actuelle minime mais un grand volume stocké, évalué entre 20&amp;nbsp;000 et 31&amp;nbsp;000 km&lt;sup&gt;3&lt;/sup&gt;.
	&lt;/p&gt;

	&lt;p&gt;
		Depuis 1970 à nos jours, l’exploitation du SASS est passée de 0,6 à plus de 2,5 milliards m3/an., d’où des risques majeurs &amp;nbsp;de salinisation des eaux, de réduction de l’artésianisme, de tarissement des exutoires naturels, de baisse de la piézométrie, d’augmentation des rabattements ou d’interférences des périmètres de captage entre pays…Ce qui menace à terme la durabilité du développement socio-économique engagé dans l’ensemble de la zone.
	&lt;/p&gt;

	&lt;p&gt;
		Pour parer au mieux à ces risques et surtout pour mieux s’en prémunir, un processus de coopération a été initié depuis 1998 sous l’égide de l’observatoire du Sahara septentrional (OSS) en partenariat avec les institutions en charge des ressources en eau dans les 3 pays.
	&lt;/p&gt;

	&lt;p&gt;
		L’importance de cet immense réservoir pour le développement de la zone SASS et la nécessité de sa gestion durable et concertée a amené à une entente pour son étude en plusieurs phases&amp;nbsp;: la caractérisation hydrogéologique du système aquifère et sa modélisation, l’identification des risques environnementaux et l’inclusion de l’aspect socio-économique dans des scénarios de développement.
	&lt;/p&gt;

	&lt;p&gt;
		Les ressources en eau du SASS sont très faiblement renouvelables, environ 1 milliard de m3/an, vis-à-vis des prélèvements actuels estimés à 2,5 milliards de m3/an. La prise en compte de cette donnée a été déterminante pour pousser les scientifiques à établir la meilleure modélisation conceptuelle possible du système qui soit à même de permettre d’envisager différents scénarios d’exploitation de la ressource tout en tenant compte des perspectives de développement socio-économique de chacun des 3 pays.
	&lt;/p&gt;

	&lt;p&gt;
		Les données actuelles, quoique rassurantes, ne signifient pas l’inexistence, à court ou moyen terme, d’un risque de conflit autour de ces eaux transfrontalières. En effet, le problème mérite d’être analysé à travers plusieurs indicateurs qui ont un impact sur ce risque.
	&lt;/p&gt;

	&lt;p&gt;
		L’objectif de cette note est d’évaluer le risque de conflit autour des eaux du SASS à travers un indice global exprimé numériquement sur la base de la combinaison de poids et de cotes de plusieurs indicateurs qui ont, directement ou indirectement, un impact sur le risque de conflit.
	&lt;/p&gt;

	&lt;p&gt;
		L’indice global de risque de conflit obtenu pour le cas du SASS semble refléter correctement la situation qui y prévaut actuellement. La comparaison de ce résultat avec ceux obtenus pour les eaux transfrontalières du bassin du Jourdain (risque élevé) et ceux du système aquifère du Guarani (risque faible), conforte l’échelle des valeurs adoptée dans cette méthode d’indexation numérique.
	&lt;/p&gt;
&lt;/div&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Righi Asma</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution au Suivi piézométrique et hydrochimie  dans la plaine de Belezma (W, de Batna)</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Touahria Kamel</style></author><author><style face="normal" font="default" size="100%">Khabar Ali</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Étude stratigraphique et sédimentologique du Campanien supérieur du massif d&amp;#39;El Kantara</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Toumi.A</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à l&amp;rsquo;étude hydrogéologique de la nappe Mio-Pliocène de la région de Tolga</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Ghemima. Z</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Impact des plans d&amp;rsquo;eau artificiels sur les régimes hydrologiques - Cas du barrage de beni haroune - mila - Est algérien</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Azizi Yacine</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Les effondrements dans les terrains karstiques du plateau de Cheria (NE de l&amp;#39;Algérie), impacts gotechnique et environnementaux et cartographie des zones vulnérables au phénomène.</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://www.secheresse.info/spip.php?article79566</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Les effondrements des cavités souterraines dans les calcaires karstifiés constituent un aléa géologique sérieux qui continue à recevoir une intention particulière à l’échelle de la planète. Il s’agit d’un phénomène très connus, lié à la présence de vides souterrains dans les terrains calcaires, dolomitiques et gypsifères. Le plateau de Chéria correspond à une structure synclinale, grossièrement triangulaire d’orientation NE – SW affecté par une fracturation orthogonale à l‘axe du pli. Il est essentiellement formé de calcaires Eocène largement karstifié et recouvert de matériaux meubles, essentiellement des alluvions, des argiles et des encroutements calcaires. Ce bassin en question abrite trois aquifères superposés, l’aquifère du Maastrichtien, l’Eocène et la nappe alluviale du Moi-Plio-Quaternaire. Celle qui fait l’objet de cette étude est la nappe de l’Eocène. Le sens d’écoulement générale dans les nappes souterraines notamment les alluvions et l’Eocène est sensiblement Nord-Sud. La surexploitation actuelle des eaux souterraines a rendu la nappe des alluvions sans intérêt hydrogéologique, et a causé un grand rabattement dans les calcaires de l’Eocène. Les méthodes directes et indirectes d’explorations du sous-sol de la région ont révélés la présence de plusieurs cavités souterraines de dimensions importantes. La méthode de tomographie électrique, Géoradar et les sondages mécaniques ont montré l’existence à faible profondeur des cavités dans la région d’étude. La stabilité de ces cavités dépend d’un côté des propriétés mécaniques de la masse rocheuse formant le toit de la galerie, et les dimensions de cette dernière. Cette étude nous a permis d’établir des relations entre l’épaisseur du toit, largeur de cavité, et la charge pour un RMR (Rock masse rating) variable. La cartographie menée à l’échelle de la région a pu délimiter les zones susceptibles de présenter des cavités naturelles instables et cela va permet en conséquence de trouver des solutions au problème de l’effondrement à l’échelle de la région</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Chafou Nasereddine</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">APPROCHES HYDROGEOCHIMIQUES ET GEOTHERMOMETRIQUES POUR L&amp;rsquo;ETUDE DES EAUX THERMALES  CAS DU SYSTEME GEOTHERMAL EXPLOITE DANS LA REGION DE BISKRA AU SUD ALGERIEN</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Benmansour Sana</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Étude tectono-sédimentaire de la série campanienne de Dj. Lekhal (plaine d&amp;#39;ain Touta)</style></title><secondary-title><style face="normal" font="default" size="100%">La 4eme édition du Congrès des Doctorants 2017 de la FSTGAT se tiendra le 24 et 25 Avril 2017, &amp;aacut la maison de la science, USTHB, Alger</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Slami Rafika</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Sedimentology, Geochemistry and Various Microfaunal Component Responses to Environmental Fluctuations of the Cenomanian-Turonian Boundary at Thénièt El Manchar (Batna, NE Algeria)</style></title><secondary-title><style face="normal" font="default" size="100%">19th International Conference on Geological and Earth Sciences, Word Academy of Science Energinee Ring and Technology, Rome, Italy </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Belalit Halima</style></author><author><style face="normal" font="default" size="100%">Guemima. Z</style></author><author><style face="normal" font="default" size="100%">Toufaha. S</style></author><author><style face="normal" font="default" size="100%">Kihel. K</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Les impactes des plans d&amp;rsquo;eaux artificielles sur les régimes climatiques et hydrologiques à l&amp;rsquo;échelle. Cas d&amp;rsquo;un bassin versant du barrage de Beni Haroune, (Mila Est Algérien)</style></title><secondary-title><style face="normal" font="default" size="100%">Colloque International Eau-Société-Climat 2017(ESC- 2017) Hammamet 2-3-4 Octobre 2017.</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Géométrie de l&amp;rsquo;aquifère Néogène dans le bassin d&amp;rsquo;El Outaya, Atlas saharien au sud algérien</style></title><secondary-title><style face="normal" font="default" size="100%">Colloque International Eau-Société-Climat 2017(ESC- 2017) Hammamet 2-3-4 Octobre 2017</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">caracterisation hydrogeologique et hydro-chimique du bassin neogene de timgad (nord-est algerien)</style></title><secondary-title><style face="normal" font="default" size="100%">The 1st International Symposium (WREIANA 2017) Water Resources and Environmental Impact Assessment in North Africa, Gafsa, Tunisie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Lebchek Soumia</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation hydrogéologique et hydrochimique du bassin néogèn,e de Timgad, NE algérien</style></title><secondary-title><style face="normal" font="default" size="100%">1er International symposium - WREIANA, 24-26, Gafsa, Tunisie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Benmansour Sana</style></author><author><style face="normal" font="default" size="100%">Yahiaoui Abdelouahab</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Le campanien -Maastrichtien du bassin des Aurès, Algérie: Biostratigraphie, Paléoenvironnements et leurs implications.</style></title><secondary-title><style face="normal" font="default" size="100%">Annal de paléontologie , Science Direct-Elsevier masson France</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://doi.org/10.1016/j.annpal. 2017.11.001</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Mansouri Zineb</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">EVALUATION OF THE WATER NEEDS OF CROPS UNDER ARID CLIMATIC CONDITIONS. CASE OF TINIBAOUINE REGION (NORTH EAST OF ALGERIA), Feb, ISSN / e-ISSN: 2186-2990 / 2186-2990 </style></title><secondary-title><style face="normal" font="default" size="100%">International Journal of GEOMATE</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.researchgate.net/publication/313316435_Assessment_of_the_water_needs_of_apricot_and_olive_crops_under_arid_climatic_conditions_Case_study_of_Tinibaouine_region_Northeast_of_Algeria</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Vol. 12</style></volume><pages><style face="normal" font="default" size="100%">pp. 1 - 7</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">The Tinibaouine region, located in north-eastern Algeria on the borders of the Batna-Belezma Mountains, is characterized by a semi-arid to arid climate with an average annual rainfall not exceeding 465 mm and an average annual temperature of around 22 C. This region is characterized by the cultivation of apricots as essential crop followed by that of olives, whose plots are all irrigated with the Tinibaouine spring water. These are 450 Ha of trees for apricot and 108 Hectare for olives which constitute the principal revenue of the citizens of this small village. This paper estimated the crop reference and actual evapotranspiration (ETO) respectively and the irrigation water requirement of apricot trees and olive trees. The long recorded climatic data, crop and soil data, effective water allocation and planning, the information about crop water requirements, irrigation withdrawals were computed with the Cropwat model which is based on the United Nations’ Food and Agriculture Organization (FAO), the Penman-Monteith method was used to estimate ETo. Crop coefficients (Kc) from the phenomenological stages of apricot and olive were applied to adjust and estimate the actual evapotranspiration ETc through a water balance of the irrigation water requirements (IR). The results showed that the annual reference evapotranspiration (ETO) was estimated at 3.71 mm/day. The irrigation requirements were estimated at 35800 m3/hectare for apricot, 6980 m3/hectare for olive, also Irrigation needs estimated on land at 14185, 05 m3/hectare for olive and apricot.</style></abstract><issue><style face="normal" font="default" size="100%">Issue 30</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Bentahar Fahima</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etudes sédimentologiques de la série coniacienne du Dj Metlili (Algerie nord oriental)</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brikat</style></author><author><style face="normal" font="default" size="100%">Sehtal Sami</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude Paléo-Environnemental de la Région de Ain Touta Au Quaternaire : Terrasses Fluviatiles d&amp;rsquo;Oued El Hai.</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Bekkari Sif eddine</style></author><author><style face="normal" font="default" size="100%">Adel Abdelhak</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude Paléo-Environnemental de la Région d&amp;rsquo;El Mather Au Quaternaire : Terrasses Fluviatiles d&amp;rsquo;Oued El Gourzi</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Saada Brahim Oussama</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à l&amp;rsquo;étude hydrogéologique de la région du Droh (w) Biskra</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Saber A</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à l&amp;rsquo;étude hydrogéologique du champ captant de l&amp;rsquo;oued Biskra</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Drias Tarek</style></author><author><style face="normal" font="default" size="100%">Fehdi Chemseddine</style></author><author><style face="normal" font="default" size="100%">Belloula Moufida</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">hydrochemical analysis and evaluation of groundwater quality of an alluvial aquifer. algeria</style></title><secondary-title><style face="normal" font="default" size="100%">1st Euro-Mediterranean Conference for Environmental Integration (EMCEI) Springer, Sousse. Tunisia</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.emcei.net</style></url></web-urls></urls><pub-location><style face="normal" font="default" size="100%">Sousse. Tunisia</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Qualité chimique des eaux de l&amp;rsquo;aquifère Moi-pliocène utilisé pour l&amp;rsquo;irrigation de la plaine d&amp;rsquo;El Outaya au sud Algérien</style></title><secondary-title><style face="normal" font="default" size="100%">Colloque International Eau-Société-Climat 2017(ESC- 2017) Hammamet 2-3-4 Octobre </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Zouaoui Siham</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">Bouabid Abd Ennasser</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Qualité des eaux du Complexe Terminale du Nord-Est Algérien. Région de Tolga</style></title><secondary-title><style face="normal" font="default" size="100%">The 1St Atlas Georessources International Congress, (AGIC). 20-22 March, Hammet, Tunisia.</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><pub-location><style face="normal" font="default" size="100%"> Hammet, Tunisia.</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Benzagouta Mohammed Said</style></author><author><style face="normal" font="default" size="100%">Belhouchet Houssam</style></author><author><style face="normal" font="default" size="100%">Achi. N</style></author><author><style face="normal" font="default" size="100%">Amro.M</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Rock Typing: Reservoir Determination from rock &amp;ndash; fluid interaction and dynamic behavior : Case Study from an Algerian Oil Field Reservoir</style></title><secondary-title><style face="normal" font="default" size="100%">DGMK/ÖGEW-Frühjahrstagung, Fachbereich Aufsuchung und Gewinnung Celle, 5./6. April</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;
	Rock typing is a process of rock classification based on mineralogical composition, grainshape pore size distribution (PSD) and communication. In addition to rock-fluid interaction, dynamic behavior and the capillary effect are also considered. In that purpose data need process involve: integrating, analyzing and synthesizing data brought out from different source: Petrophysics, cores analysis, well tests, MDT tooland production profiles. Achievement of rock typing reservoir based on fluid - solid behavior and their relation constitute an important issue not only for making distinguished different rock types but also for fluid gas contacts.&lt;br&gt;For the case study, our investigation is concerned with the determination of the rock type dynamism resulting in reservoir rocks having similar dynamic behavior. Outcome from this process is to establish a representative petrophysical model able to predict any effect own to the change of the rock properties or fluid characteristics. Establishment of numerical model in&amp;nbsp; that context, and its relative changes can be ascribed to rapid petrophysical variation characteristics: related to pore size, geometry, grain size distribution, fluid behavior and circulation with essential reference to permeability. This latter can affect the simulation time and consequently, the accuracy in the calculation process.
&lt;/p&gt;

&lt;p&gt;
	In this conducted investigation, application of linear regression method is involving permeability and porosity core measurement, stressing on their coefficient of correlation. Results have led to different clusters classification according to the linearity regarding permeability-porosity changes. Extrapolation can be made for the non-cored reservoir sections or non-cored boreholes associated to the considered field. In that principle geological models can be set.
&lt;/p&gt;

&lt;p&gt;
	Application of these listed method for TAGI (TriasArgilo-GreseuxInferieur: Lower Shaly – SansdtoneTriasic Formation) in B-H Basin (Algeria) has revealed the presence of six main rock types: sand type 1 (RT-1), sand Type 2 (RT-2), sand type 3 (RT-3), sand type 4 (RT-4), sand type 5 (RT-5) and sand type 6 (RT-6).
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Defaflia Nabil</style></author><author><style face="normal" font="default" size="100%">Boushaba Abdellah</style></author><author><style face="normal" font="default" size="100%">Marmi Ramdane</style></author><author><style face="normal" font="default" size="100%">Dardakhe Mohamed</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Malika</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation géologique et apport de la géophysique pour la mobilisation des ressources hydrique dans le bassin d&amp;#39;Ain Djasser (Sud-setifien, Algérien NE)</style></title><secondary-title><style face="normal" font="default" size="100%">Colloque international Eau–Société–Climat’2017 (ESC-2017), Hammamet, Tunis le 2, 3 et 4 Octobre .</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><pub-location><style face="normal" font="default" size="100%">Hammamet, Tunis</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Bilalite Halima</style></author><author><style face="normal" font="default" size="100%">Ghenima Z</style></author><author><style face="normal" font="default" size="100%">Teffaha S</style></author><author><style face="normal" font="default" size="100%">Kihel K</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Impacts des plans d&amp;#39;Eau sur les régimes hydro-climatiques a l&amp;#39;échelle d&amp;#39;un bassin verssant, cas du barrage de Beni Haroun, Milan Est Algerien</style></title><secondary-title><style face="normal" font="default" size="100%">Colloque international Eau–Société–Climat’2017 (ESC-2017), Hammamet, Tunis le 2, 3 et 4 Octobre</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><pub-location><style face="normal" font="default" size="100%">Hammamet, Tunis</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Géométrie de l&amp;rsquo;aquifère Néogène dans le bassin d&amp;rsquo;El-Outaya, Atlas saharien au sud algérien </style></title><secondary-title><style face="normal" font="default" size="100%">Colloque international Eau–Société–Climat’2017 (ESC-2017), Hammamet, Tunis le 2, 3 et 4 Octobre </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><pub-location><style face="normal" font="default" size="100%">Hammamet, Tunis </style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Qualité chimique des eaux de l&amp;rsquo;aquifère Mio-pliocène utilisées pour l&amp;rsquo;irrigation de la plaine d&amp;rsquo;El-Outaya au sud algérien</style></title><secondary-title><style face="normal" font="default" size="100%">Colloque international Eau–Société–Climat’2017 (ESC-2017),Hammamet, Tunis le 2, 3 et 4 Octobre </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><pub-location><style face="normal" font="default" size="100%">Hammamet, Tunis </style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Boulahbal Souad</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation des écoulements souterrains dans le socle precambrien fissure  de la region de tamanrasset</style></title><secondary-title><style face="normal" font="default" size="100%">The 1st international symposium WREIANA, Gafsa 24-26 mars </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><pub-location><style face="normal" font="default" size="100%"> Gafsa </style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Boulahbal Souad</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude des ecoulements souterrains dans les gneiss schisteux fissurés du précambrien de la region de tamanrasset</style></title><secondary-title><style face="normal" font="default" size="100%">The 1st Atlas Georesources International Congress, Hammamet, tunisia 20-22 mars</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><pub-location><style face="normal" font="default" size="100%">Hammamet, tunisia</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Mansouri Zineb</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Assessment of water requirements of olive and apricots trees in Tinibaouine region (north-eastern of Algeria). Impacts of Global Change on Western Mediterranean Aquifers,</style></title><secondary-title><style face="normal" font="default" size="100%">Proceedings Congress on Groundwater and Global Change in the Western Mediterranean, Granada </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://www.aih-ge.org/index.php/gwm-change-2017/</style></url></web-urls></urls><pub-location><style face="normal" font="default" size="100%">Granada </style></pub-location><pages><style face="normal" font="default" size="100%">pp 277-282</style></pages><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Bilalite Halima</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Influence des variations climatiques sur les réserves d&amp;rsquo;eau souterraine des plaines de Zana Chott Saboun et Gadaine (Nord-Est Algérien)</style></title><secondary-title><style face="normal" font="default" size="100%">Proceedings Congress on Groundwater and Global Change in the Western Mediterranean Granada. Impacts of Global Change on Western Mediterranean Aquifers</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://www.aih-ge.org/index.php/gwm-change-2017/</style></url></web-urls></urls><pub-location><style face="normal" font="default" size="100%">Granada</style></pub-location><pages><style face="normal" font="default" size="100%">pp 171-176</style></pages><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">BOUHADEB</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">BOUGUERRA H</style></author><author><style face="normal" font="default" size="100%">DERDOUS O</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Assessing soil loss using GIS based RUSLE methodology. Case of the Bou Namoussa watershed &amp;ndash; North-East of Algeria, 2018, PL ISSN 1429&amp;ndash;7426., Polish Academy of Sciences (PAN), Committee on Agronomic Sciences, Degruyte, DOI: 10.2478/jwld-2018</style></title><secondary-title><style face="normal" font="default" size="100%">Journal of Water and Land Development </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://www.itp.edu.pl/wydawnictwo/journal/36_2018_I_III/Bouhadeb.pdf</style></url></web-urls></urls><pages><style face="normal" font="default" size="100%">pp 27–35</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;span style=&quot;left:131.333px;top:688.416px;14.9711px;serif;transform:scaleX(1.00015);&quot;&gt;This study aims to estimating annual soil erosion rate and its &lt;/span&gt;&lt;span style=&quot;left:497.629px;top:688.416px;14.9711px;serif;transform:scaleX(1.00136);&quot;&gt;spatial distribution in the Bou Namoussa water-&lt;/span&gt;&lt;span style=&quot;left:105.963px;top:705.538px;14.9711px;serif;transform:scaleX(1.03121);&quot;&gt;shed located in the North-East of Algeria by applying the revis&lt;/span&gt;&lt;span style=&quot;left:493.416px;top:705.538px;14.9711px;serif;transform:scaleX(1.02336);&quot;&gt;ed universal soil loss equation (RUSLE) within &lt;/span&gt;&lt;span style=&quot;left:105.963px;top:722.751px;14.9711px;serif;transform:scaleX(0.998512);&quot;&gt;a Geographical Information System environment (GIS). The applic&lt;/span&gt;&lt;span style=&quot;left:507.581px;top:722.751px;14.9711px;serif;transform:scaleX(0.999618);&quot;&gt;ation of the RUSLE model in different natural &lt;/span&gt;&lt;span style=&quot;left:105.963px;top:739.963px;14.9711px;serif;transform:scaleX(1.00806);&quot;&gt;environments and on every scale takes into account five key fac&lt;/span&gt;&lt;span style=&quot;left:491.354px;top:739.963px;14.9711px;serif;transform:scaleX(1.01094);&quot;&gt;tors namely: the rainfall erosivity, the soil erodi-&lt;/span&gt;&lt;span style=&quot;left:105.963px;top:757.085px;14.9711px;serif;transform:scaleX(1.03489);&quot;&gt;bility, the steepness and length of slopes, the vegetation cove&lt;/span&gt;&lt;span style=&quot;left:482.837px;top:757.085px;14.9711px;serif;transform:scaleX(1.02999);&quot;&gt;r and the conservation support practices. Each of &lt;/span&gt;&lt;span style=&quot;left:105.963px;top:774.298px;14.9711px;serif;transform:scaleX(1.01278);&quot;&gt;these factors was generated in GIS as a raster layer, their com&lt;/span&gt;&lt;span style=&quot;left:478.982px;top:774.298px;14.9711px;serif;transform:scaleX(1.01092);&quot;&gt;bination, resulted in the development of a soil loss &lt;/span&gt;&lt;span style=&quot;left:105.963px;top:791.42px;14.9711px;serif;transform:scaleX(0.988245);&quot;&gt;map indicating an average erosion rate of 7.8 tꞏha&lt;/span&gt;&lt;span style=&quot;left:407.536px;top:789.41px;9.68188px;serif;transform:scaleX(1.00157);&quot;&gt;–1&lt;/span&gt;&lt;span style=&quot;left:417.217px;top:791.42px;14.9711px;serif;transform:scaleX(0.612241);&quot;&gt;ꞏy&lt;/span&gt;&lt;span style=&quot;left:429.678px;top:789.41px;9.68188px;serif;transform:scaleX(1.00157);&quot;&gt;–1&lt;/span&gt;&lt;span style=&quot;left:439.36px;top:791.42px;14.9711px;serif;transform:scaleX(1.01647);&quot;&gt;. The obtained soil loss map was classified into four ero-&lt;/span&gt;&lt;span style=&quot;left:105.963px;top:808.632px;14.9711px;serif;transform:scaleX(1.02139);&quot;&gt;sion severity classes; low, moderate, high and very high severi&lt;/span&gt;&lt;span style=&quot;left:487.32px;top:808.632px;14.9711px;serif;transform:scaleX(1.01543);&quot;&gt;ty representing respectively 40, 30.48, 22.59 and &lt;/span&gt;&lt;span style=&quot;left:105.963px;top:825.845px;14.9711px;serif;transform:scaleX(1.01372);&quot;&gt;6.89% of the total surface. The a&lt;/span&gt;&lt;span style=&quot;left:303.993px;top:825.845px;14.9711px;serif;transform:scaleX(1.00953);&quot;&gt;reas, showing moderate, high a&lt;/span&gt;&lt;span style=&quot;left:491.893px;top:825.845px;14.9711px;serif;transform:scaleX(1.00919);&quot;&gt;nd very high erosion rates which represent more &lt;/span&gt;&lt;span style=&quot;left:105.963px;top:842.967px;14.9711px;serif;transform:scaleX(1.0084);&quot;&gt;than half of the basin area were found generally located in reg&lt;/span&gt;&lt;span style=&quot;left:480.148px;top:842.967px;14.9711px;serif;transform:scaleX(1.00558);&quot;&gt;ions having high erodibility soils, steep slopes and &lt;/span&gt;&lt;span style=&quot;left:105.963px;top:860.179px;14.9711px;serif;transform:scaleX(1.01828);&quot;&gt;low vegetation cover. These areas should be considered as prior&lt;/span&gt;&lt;span style=&quot;left:494.403px;top:860.179px;14.9711px;serif;transform:scaleX(1.01575);&quot;&gt;ities in future erosion control programs in order &lt;/span&gt;&lt;span style=&quot;left:105.963px;top:877.392px;14.9711px;serif;transform:scaleX(0.998794);&quot;&gt;to decrease the siltation rate&lt;/span&gt;&lt;span style=&quot;left:272.795px;top:877.392px;14.9711px;serif;transform:scaleX(1.00459);&quot;&gt; in the Cheffia reservoir. &lt;/span&gt;</style></abstract><issue><style face="normal" font="default" size="100%">No. 36 (I–III)</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJEMMAL S</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">CHAMEKH K</style></author><author><style face="normal" font="default" size="100%">BAALI F</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">The contribution of fracturations in the emergence of the thermal springs in Setif city, Eastern Algeria, Carbonates Evaporites</style></title><secondary-title><style face="normal" font="default" size="100%">Springer</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.researchgate.net/publication/318603314_The_contribution_of_fracturations_in_the_emergence_of_the_thermal_springs_in_Setif_city_Eastern_Algeria</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Setif city covers an area of 6550&amp;nbsp;km&lt;sup&gt;2&lt;/sup&gt;; it is located about 300&amp;nbsp;km southeast of Algiers and 100&amp;nbsp;km to the south of the Mediterranean sea. The aim of our study is to know the tectonic mechanisms responsible for the emergencies and to highlight their chemical characteristics of water springs in Setif. Wherein thermalism is characterized by the presence of a number of thermal springs, the latest are usually related to recent large fractures deeply affecting the sedimentary formations and sometimes even crystallin basement. These fractures are often injected by Triassic evaporates; their directions are NNW–SSE, NW–SE, and NE–SW and limiting great structural units. Four groundwater facies were identified: the high percentage of sources, staking major accidents related to limestone mountains or to the basement, shows a calcium or sodium sulfate facies; and the sources are often hot (meso or hyperthermal). A second group, related to terrigenous saliferous formations, shows a sodium bicarbonate or sodium chloride facies. The geothermic interpretation allows us to conclude that the reservoir supplies the two aquifer systems of the thermal complex, and is stored in fissured Jurassic limestone, where water storage and circulation is beyond 2600&amp;nbsp;m deep.</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Mensouri Z</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Assessment of the water needs of apricot and olive crops under arid climatic conditions: case study of Tinibaouine Region (northeast of Algeria), Special Issue on Science, Engineering &amp;amp; Environment, ISSN: 2186-2990, Japan. Feb,2017</style></title><secondary-title><style face="normal" font="default" size="100%">International Journal of GEOMATE</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.geomatejournal.com/sites/default/files/articles/46-52-160424-Zineb-Feb-2017.pdf</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%"> Vol. 12</style></volume><pages><style face="normal" font="default" size="100%">pp. 46 - 52. </style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;span style=&quot;left:237.991px;top:383.527px;16.6px;serif;transform:scaleX(1.01562);&quot;&gt;The Tinibaouine region, located in north&lt;/span&gt;&lt;span style=&quot;left:515.194px;top:383.527px;16.6px;serif;transform:scaleX(1.01416);&quot;&gt;-eastern Algeria on the borders of the Batna&lt;/span&gt;&lt;span style=&quot;left:810.392px;top:383.527px;16.6px;serif;transform:scaleX(1.00298);&quot;&gt;-Belezma &lt;/span&gt;&lt;span style=&quot;left:141.794px;top:402.534px;16.6px;serif;transform:scaleX(1.01773);&quot;&gt;Mountains, is characterized by a semi&lt;/span&gt;&lt;span style=&quot;left:397.201px;top:402.534px;16.6px;serif;transform:scaleX(1.02308);&quot;&gt;-arid to arid climate with an average annual rainfall not exceeding 465 &lt;/span&gt;&lt;span style=&quot;left:141.794px;top:421.741px;16.6px;serif;transform:scaleX(0.931907);&quot;&gt;mm and an average annual temperature of around 22 ° C. This region is char&lt;/span&gt;&lt;span style=&quot;left:670.188px;top:421.741px;16.6px;serif;transform:scaleX(1.03469);&quot;&gt;acterized by the cultivation of &lt;/span&gt;&lt;span style=&quot;left:141.794px;top:440.947px;16.6px;serif;transform:scaleX(1.01482);&quot;&gt;apricots as essential crop followed by th&lt;/span&gt;&lt;span style=&quot;left:412.191px;top:440.947px;16.6px;serif;transform:scaleX(1.01725);&quot;&gt;at of olives, whose plots are all irrigated with the Tinibaouine spring &lt;/span&gt;&lt;span style=&quot;left:141.794px;top:460.153px;16.6px;serif;transform:scaleX(1.01054);&quot;&gt;water. These are 450 Ha of trees for apricot and 108 Hectare&lt;/span&gt;&lt;span style=&quot;left:546.801px;top:460.153px;16.6px;serif;transform:scaleX(1.00782);&quot;&gt; for olives which constitute the principal revenue &lt;/span&gt;&lt;span style=&quot;left:141.794px;top:479.359px;16.6px;serif;transform:scaleX(0.953916);&quot;&gt;of the citizens of this small village. This paper estimated the crop refe&lt;/span&gt;&lt;span style=&quot;left:631.394px;top:479.359px;16.6px;serif;transform:scaleX(0.97168);&quot;&gt;rence and actual evapotranspiration &lt;/span&gt;&lt;span style=&quot;left:141.794px;top:498.565px;16.6px;serif;transform:scaleX(0.956391);&quot;&gt;(ETO) respectively and the irrigation water requirement of apricot trees an&lt;/span&gt;&lt;span style=&quot;left:654.601px;top:498.565px;16.6px;serif;transform:scaleX(0.939249);&quot;&gt;d olive tree&lt;/span&gt;&lt;span style=&quot;left:732.604px;top:498.565px;16.6px;serif;transform:scaleX(0.937488);&quot;&gt;s. The long recorded &lt;/span&gt;&lt;span style=&quot;left:141.81px;top:517.572px;16.6px;serif;transform:scaleX(0.951769);&quot;&gt;climatic data, crop and soil data, effective water allocation and planning, the information about crop water &lt;/span&gt;&lt;span style=&quot;left:141.81px;top:536.779px;16.6px;serif;transform:scaleX(1.00641);&quot;&gt;req&lt;/span&gt;&lt;span style=&quot;left:163.208px;top:536.779px;16.6px;serif;transform:scaleX(0.949313);&quot;&gt;uirements, irrigation withdrawals were computed with the Cropwat model which is based on the United &lt;/span&gt;&lt;span style=&quot;left:141.81px;top:555.985px;16.6px;serif;transform:scaleX(1.0089);&quot;&gt;Nations’ Food and Agriculture Organization (FAO), the Penman&lt;/span&gt;&lt;span style=&quot;left:574.008px;top:555.985px;16.6px;serif;transform:scaleX(1.01081);&quot;&gt;-Monteith method was used to estimate ETo. &lt;/span&gt;&lt;span style=&quot;left:141.81px;top:575.191px;16.6px;serif;transform:scaleX(0.977037);&quot;&gt;Crop coefficients (Kc) from the phenomenological stag&lt;/span&gt;&lt;span style=&quot;left:525.204px;top:575.191px;16.6px;serif;transform:scaleX(0.957203);&quot;&gt;es of apricot and olive were applied to adjust and &lt;/span&gt;&lt;span style=&quot;left:141.81px;top:594.397px;16.6px;serif;transform:scaleX(1.01635);&quot;&gt;estimate the actual evapotranspiration ETc through a water balance of the irrigation water requirements (IR). &lt;/span&gt;&lt;span style=&quot;left:141.81px;top:613.603px;16.6px;serif;transform:scaleX(1.02307);&quot;&gt;The results showed that the&lt;/span&gt;&lt;span style=&quot;left:327.813px;top:613.603px;16.6px;serif;transform:scaleX(1.02412);&quot;&gt; annual reference evapotranspiration (ETO) was estimated at &lt;/span&gt;&lt;span style=&quot;left:745.005px;top:613.603px;16.6px;serif;transform:scaleX(1.00205);&quot;&gt;3.71mm&lt;/span&gt;&lt;span style=&quot;left:799.801px;top:613.603px;16.6px;serif;transform:scaleX(0.966408);&quot;&gt; / day. The &lt;/span&gt;&lt;span style=&quot;left:141.794px;top:632.61px;16.6px;serif;transform:scaleX(0.983996);&quot;&gt;irrigation requirements were estimated at 35800 &lt;/span&gt;&lt;span style=&quot;left:482.5917999999999px;top:632.6104000000004px;16.6px;serif;&quot;&gt;m&lt;/span&gt;&lt;span style=&quot;left:495.2px;top:632.768px;10.799999999999999px;serif;&quot;&gt;3&lt;/span&gt;&lt;span style=&quot;left:500.6px;top:632.536px;16.6px;serif;transform:scaleX(0.989751);&quot;&gt;/ hectare&lt;/span&gt;&lt;span style=&quot;left:560.609px;top:632.536px;16.6px;serif;transform:scaleX(0.973416);&quot;&gt; for apricot, 6980 &lt;/span&gt;&lt;span style=&quot;left:691.8154px;top:632.5359999999998px;16.6px;serif;&quot;&gt;m&lt;/span&gt;&lt;span style=&quot;left:704.3999999999999px;top:632.768px;10.799999999999999px;serif;&quot;&gt;3&lt;/span&gt;&lt;span style=&quot;left:709.8px;top:632.536px;16.6px;serif;transform:scaleX(0.984352);&quot;&gt;/ hectare &lt;/span&gt;&lt;span style=&quot;left:776.598px;top:632.536px;16.6px;serif;transform:scaleX(0.965348);&quot;&gt;for olive, also &lt;/span&gt;&lt;span style=&quot;left:141.798px;top:651.742px;16.6px;serif;transform:scaleX(1.00386);&quot;&gt;Irrigation needs estimated on land at &lt;/span&gt;&lt;span style=&quot;left:389.005px;top:651.742px;16.6px;serif;transform:scaleX(1.009);&quot;&gt;14185, 05&lt;/span&gt;&lt;span style=&quot;left:455.803px;top:651.742px;16.6px;serif;transform:scaleX(1.00281);&quot;&gt; m&lt;/span&gt;&lt;span style=&quot;left:472.59999999999997px;top:651.968px;10.799999999999999px;serif;&quot;&gt;3&lt;/span&gt;&lt;span style=&quot;left:478px;top:651.736px;16.6px;serif;transform:scaleX(1.00541);&quot;&gt;/ hectare &lt;/span&gt;&lt;span style=&quot;left:539.204px;top:651.736px;16.6px;serif;transform:scaleX(1.00584);&quot;&gt;for olive and apricot&lt;/span&gt;</style></abstract><issue><style face="normal" font="default" size="100%">Issue 30</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Belaloui souad</style></author><author><style face="normal" font="default" size="100%">Seba sakina</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">les caracteristiques physicovhimiques des eaux de continentale intercalaire et de complexe ternimale daans la région d&amp;#39;oued Righ</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Nezzar Badreddine</style></author><author><style face="normal" font="default" size="100%">Bezai Abderahim</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution hydrogéologique de la plaine de Ain Djasser</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Guetafi Anfal</style></author><author><style face="normal" font="default" size="100%">Touati Zina</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude Téctono- sédimentaire de la série Campanienne de Dj. Lekhal (Plaine d&amp;rsquo;Ain-Touta)</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Benmansour Sana</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">La série compano-maestrichtienne de l&amp;rsquo;anticlinal de Djebel El Azreg : Lithostratigraphie, Paléodiversité et Sédimentologie (Aurès, Algérie oriental</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Khelil.M</style></author><author><style face="normal" font="default" size="100%">Fedel.W</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude de la qualité des eaux souterraines de la nappe profonde destinées a l&amp;rsquo;irrigation cas de la région de Tolga (W de Biskra)</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Boukhnissa.F</style></author><author><style face="normal" font="default" size="100%">Ahmadi. L</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude de la qualité des eaux souterraines de la nappe du quaternaire de la région de Tolga (W de Biskra)</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Mansouri Zineb</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude hydrogéologique et gestion intégrée des eaux de la source de Tinibaouine (Wilaya de Batna -NE Algérien)</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://www.secheresse.info/spip.php?article67759</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">La région de Tinibaouine est située au Nord-est de l’Algérie, en bordure Septentrionale des Monts de Batna-Belezma, Elle est caractérisée par un climat de type semi-aride à aride avec une précipitation moyenne annuelle qui n’excède pas 465mm, et une température moyenne annuelle de l’ordre de 22°C. Cette région est caractérisée par la culture de l’abricot comme culture essentielle suivie des olives, dont les parcelles sont toutes irriguées à partir de la source. Il s’agit en effet de 450 Ha d’arbres destinés à l’abricotier et de 108 Ha aux olives. L’émergence naturelle des eaux qui ont pour le réservoir Dj. Refaa situé en contrefort Sud de la plaine de Tinibaouine où émerge la source. Son débit actuel est de l’ordre de 100 à 110 l/s (mesuré en Mars 2015) alors qu’il pouvait atteindre 200 l/s par le passé en 1971. L’objectif de ce travail est de cerner les contraintes naturelles et anthropiques ayant une incidence directe sur l’usage de la source et de chercher le mode de gestion approprié, qui tienne compte non seulement des solutions techniques qui s’inspire également des règles sociales qui régissent l’usage et les conflits qui leurs sont liés.</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Mekaoussi Adel</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">ORIGINES ET MÉCANISMES D&amp;#39;ACQUISITION DE LA MINERALISATION DES EAUX SOUTERRAINES EXPLOITEES DANS LES AURES.  Cas de la vallée de l&amp;rsquo;Oued Abdi (w) de Batna (Nord-Est Algérien)</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Slami Rafika</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Stratigraphie, géochimie et réponses microfaunistiques aux changement environnementals autour de la limite Cénomanien-Turonien dans les monts Bellezma-Batna, NE Algérie</style></title><secondary-title><style face="normal" font="default" size="100%">Le 1er Colloque International sur la géologie de la chaîne des Maghrébides et des régions voisines (CIGCM 2016), Université Ferhat Abbas -Sétif 1</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Slami Rafika</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude micropaléontologique (foraminifères, ostracodes) et paléoenvironnementale de la limite Cénomano-Turonienne dans les monts de Batna (Exemple : coupe de Thénièt El Manchar, Nord-Est Algérie)</style></title><secondary-title><style face="normal" font="default" size="100%">1st Arabian Geosciences Union International Conference AIC1, USTHB Alger </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Intérêt de l&amp;rsquo;étude géologique et hydrogéologique pour la mobilisation des ressources hydriques dans le bassin de Timgad (Aurès, algérie NE)</style></title><secondary-title><style face="normal" font="default" size="100%">Le 1er séminaire national sur l’eau et l’environnement (SNEE, 2016). Mila, Algérie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Belalit Halima</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Les variations climatiques sur les eaux souterraines de la plaine de Gadaine (nord-est algérien)</style></title><secondary-title><style face="normal" font="default" size="100%">1er Séminaire National sur l'eau</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Lebchek Soumia</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Approche hydrogéologique du bassin néogène de Timgad, NE algérien</style></title><secondary-title><style face="normal" font="default" size="100%">2nd Ionternational conference on water resources, ICWR, Ouragla, 21-22 Nov </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Rihani Abla</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation hydrochimique et isotopique des eaux souterraines du sous bassin de Oued Labiod, massif des aurès, NE Algérien </style></title><secondary-title><style face="normal" font="default" size="100%">5ème conférence internationale du réseau eaux et climats, Fes, 12-13 Oct </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">IWRM in north Eastern Batna plains</style></title><secondary-title><style face="normal" font="default" size="100%">43rd IAH congress, Montpellier 25-29 sept</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">www.iah.org</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Benmansour Sana</style></author><author><style face="normal" font="default" size="100%">Yahiaoui Abdelouahab</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">The Campaniane Maastrichtian of the Aures basin, Algeria  Paleobiogeographical distrubution of Ostracods</style></title><secondary-title><style face="normal" font="default" size="100%">Elsevier Cretaceous Research </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.1016/j.cretres.2015.09.015</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Vol. 58</style></volume><pages><style face="normal" font="default" size="100%">pp.86-107</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">A detailed biostratigraphic study of four sections (El Kantara, Menaa, Tighanimine and El Gaâga) in the Campanian–Maastrichtian of the Aures Basin in Algeria allows the identification of 109&amp;nbsp;&lt;a href=&quot;https://www.sciencedirect.com/topics/earth-and-planetary-sciences/ostracod&quot; title=&quot;Learn more about Ostracod from ScienceDirect's AI-generated Topic Pages&quot;&gt;ostracod&lt;/a&gt;&amp;nbsp;species belonging to 50 genera. From a biochronostratigraphic point of view, none of the identified ostracod assemblages are typically restricted to the&amp;nbsp;&lt;a href=&quot;https://www.sciencedirect.com/topics/earth-and-planetary-sciences/campanian&quot; title=&quot;Learn more about Campanian from ScienceDirect's AI-generated Topic Pages&quot;&gt;Campanian&lt;/a&gt;&amp;nbsp;or to the&amp;nbsp;&lt;a href=&quot;https://www.sciencedirect.com/topics/earth-and-planetary-sciences/maastrichtian&quot; title=&quot;Learn more about Maastrichtian from ScienceDirect's AI-generated Topic Pages&quot;&gt;Maastrichtian&lt;/a&gt;, but rather characterize a range covering the Campanian–Maastrichtian. As regards the paleobiogeography, the presence of species in common between Algeria and other countries or regions enables us to compile four maps showing the distribution of two provinces that developed during the Santonian-Paleocene, i) the South-West and South Tethyan Margins Province, including North Africa, the Middle East and Arabian Peninsula, and ii) the East Atlantic Margin Province, bordering West and Central-West Africa. We can also recognize relationships between the different regions making up these provinces, which remained under more or less arid, subtropical to tropical climates, with ostracods migrating according to the directions of ocean currents during the&amp;nbsp;&lt;a href=&quot;https://www.sciencedirect.com/topics/earth-and-planetary-sciences/late-cretaceous&quot; title=&quot;Learn more about Late Cretaceous from ScienceDirect's AI-generated Topic Pages&quot;&gt;Late Cretaceous&lt;/a&gt;. The&amp;nbsp;&lt;a href=&quot;https://www.sciencedirect.com/topics/earth-and-planetary-sciences/dispersal&quot; title=&quot;Learn more about Dispersal from ScienceDirect's AI-generated Topic Pages&quot;&gt;dispersal&lt;/a&gt;&amp;nbsp;of the ostracods reflects marine communication between these provinces and India, the southern USA and Jamaica, Brazil and Europe.</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Naji Hossein</style></author><author><style face="normal" font="default" size="100%">Meddour Taib</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Étude géologique de la plaine d&amp;rsquo;El Mather par une approche géophysique.</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Derdakhe Mohamed</style></author><author><style face="normal" font="default" size="100%">Baci Maamer</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Étude géologique de la plaine d&amp;rsquo;Ain Djasser par une approche géophysique.</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Beldjani I</style></author><author><style face="normal" font="default" size="100%">Henni Y</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Traitement des eaux salées -par osmose inverse- pour la production d&amp;#39;eau potable dans le sud algérien / Unité de déminéralisation de Touggourt</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Dif H</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à une étude Comparative entre    la qualité des eaux du Complexe Terminal et du Continental Intercalaire dans la région D&amp;rsquo;EL-OUED.</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Djenba Samir</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">water resources in a semi-arid country case aïn djasser northeast Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">Desalination for Environment : Clean Water and Energy May22–26, Rome-Italy</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><pub-location><style face="normal" font="default" size="100%"> Rome-Italy</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Djenba Samir</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">les problèmes de mouvement de sols nord de wilaya de Sétif</style></title><secondary-title><style face="normal" font="default" size="100%">1er colloque international sur la géologie de la chaine maghrébides et des régions limitrophes Sétif </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">khadidja A</style></author><author><style face="normal" font="default" size="100%">Djenba Samir</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">hydrodynamic caracreization of ground of the region of Tadjnenet- Chelghoum aid (eastern algeria)</style></title><secondary-title><style face="normal" font="default" size="100%">International conference on Applied Geology and Environment May19–21, Mahdia-  Tunisia</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><pub-location><style face="normal" font="default" size="100%">Mahdia-  Tunisia</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Djenba Samir</style></author><author><style face="normal" font="default" size="100%">khadidja A</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Study of the instability of the land : typology and mapping cases of the wilaya of setif (eastern algeria)</style></title><secondary-title><style face="normal" font="default" size="100%">International conference on Applied Geology and Environment May19–21 Mahdia-  Tunisia</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><pub-location><style face="normal" font="default" size="100%">Mahdia-  Tunisia</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Belloula Moufida</style></author><author><style face="normal" font="default" size="100%">Drias Tarek</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Assessment of groundwater quality in the plain of ichemoul using the geomatics approach</style></title><secondary-title><style face="normal" font="default" size="100%">ISER-78th International Conference on Chemical and Environmental Science (ICCES) Zurich, Switzerland November 22nd -23rd</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><pub-location><style face="normal" font="default" size="100%">Zurich, Switzerland </style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Drias Tarek</style></author><author><style face="normal" font="default" size="100%">Belloula Moufida</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Hydrogeochemical assessment of an alluvial aquifer under semi-arid climat. Eastern Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">ISER-78th International Conference on Chemical and Environmental Science (ICCES) Zurich, Switzerland November 22nd -23rd </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><pub-location><style face="normal" font="default" size="100%">Zurich, Switzerland </style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Djenba Samir</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Les problèmes de mouvements de sols au nord de la wilaya de Setif</style></title><secondary-title><style face="normal" font="default" size="100%">1er colloque international sur la géologie de la chaine des maghrébides et des régions voisines (CIGCM 2016), université Ferhat Abbas Setif1 Setif, Alger</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><pub-location><style face="normal" font="default" size="100%">Setif, Alger</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Cheriet Manel</style></author><author><style face="normal" font="default" size="100%">Benzagouta Mohamed Said</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">CONTROLE DES CARACTERISTIQUES PETROPHYSIQUES DES RESERVOIR CARBONATES: CAS DU CONIACIEN &amp;ndash;SANTONIEN(SUD EST CONSTANTINOIS)</style></title><secondary-title><style face="normal" font="default" size="100%">Sciences &amp; Technologie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://revue.umc.edu.dz/index.php/d/article/view/2148/2291</style></url></web-urls></urls><pages><style face="normal" font="default" size="100%">pp 27-40</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Investigation on oil reservoirs is up to several approaches under different aspects. oilreservoir is dependent on several approaches in different aspects. Distinct settings may be considered for the qualitative and quantitative reservoir evaluation. Control on potential reservoir accumulation is related to permeability and poroslty, in addition to diagenetic and petrographic effects. ln the case study, the considered reservoir is dealing with Cretaceous Carbonate series of ConiacianSantonian age located in the South East of Constantine area (Sud-Est Constontinois). From exploration and evaluation point of view, the oil potential, in the cited area levels, remains almost unexplored. Based on logging and drilling collected data indicates that the approached level of Coniancian -Santonian age can be a tight type. Evidences is from the permeability which is ranging from 0.1 md to 50 md and porosity stretching from lYo up to 16%o. Thus, contribution of tectonic effect is minimized. In the same harmony is the diagenetic and petrographic attitude which is responsible for the compaction and lesser dissolution with occlusion mostly of the intergranular.</style></abstract><issue><style face="normal" font="default" size="100%">N°43</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Aoun Mounira</style></author><author><style face="normal" font="default" size="100%">Benzagouta Mohamed Said</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Expansive And Aggressive Soil Characteristics And Their Impact On Building Construction: Case Of El Kouif City (tebessa, Algeria)</style></title><secondary-title><style face="normal" font="default" size="100%">Bulletin du Service Géologique de l'Algérie </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://asga.dz/wp-content/uploads/2019/01/Bulletin-vol-27-2016.pdf</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Volume 27</style></volume><pages><style face="normal" font="default" size="100%">pp 105-121 </style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Prediction of soil swelling characteristics and accurate quality estimation can be of a great consideration and contribution regarding the site stability. Any concerned investigation is correspondingly an advanced priority for the project realization. Related inquiries allow potential reduction concerning financial and technical charges damage prior to any urban development. The determination of soil characteristics lead for a better recognition, and allow to make the best choice of foundation type adopted for each site. Thus, in any urban case study, much gain can be made by team work recording and surveying the related data. In the considered city of El Kouif, located in Tebessa (Algeria), several buildings have been mainly built on expansive soils. Observations indicate different severe damages which were caused mostly in the nearby structures. These damages are characterized by deflection and failure of walls. Lateral and vertical displacements evidences support the presence of shear movements and subsidence. The scale up of these movements occurrence can reach millimetric shifting dimension. Ground and subsurface risk activity affecting El Kouif city site are also related to the presence of destructive chemical components such as sulfates. The sulfate occurrence is illustrated through generally gypsum minerals concentration present in the concerned soil. During building projects, these soils, in meeting concrete and in presence of water, are source of new mineral generation such as ettringite. It consists on the assemblage of water and sulfate in addition to calcium. Source for these chemical products expansion might be associated to historical event: the city of El Kouif was the field of phosphates mining area in addition to established phosphate extraction plant. Thus, determination of soil characteristics and involvement of chemical components turn out to be the main objectives in this investigation.</style></abstract><issue><style face="normal" font="default" size="100%">Numéro 1</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Aptitude a l&amp;#39;irrigation par les eaux uses epurees cas de la STEP de Sidi Merouane, willaya de Mila, Est Algerien</style></title><secondary-title><style face="normal" font="default" size="100%">10th international conference for water ressources and water security in the middle East and North Africa, held in Istanbul, Turkey on th 14th-16th November</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><pub-location><style face="normal" font="default" size="100%">Istanbul, Turkey </style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">les impacts climatiques sur les eaux souterraines, cas de la plaine de Zana-Chott saboun, Est Algerien</style></title><secondary-title><style face="normal" font="default" size="100%">10th international conference for water ressources and water security in the middle East and North Africa, held in Istanbul, Turkey on th 14th-16th November</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><pub-location><style face="normal" font="default" size="100%">Istanbul, Turkey</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Defaflia Nabil</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">Marmi Ramdane</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">L&amp;#39;intéret de l&amp;#39;etude géologique et hydrogéologique pour la mobilisation des ressources hydriques dans le bassin de Timgad (Aures, Algerie Nord oriental)</style></title><secondary-title><style face="normal" font="default" size="100%">1er Séminaire National sur l'eau et l'environnement (SNEE 2016), Centre universitaire Abdelhafid Boussouf, Milla, Alger 28-29 novembre</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><pub-location><style face="normal" font="default" size="100%">Milla, Alger</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">Lehchili Nouh</style></author><author><style face="normal" font="default" size="100%">Benchaoui Amine</style></author><author><style face="normal" font="default" size="100%">Benabdelaziz Noureddine</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Aptitude à l&amp;#39;irrigation par les eaux usées épurées, cas de la STEPde Sidi Merouane, willaya de Mila, Est Algerien</style></title><secondary-title><style face="normal" font="default" size="100%">1er Séminaire National sur l'eau et l'environnement (SNEE 2016), Centre universitaire Abdelhafid Boussouf, Milla, Alger 28-29 novembre</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><pub-location><style face="normal" font="default" size="100%">Milla, Alger</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">Bilalite Halima</style></author><author><style face="normal" font="default" size="100%">Bechar Salah-Eddine</style></author><author><style face="normal" font="default" size="100%">Guesmi Hayat</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Fluctuation du niveau piézométrique des eaux souterraines cas de la plaine de Zana-Chott Saboun, Batna Est Algerien</style></title><secondary-title><style face="normal" font="default" size="100%">1er Séminaire National sur l'eau et l'environnement (SNEE 2016), Centre universitaire Abdelhafid Boussouf, Milla, Alger 28-29 novembre</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><pub-location><style face="normal" font="default" size="100%">Milla, Alger</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Anthropogenic pressures on groundwater resources. Case of the Northern plains of Batna region (North-East Algeria)</style></title><secondary-title><style face="normal" font="default" size="100%">43rd IAH  Congress, 25-29 September, Montpellier, France, </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language><issue><style face="normal" font="default" size="100%">Abstract n° 2701. </style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Defaflia N</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">Marmi R</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Geological, Hydrological and Hydrogeological Characterization of the Timgad&amp;rsquo;s Basin (Aures, Algeriane) for the Mobilization of Water Resources</style></title><secondary-title><style face="normal" font="default" size="100%">International Journal of Environment and Water ISSN 2052-3408</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.researchgate.net/publication/330038879_Geological_Hydrological_and_Hydrogeological_Characterization_of_the_Timgad's_Basin_Aures_Algeria_ne_for_the_Mobilization_of_Water_Resources</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Vol 5</style></volume><pages><style face="normal" font="default" size="100%">pp 143</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">The basin of Timgad is located in the Aures. It is characterized by an average annual precipitation which reaches 800 mm. Hydrology tributary of the relief is the direct result of surface water and snowmelt from the heights of the Massif of Chélia. The origin of groundwater: semi-deep to deep aquifer is mainly from the infiltration of precipitation in the geological layers. This rock forms a water table that is intersected by drilling to a depth of 137-400 m giving a flow rate of 6 l / s. and white fractured sandstone forming a confined aquifer 190 m with a flow rate of 28 l / s. The check of geo-electric results of the basin show that the Miocene and Cretaceous layers have important thickness, they are heterogeneous and may contain large aquifer at different levels. The influence of vertical normal faults makes possible an exchange of waters between theses aquifers. The implementation of dam project in the basin will minimize the silting, regulate the flow rate, and contribute to the irrigation of the plain, it can be used for industry too. The objective of this approach is the mobilization of surface water resources decided by the government for a rational and planned of this vital factor which is water. Caractérisation géologique, hydrologique et hydrogéologique du bassin de Timgad (Aurès, Algérie NE), pour la mobilisation des ressources hydriques Résumé : Le bassin de Timgad est située dans les Aurès. Il est caractérisé par une moyenne annuelle des précipitations de l'ordre de 800 mm. L'hydrologie tributaire du relief est la conséquence directe des eaux de surface et de la fonte des neiges provenant des hauteurs du massif de Chélia. L'alimentation de l'eau souterraine des différentes nappes phréatiques profondes à semi-profonde provient essentiellement de l'infiltration des eaux de pluies dans les couches géologiques. Ce cortège de roche forme une nappe libre qui est recoupée par des forages sur une profondeur de 137-400 m fournissant un débit de 6 l/s. et des grés blancs grossiers fracturés formant une nappe captive à 190 m avec un débit de 28 l/s. L'examen des coupes géoélectriques du bassin montrent que les formations du miocène et du crétacé sont dont l'ensemble, épais, hétérogène et susceptible de contenir de grandes potentialités d'aquifères à des niveaux différents. L'influence de failles normales verticales rend possible une éventuelle alimentation des aquifères entres eux. L'importance de l'implantation d'ouvrage de retenue dans le bassin est de minimiser le phénomène d'envasement, de réguler le débit d'écoulement et de contribuer à l'irrigation de la plaine ainsi que l'alimentation des briqueteries. L'objectif de cette approche, est la mobilisation des ressources en eaux superficielles décidée par l'état en vue d'une utilisation rationnelle et planifiée de ce facteur vital qui et l'eau.</style></abstract><issue><style face="normal" font="default" size="100%">Issue 3</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Mensouri Z</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">L&amp;rsquo;étude des caractéristiques hydrodynamiques et la vulnérabilité de la plaine alluvionnaire de Ksar Belezma (Batna - nord-est Algérien), ISSN 1112-3680,Juin 2016</style></title><secondary-title><style face="normal" font="default" size="100%">Larhyss Journal</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.asjp.cerist.dz/en/article/55339</style></url></web-urls></urls><pages><style face="normal" font="default" size="100%">pp. 237-247</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;span style=&quot;left:82.64px;top:914.206px;18.4px;sans-serif;transform:scaleX(0.900078);&quot;&gt;The cartography of the vulnerability in the pollution of subterranean waters &lt;/span&gt;&lt;span style=&quot;left:82.64px;top:935.406px;18.4px;sans-serif;transform:scaleX(0.925887);&quot;&gt;allows identifying zones with high risk of contamination who takes into account &lt;/span&gt;&lt;span style=&quot;left:82.64px;top:956.406px;18.4px;sans-serif;transform:scaleX(0.887344);&quot;&gt;the major part of th&lt;/span&gt;&lt;span style=&quot;left:237.833px;top:956.406px;18.4px;sans-serif;transform:scaleX(0.891738);&quot;&gt;e hydrogeological factors which allocate and control the &lt;/span&gt; &lt;span style=&quot;left:82.64px;top:61.6094px;16.6px;sans-serif;transform:scaleX(0.983122);&quot;&gt;Mansouri Z.&lt;/span&gt;&lt;span style=&quot;left:174.033px;top:61.6094px;16.6px;sans-serif;transform:scaleX(0.944038);&quot;&gt;&amp;amp; al. / Larhyss Journal, 2&lt;/span&gt;&lt;span style=&quot;left:346.6833333333333px;top:61.609399999999866px;16.6px;sans-serif;&quot;&gt;6&lt;/span&gt;&lt;span style=&quot;left:359.283px;top:61.6094px;16.6px;sans-serif;transform:scaleX(0.920009);&quot;&gt;(2016), &lt;/span&gt;&lt;span style=&quot;left:412.117px;top:61.6094px;16.6px;sans-serif;transform:scaleX(0.888087);&quot;&gt;23&lt;/span&gt;&lt;span style=&quot;left:428.71666666666664px;top:61.609399999999866px;16.6px;sans-serif;&quot;&gt;7&lt;/span&gt;&lt;span style=&quot;left:437.1166666666666px;top:61.609399999999866px;16.6px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:442.517px;top:61.6094px;16.6px;sans-serif;transform:scaleX(0.909747);&quot;&gt;24&lt;/span&gt;&lt;span style=&quot;left:459.3166666666666px;top:61.609399999999866px;16.6px;sans-serif;&quot;&gt;7&lt;/span&gt;&lt;span style=&quot;left:82.64px;top:1052.01px;18.4px;sans-serif;transform:scaleX(0.899023);&quot;&gt;238&lt;/span&gt;&lt;span style=&quot;left:82.64px;top:142.039px;18.4px;sans-serif;transform:scaleX(0.929441);&quot;&gt;flow of subterranean waters: the depth of the water, the refill.&lt;/span&gt;&lt;span style=&quot;left:546.717px;top:142.039px;18.4px;sans-serif;transform:scaleX(0.88392);&quot;&gt;These factors are &lt;/span&gt;&lt;span style=&quot;left:82.64px;top:163.039px;18.4px;sans-serif;transform:scaleX(0.908482);&quot;&gt;represented by weights and quotations which depend respectively on their &lt;/span&gt;&lt;span style=&quot;left:82.64px;top:184.239px;18.4px;sans-serif;transform:scaleX(0.925057);&quot;&gt;relative importance and on local hydrogeolo&lt;/span&gt;&lt;span style=&quot;left:412.317px;top:184.239px;18.4px;sans-serif;transform:scaleX(0.932673);&quot;&gt;gical conditions.&lt;/span&gt;&lt;span style=&quot;left:539.717px;top:184.239px;18.4px;sans-serif;transform:scaleX(0.937613);&quot;&gt;The overall of the &lt;/span&gt;&lt;span style=&quot;left:82.64px;top:205.239px;18.4px;sans-serif;transform:scaleX(0.848433);&quot;&gt;weights and the quotations of the diverse parameters &lt;/span&gt;&lt;span style=&quot;left:486.31666666666666px;top:205.23893333333322px;18.4px;sans-serif;&quot;&gt;a&lt;/span&gt;&lt;span style=&quot;left:494.517px;top:205.239px;18.4px;sans-serif;transform:scaleX(0.853118);&quot;&gt;nd in a numerical value &lt;/span&gt;&lt;span style=&quot;left:82.64px;top:226.239px;18.4px;sans-serif;transform:scaleX(0.918584);&quot;&gt;which is the indication Drastic. The cartography of the indication of &lt;/span&gt;&lt;span style=&quot;left:82.64px;top:247.439px;18.4px;sans-serif;transform:scaleX(0.90494);&quot;&gt;vulnerability bases on the overlapping of 7 indexed cards. &lt;/span&gt;</style></abstract><issue><style face="normal" font="default" size="100%">n°26</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Djenba Samir</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Les instabilités de terrain le long de la route nationale N&amp;deg;9 Sétif-Bejaia N.E Algérien</style></title><secondary-title><style face="normal" font="default" size="100%">2 ème séminaire national sur les géorisques Jijel, 17 et 18 Novembre 2015</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2015</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Drias Tarek</style></author><author><style face="normal" font="default" size="100%">Toubal Ahmed Chérif</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Cartographie de la vulnérabilité de l&amp;rsquo;aquifère alluvionnaire de Tébessa-Morsott. Est Algérien, ISSN 1112-3680</style></title><secondary-title><style face="normal" font="default" size="100%">LARHYSS Journal</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2015</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://archives.univ-biskra.dz/bitstream/123456789/2888/1/4.Seghir_Karima.pdf</style></url></web-urls></urls><pages><style face="normal" font="default" size="100%">pp.35-48</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;span style=&quot;left:82.6px;top:497px;18.4px;serif;transform:scaleX(1.01655);&quot;&gt;Comme dans tou&lt;/span&gt;&lt;span style=&quot;left:209.2px;top:497px;18.4px;serif;transform:scaleX(1.0185);&quot;&gt;tes les régions de l’Afrique du Nord, notamment du Maghreb,&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:518px;18.4px;serif;transform:scaleX(1.00748);&quot;&gt;la région du grand bassin Méllègue a connu au cours des vingt dernières années&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:539.2px;18.4px;serif;transform:scaleX(1.00535);&quot;&gt;une sécheresse très intense et persistante. Cette sécheresse&lt;/span&gt;&lt;span style=&quot;left:518.4px;top:539.2px;18.4px;serif;transform:scaleX(1.01531);&quot;&gt;a été&lt;/span&gt;&lt;span style=&quot;left:553.2px;top:539.2px;18.4px;serif;transform:scaleX(1.00445);&quot;&gt; caractérisée par&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:560.2px;18.4px;serif;transform:scaleX(0.973116);&quot;&gt;un défi&lt;/span&gt;&lt;span style=&quot;left:137.4px;top:560.2px;18.4px;serif;transform:scaleX(0.982605);&quot;&gt;cit pluviométrique considé&lt;/span&gt;&lt;span style=&quot;left:339.4px;top:560.2px;18.4px;serif;transform:scaleX(0.970229);&quot;&gt;rable et&lt;/span&gt;&lt;span style=&quot;left:397px;top:560.2px;18.4px;serif;transform:scaleX(0.957922);&quot;&gt; a eu un impact très négatif sur les&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:581.2px;18.4px;serif;transform:scaleX(1.00973);&quot;&gt;régimes d’écoulement des oueds et des sources et sur l’alimentation des nappes&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:602.4px;18.4px;serif;transform:scaleX(0.971019);&quot;&gt;aquifères. Ce déficit hydro pluviométrique s’est répercuté sur l’ensemble des&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:623.4px;18.4px;serif;transform:scaleX(1.00328);&quot;&gt;activités socio&lt;/span&gt;&lt;span style=&quot;left:192.4px;top:623.4px;18.4px;serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:198.2px;top:623.4px;18.4px;serif;transform:scaleX(1.00696);&quot;&gt;économiques de cette région surtout su&lt;/span&gt;&lt;span style=&quot;left:510.2px;top:623.4px;18.4px;serif;transform:scaleX(1.00327);&quot;&gt;r son développement&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:644.6px;18.4px;serif;transform:scaleX(1.03248);&quot;&gt;agricole. Par ailleurs ce phénomène a eu ainsi un impact écologique en&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:665.6px;18.4px;serif;transform:scaleX(0.988863);&quot;&gt;dégradant, en générale, l’environnement&lt;/span&gt;&lt;span style=&quot;left:417px;top:665.6px;18.4px;serif;transform:scaleX(0.985136);&quot;&gt;et en favorisant notamment, la&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:686.6px;18.4px;serif;transform:scaleX(1.00189);&quot;&gt;pollution des eaux et le dépérissement du milieu naturel.&lt;/span&gt;&lt;span style=&quot;left:536px;top:686.6px;18.4px;serif;transform:scaleX(1.00544);&quot;&gt; Pour cela, i&lt;/span&gt;&lt;span style=&quot;left:638.4px;top:686.6px;18.4px;serif;transform:scaleX(1.00401);&quot;&gt;l est&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:707.8px;18.4px;serif;transform:scaleX(1.00182);&quot;&gt;important de mettr&lt;/span&gt;&lt;span style=&quot;left:219.8px;top:707.8px;18.4px;serif;transform:scaleX(1.00323);&quot;&gt;e en place une politique qui permettrait&lt;/span&gt;&lt;span style=&quot;left:514.2px;top:707.8px;18.4px;serif;transform:scaleX(0.998954);&quot;&gt;d’une part&lt;/span&gt;&lt;span style=&quot;left:594.2px;top:707.8px;18.4px;serif;transform:scaleX(0.991838);&quot;&gt;d’accroître&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:728.8px;18.4px;serif;transform:scaleX(0.997644);&quot;&gt;nos ressources en eau&lt;/span&gt;&lt;span style=&quot;left:245.6px;top:728.8px;18.4px;serif;transform:scaleX(1.00153);&quot;&gt;et&lt;/span&gt;&lt;span style=&quot;left:259px;top:728.8px;18.4px;serif;transform:scaleX(0.99446);&quot;&gt; de les&lt;/span&gt;&lt;span style=&quot;left:305.8px;top:728.8px;18.4px;serif;transform:scaleX(0.994057);&quot;&gt; protéger&lt;/span&gt;&lt;span style=&quot;left:371.4px;top:728.8px;18.4px;serif;transform:scaleX(0.994171);&quot;&gt; d’autre part&lt;/span&gt;&lt;span style=&quot;left:461px;top:728.8px;18.4px;serif;&quot;&gt;.&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:750px;18.4px;serif;transform:scaleX(0.999108);&quot;&gt;Dans le but de localiser les zones vulnérables à la pollution et leurs origine&lt;/span&gt;&lt;span style=&quot;left:632.8px;top:750px;18.4px;serif;&quot;&gt;s&lt;/span&gt;&lt;span style=&quot;left:640px;top:750px;18.4px;serif;transform:scaleX(0.988947);&quot;&gt;, des&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:771px;18.4px;serif;transform:scaleX(0.996337);&quot;&gt;campagnes d’échantillonnage d’eaux et des&lt;/span&gt;&lt;span style=&quot;left:429px;top:771px;18.4px;serif;transform:scaleX(0.993638);&quot;&gt;mesures pi&lt;/span&gt;&lt;span style=&quot;left:512.4px;top:771px;18.4px;serif;transform:scaleX(0.996248);&quot;&gt;ézométriques ont été&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:792px;18.4px;serif;transform:scaleX(0.986892);&quot;&gt;réalisées pendant les périodes des Hautes et Basses Eaux des années 2005,&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:813.2px;18.4px;serif;transform:scaleX(1.01842);&quot;&gt;2006. L’indice de contamination calculé nous a permis de dresser des cartes de&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:834.2px;18.4px;serif;transform:scaleX(1.01208);&quot;&gt;vulnérabilité sur lesquelles on a distingué trois zones à degré de contamination&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:855.4px;18.4px;serif;transform:scaleX(0.998946);&quot;&gt;croissant.&lt;/span&gt;</style></abstract><issue><style face="normal" font="default" size="100%">N°22</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Djenba Samir</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderrahmane</style></author><author><style face="normal" font="default" size="100%">BENCER</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Approche Hydrochimique De L&amp;rsquo;aquifere Superficiel De Ain Djacer. Est Algerien  SSN 1112-3680</style></title><secondary-title><style face="normal" font="default" size="100%">LARHYSS Journal </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2015</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://www.univ-tebessa.dz/fichiers/univ-batna/344-1161-1-PB.pdf</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Volume 12</style></volume><pages><style face="normal" font="default" size="100%">pp. 281-299</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">La région de Ain Djacer est le siège d’un aquifère superficiel qui se trouve dans les alluvions du Mio-Plio-Quaternaire. Cette nappe qui a pour substratum les argiles et les marnes gypseuses du Miocène, est entourée par les calcaires du Crétacé qui constituent une limite à potentiel imposé. Il s’agit d’un synclinal comblé par les sédiments du Mio-Plio-Quaternaire où tous les écoulements convergent vers le centre de la plaine. L’exploitation intensive des ressources en eaux souterraines de la région a largement influencé le fonctionnement hydrodynamique et hydrochimique de cette nappe. Ceci a induit une baisse du niveau statique et une minéralisation des eaux souterraines. Afin de mettre en évidence l’effet de cette situation sur la qualité des eaux souterraines, une étude hydrogéochimique a été menée. Cette étude a montré que le faciès est bicarbonaté calcique près des calcaires et chloruré sodique au centre de la plaine en liaison avec la lithologie. L’analyse thermodynamiques a montré que les principaux phénomènes géochimiques intervenant dans l’acquisition de la charge saline sont liés à l'interaction eau-roche (dissolution des minéraux carbonatés et évaporitiques), à l'échange cationique et à la concentration le long de l’écoulement</style></abstract><issue><style face="normal" font="default" size="100%">N°24</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Boudour Nassima</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude hydrogéologique de la plaine de Balezma. BAtna</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2015</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Ghori S</style></author><author><style face="normal" font="default" size="100%">Henka A </style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à l&amp;#39;étude hydrochimique des eaux de la nappe phréatique d&amp;#39;oued souf et détection d&amp;#39;éventuelles traces de pollution</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2015</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Hamidi. N</style></author><author><style face="normal" font="default" size="100%">Hamidi</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution a l&amp;rsquo;étude hydrogeologique de la nappe du complexe terminal  de la vallée nord  d&amp;rsquo;oued Righ.</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2015</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Djenba Samir</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author><author><style face="normal" font="default" size="100%">Belkhiri Chettah Badani</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Les instabilités de terrain le long de la route nationale N&amp;deg;9 Sétif-Bejaia N.E Algérien</style></title><secondary-title><style face="normal" font="default" size="100%">2 ème séminaire national sur les géorisques Jijel, 17 et 18 Novembre</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2015</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Drias Tarek</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Hydrochemical characterization of alluvial aquifer of Tebessa- Morsott - Eastern Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">2nd International Scientific Conference on Applied Sciences and Engineering. 16-17 February, Dubai, United Arab Emirates. </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2015</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">khadidja A</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author><author><style face="normal" font="default" size="100%">Drias Tarek</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Effect of the salinity on water for irrigation in the upper valley of Oued Rhumel - Eastern Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">International conference of Desalination for clean water and energy - Salinity gradient power session. 10 -14 May, Palermo, Italy. </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2015</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Drias Tarek</style></author><author><style face="normal" font="default" size="100%">khadidja A</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Effect of the salinity on water quality of the alluvial aquifer of Tebessa-Morsott - Eastern Algeria</style></title><secondary-title><style face="normal" font="default" size="100%"> International conference of Desalination for clean water and energy - Salinity gradient power session. 10 -14 May, Palermo, Italy </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2015</style></year></dates><pub-location><style face="normal" font="default" size="100%">Palermo, Italy </style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Malika</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Impact de la mobilisation des ressources hydriques dans les zones semi arides sur le développement durable, Cas du bassin de Timgad, Algérie, ISSN 2052-3408</style></title><secondary-title><style face="normal" font="default" size="100%">International Journal of Environment &amp; Water </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2015</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://ijew.ewdr.org/component/k2/item/372-impact-de-la-mobilisation-des-ressources-hydriques-dans-les-zones-semi-arides-sur-le-d%C3%A9veloppement-durable,-cas-du-bassin-de-timgad,-alg%C3%A9rie-nord-oriental.html</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Volume 4</style></volume><pages><style face="normal" font="default" size="100%">pp 118-123</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">La retenue collinaire est un ouvrage destiné généralement à améliorer une agriculture&lt;br&gt;existante par l’irrigation de petits périmètres et par conséquent améliorer les terres irriguées,&lt;br&gt;elle peut avoir d’autres objectifs.L’étude de faisabilité de tout terrain (région) reste&lt;br&gt;fondamentale avant d’entreprendre tout projet de recherche appliquée. Notre travail&lt;br&gt;proposé revêt une importance socio-économique pour la région de Timgad. Les résultats de ce travail constituent un apport scientifique utilisable aussi bien par les opérateurs socio-économiques que les décideurs pour tout plan d’aménagement. Dans la région étudiée, Les ressources hydriques sont en étroite relation avec les formations géologiques de la région, donc l’analyse de ces derniers est primordial. L’objectif principal de l’implantation de la retenue de Foum Toub est de contribuer à l’irrigation de la plaine de Foum Toub, de régulariser le débit de l’Oued Foum Toub et de minimiser le phénomène d’envasement du barrage de Koudiet Lemdaour. Pour cela, les sites retenus pour la construction de cet ouvrage sont représentés par un substratum imperméable. Les matériaux meubles, favorable pour servir de zones d’emprunt sont localisés dans les dépressions avoisinantes ainsi que les grès qui peuvent être utilisés comme matériaux de construction de la digue.</style></abstract><issue><style face="normal" font="default" size="100%">Numéro 2</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Sbih Mahtali</style></author><author><style face="normal" font="default" size="100%">Bensid Zoubeir</style></author><author><style face="normal" font="default" size="100%">Bounouara Zohra</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Ferrag Youcef</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Establishment theoretical of recommendation fertilization guide of vegetable crops in Algeria: concept and validation, ISSN 2349-0837 </style></title><secondary-title><style face="normal" font="default" size="100%">JOURNAL OF ADVANCES IN AGRICULTURE </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2015</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.researchgate.net/publication/284030914_Establishment_theoretical_of_recommendation_fertilization_guide_of_vegetable_crops_in_Algeria_concept_and_validation</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%"> Volume 5</style></volume><pages><style face="normal" font="default" size="100%">pp  606-620</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">The goal of fertilization is to meet the nutritional needs of plants by completing the supply of soil nutrients in an economically profitable and environmentally friendly. Achieving on-farm optimum economic crop yields of marketable quality with minimum adverse environmental impact requires close attention to fertilization guide. The recommendations seek to do this by ensuring that the available supply of plant nutrients in soil is judiciously supplemented by additions of nutrients in fertilizers. The objective is that crops must have an adequate supply of nutrients, and many crops show large and very profitable increases in yield from the correct use of fertilizers to supply nutrients. The main objective of this work is to establishing a reference guide of fertilization of vegetable crops and cereal in Algeria. To meet this objective, we have processes in two steps: 1) Establishment of theoretical fertilizer recommendation from international guide of crop fertilization; 2) Validation of these developed theoretical fertilizer recommendation by trials in the fields. Sixteen fertilization guides of vegetable crops from the Canadian provinces (5 guides), USA (10 guides) and countries of northern Europe England (1 guide). Generally, the rating of these recommendation is ranging from poor soil to soil exceedingly rich; however, the numbers of fertility classes are very different. Indeed, Quebec Ontario, Minnesota, Wisconsin New England, Maryland and Kentucky and Florida guides are subdivided into 5 fertility classes, ranging from poor soil to soil exceedingly rich. The recommendation of New Brunswick and Manitoba contain six classes. The recommendation of Michigan, Nova Scotia and England contain 10 and 7 fertility classes respectively. The recommendation fertilizer of New York and New Jersey have 3classes. Unlike the systems of fertilization recommendation mentioned above, the recommendation fertilizer of Pennsylvania is based on continuous models of P, K and contains 34 classes for P and 22 classes K. Then we standardized the P soil analysis with conversion equations (Olsen method) and units of measurement (kg/ha, mg/kgâ€¦).Following this procedure we transformed discontinued systems of fertility classes in to continuous models to facilitate comparison between the different fertilization recommendation models in one hand, in other hand to obtain critical value (CV).Finally, we used statistics of the conditional expectation in order to generate the theoretical recommendation fertilization guide of fertilization with 7 fertility classes (VL, L, M, MH, OP, H and VH). The next step was calibrating soil tests against yield responses to applied nutrient in field experiments. A database (not published data) from agriculture and agri-food Canada, were used. Production of pumpkin responded positively and significantly to P or K soil fertility levels, increases being observed with P more often than with K. According to the Cate-Nelson methods, the critical value of Olsen-P in the top 20 cm of soil was about 25 mg/kg: at values of greater than or equal to 25 mg/kg, crops achieved about 80% of their maximal yield in the absence of fertilizer application. The CV of K in soil for this crop was about 140 mg/kg. The CV found was very close to this generated by the theoretical method for recommendation of fertilization guide. Finally, we used the procedure of Cope and Rouse in both sides of the CV in order to make subdivisions of different groups of soil fertility. One calibrates the soil-test value against yield response to tile nutrient to predict fertilizer requirement.</style></abstract><issue><style face="normal" font="default" size="100%">Numéro  1</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Marmi Ramdane</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Le bassin néogène de Timgad : Paléocourants et sédimentation (Algérie Nord-Orientale)</style></title><secondary-title><style face="normal" font="default" size="100%">3émé colloque international sur la Géologie du Sahara  du 09 au 10 Décembre 2015, Université Kasdi Merbah OUARGLA</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2015</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Marmi Ramdane</style></author><author><style face="normal" font="default" size="100%">Ayhamena Ali</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">La mobilisation des ressources hydriques dans le bassin de Timgad (Aurès, Algérie NE)</style></title><secondary-title><style face="normal" font="default" size="100%">3émé colloque international sur la Géologie du Sahara  du 09 au 10 Décembre 2015, Université Kasdi Merbah OUARGLA</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2015</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Brahmia Ali</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude des caractéristiques hydrochimiques des eaux des sources de la partie nord du synclinal de Ghassira dans le massif des Aurès dans l&amp;rsquo;atlas saharien. Algérie.</style></title><secondary-title><style face="normal" font="default" size="100%">3eme colloque international sur la géologie du Sahara Algérien: Ressources minérales, en hydrocarbures et en eaux, Ouargla, Alger</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2015</style></year></dates><pub-location><style face="normal" font="default" size="100%">Ouargla, Alger</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Lebchek. S</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Approche hydrogéologique du bassin néogène de Timgad (nord-est algérien), 9-10 décembre 2015</style></title><secondary-title><style face="normal" font="default" size="100%">3ème Colloque International sur la Géologie du Sahara, Thème III Eau &amp; Environnement, Ouargla</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2015</style></year></dates><pub-location><style face="normal" font="default" size="100%">Ouargla</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Azizi Yacine</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">Boucenna Fatih</style></author><author><style face="normal" font="default" size="100%">Cheref Nouar</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Aspects quantitatifs et qualitatifs de la source de Chapuis (Tahabort) : impact sur l&amp;rsquo;aspect touristique de la région de Tamanrasset, Ouargla, 9-10 décembre 2015.</style></title><secondary-title><style face="normal" font="default" size="100%">3ème Colloque International sur la Géologie du Sahara, Thème III Eau &amp; Environnement</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2015</style></year></dates><volume><style face="normal" font="default" size="100%">Volume 03</style></volume><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Djenba S</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Approche hydrochimique de l&amp;rsquo;aquifère superficiel de ain djacer. Est algérien, Décembre</style></title><secondary-title><style face="normal" font="default" size="100%">Larhyss Journal </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2015</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://larhyss.net/ojs/index.php/larhyss/article/view/344</style></url></web-urls></urls><pages><style face="normal" font="default" size="100%"> pp 281-299</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;div&gt;
	&lt;p&gt;
		Ain Djacer Area is the seat of an aquifer which is located in the alluvial deposits of Mio-Plio-Quaternary. This groundwater has to bedrock clays and gypsum marl Miocene, is surrounded by Cretaceous limestones which are limited to a fixed potential. It is a synclinal filled by sediments Mio-Plio-Quaternary where all flows converge toward the center of the plain. The intensive exploitation of groundwater resources in the region has greatly influenced the hydrodynamic and hydrochemical functioning of the shallow aquifer. This caused a decrease in the static level and mineralization of groundwater. To demonstrate the effect of this situation on the quality of groundwater, a hydrogeochemical study was conducted. This study showed that the calcium bicarbonate facies is near limestone and sodium chloride concentration in the center of the plain in liaison with the lithology. The thermodynamic analysis showed that the main geochemical processes involved in the acquisition of saline load are related to water-rock interaction (dissolution of carbonate and evaporate minerals), the cation exchange and concentrating along flow.&amp;nbsp;
	&lt;/p&gt;
&lt;/div&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">n°24</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Drias Tarek</style></author><author><style face="normal" font="default" size="100%">Toubal Ahmed Chérif</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Cartographie de la vulnérabilité de l&amp;rsquo;aquifère alluvionnaire de Tébessa-Morsott. Est Algérien. ISSN 1112- 3680, June 2015</style></title><secondary-title><style face="normal" font="default" size="100%">Larhyss journal </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2015</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://larhyss.net/ojs/index.php/larhyss/article/view/275</style></url></web-urls></urls><pages><style face="normal" font="default" size="100%">pp 35-48</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;div style=&quot;left:82.6px;top:552.2px;18.4px;serif;transform:scaleX(0.998792);&quot;&gt;
	&lt;div&gt;
		&lt;p&gt;
			Une nouvelle méthodologie est proposée pour la caractérisation de la vulnérabilité à la pollution des nappes d’eau souterraine libres. Cette méthodologie constitue une amélioration de la méthode DRASTIC, universellement utilisée. La vulnérabilité à la pollution est basée uniquement sur les paramètres relatifs à la recharge, au sol (pente et nature) et à la zone non saturée (faciès et épaisseur) de l'aquifère, tandis que la méthodologie proposé est&amp;nbsp; basée uniquement sur les paramètres propres à la zone saturée.
		&lt;/p&gt;

		&lt;p&gt;
			Cette méthodologie a été appliquée au bassin de l’oued Ksob situé à l’extrême Est Algérien renfermant une nappe fortement sollicité, qui s’étend sur environ 320 km² d’extension.
		&lt;/p&gt;

		&lt;p&gt;
			Les résultats ont montré que cette nappe est caractérisée par une vulnérabilité globalement moyenne à faible. Les champs captant d’eau potable (produisant environ 400 l/s) sont par contre situés dans des secteurs de moyenne à forte vulnérabilité à la pollution, leur protection par des périmètres de protection rapprochée et éloignée est recommandée dans les plus brefs délais.
		&lt;/p&gt;
	&lt;/div&gt;
&lt;/div&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">n°22</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author><author><style face="normal" font="default" size="100%">Hamel Ahmed</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Analyse statistique et géochimique de la Dynamique des paramètres physico-chimiques des Eaux souterraines du synclinal de ghassira Algérie orientale. ISSN 1112-3680, June 2015</style></title><secondary-title><style face="normal" font="default" size="100%">Larhyss Journal</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2015</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://larhyss.net/ojs/index.php/larhyss/article/view/282</style></url></web-urls></urls><pages><style face="normal" font="default" size="100%">pp 123-137</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">This paper is about groundwater’s quality in Ghassira which is located in El-Abiod valley in eastern Algeria. The water is used for human consumption and irrigation. The different layers belong to several types of rocks (limestone and evaporate ...). To study the behaviour&amp;nbsp;&amp;nbsp; of dissolved salts in this water, we have used geology of the aquifers and statistics. This combination gives us information about minerals those are responsible of water’s quality.&amp;nbsp; 80% of analyzed samples are influenced by evaporate rocks (gypsum, halite…) and 20% by limestone. Many processes have generated these two classes and are relating, especially, with the rocks of aquifers.</style></abstract><issue><style face="normal" font="default" size="100%">n°22</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Malika</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Impact de la mobilisation des ressources hydriques dans les zones semi arides sur le développement durable, Cas du bassin de Timgad, Algérie. ISSN 2052-3408</style></title><secondary-title><style face="normal" font="default" size="100%">International Journal of Environment &amp; Water</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2015</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.google.com/url?sa=t&amp;rct=j&amp;q=&amp;esrc=s&amp;source=web&amp;cd=4&amp;cad=rja&amp;uact=8&amp;ved=2ahUKEwjimLHa0cLgAhWGDewKHRXdAZQQFjADegQIBxAC&amp;url=http%3A%2F%2Farmspark.msem.univ-montp2.fr%2Fmedfriend%2FHammamet2015%2F8-ManEnvironment%2FATHAMENA_article.doc&amp;usg=AOvVaw1</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Vol 4</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;i&gt;&lt;span style=&quot;New&quot; lang=&quot;FR&quot;&gt;La retenue collinaire est un ouvrage destiné généralement à améliorer une agriculture existante par l’irrigation de petits périmètres et par conséquent améliorer les terres irriguées, elle peut avoir d’autres objectifs. &lt;/span&gt;&lt;span style=&quot;NewNewRoman&amp;quot;;mso-ansi-language:FR;mso-fareast-language:FR;mso-bidi-language:
AR-SA&quot; lang=&quot;FR&quot;&gt;L’étude de faisabilité de tout terrain (région) reste fondamentale avant d’entreprendre tout projet de recherche appliquée. Notre travail proposé revêt une importance socio-économique pour la région de Timgad. Les résultats de ce travail constituent un apport scientifique utilisable aussi bien par les opérateurs socio-économiques que les décideurs pour tout plan d’aménagement. Dans la région étudiée, Les ressources hydriques sont en étroite relation avec les formations géologiques de la région, donc l’analyse de ces derniers est primordial. L’objectif principal de l’implantation de la retenue de Foum Toub est de contribuer à l’irrigation de la plaine de Foum Toub, de régulariser le débit de l’Oued Foum Toub et de minimiser le phénomène d’envasement du barrage de Koudiet Lemdaour. Pour cela, les sites retenus pour la construction de cet ouvrage sont représentés par un substratum imperméable. Les matériaux meubles, favorable pour servir de zones d’emprunt sont localisés dans les dépressions avoisinantes ainsi que les grès qui peuvent être utilisés comme matériaux de construction de la digue. &lt;/span&gt;&lt;/i&gt;</style></abstract><issue><style face="normal" font="default" size="100%">Issue 2</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Evaluation du risque de conflit autour des eaux transfrontalières du système aquifère du Sahara Septentrional (SASS)., ISSN 1112-3680, June 2015,</style></title><secondary-title><style face="normal" font="default" size="100%"> Larhyss Journal</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2015</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://lab.univ-biskra.dz/Larhyss/images/pdf/JOURNAL%C2%B022/6.Menani.Gire.pdf </style></url></web-urls></urls><pages><style face="normal" font="default" size="100%">pp. 59-69</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;span style=&quot;left:82.6px;top:523.8px;18.4px;serif;transform:scaleX(0.982485);&quot;&gt;Le SASS co&lt;/span&gt;&lt;span style=&quot;left:180px;top:523.8px;18.4px;serif;transform:scaleX(0.982398);&quot;&gt;uvre une super&lt;/span&gt;&lt;span style=&quot;left:295.6px;top:523.8px;18.4px;serif;transform:scaleX(0.985698);&quot;&gt;ficie d’environ 1&lt;/span&gt;&lt;span style=&quot;left:430.4px;top:523.8px;18.4px;serif;transform:scaleX(1.00004);&quot;&gt;000&lt;/span&gt;&lt;span style=&quot;left:462.6px;top:523.8px;18.4px;serif;transform:scaleX(0.973613);&quot;&gt;000 km², il&lt;/span&gt;&lt;span style=&quot;left:558.4px;top:523.8px;18.4px;serif;transform:scaleX(0.983846);&quot;&gt;est partagé par&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:544.8px;18.4px;serif;transform:scaleX(1.01192);&quot;&gt;l’Algérie, la Libye et la Tunisie. Il est situé dans une zone hyper aride avec une&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:566px;18.4px;serif;transform:scaleX(1.02183);&quot;&gt;recharge actuelle minime mais un grand volume stocké, évalué entre 20&lt;/span&gt;&lt;span style=&quot;left:626.6px;top:566px;18.4px;serif;transform:scaleX(1.02232);&quot;&gt;000 et&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:587px;18.4px;serif;transform:scaleX(1.00004);&quot;&gt;31&lt;/span&gt;&lt;span style=&quot;left:105.6px;top:587px;18.4px;serif;transform:scaleX(0.99671);&quot;&gt;000 km&lt;/span&gt;&lt;span style=&quot;left:160.7999933333333px;top:585.3999983333332px;11.6px;serif;&quot;&gt;3&lt;/span&gt;&lt;span style=&quot;left:166.5999983333333px;top:586.9999616666665px;18.4px;serif;&quot;&gt;.&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:613.2px;18.4px;serif;transform:scaleX(1.00686);&quot;&gt;Depuis 1970&lt;/span&gt;&lt;span style=&quot;left:176.8px;top:613.2px;18.4px;serif;transform:scaleX(1.02681);&quot;&gt; à nos j&lt;/span&gt;&lt;span style=&quot;left:231.2px;top:613.2px;18.4px;serif;transform:scaleX(1.0013);&quot;&gt;ours&lt;/span&gt;&lt;span style=&quot;left:263px;top:613.2px;18.4px;serif;transform:scaleX(1.0106);&quot;&gt;, l’exploitation du SASS est passée de 0&lt;/span&gt;&lt;span style=&quot;left:560px;top:613.1999633333332px;18.4px;serif;&quot;&gt;,&lt;/span&gt;&lt;span style=&quot;left:564.6px;top:613.2px;18.4px;serif;transform:scaleX(1.01776);&quot;&gt;6 à&lt;/span&gt;&lt;span style=&quot;left:592px;top:613.2px;18.4px;serif;transform:scaleX(1.00933);&quot;&gt;plus de&lt;/span&gt;&lt;span style=&quot;left:650.1999916666666px;top:613.1999633333332px;18.4px;serif;&quot;&gt;2&lt;/span&gt;&lt;span style=&quot;left:659.3999733333333px;top:613.1999633333332px;18.4px;serif;&quot;&gt;,&lt;/span&gt;&lt;span style=&quot;left:663.9999899999999px;top:613.1999633333332px;18.4px;serif;&quot;&gt;5&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:634.2px;18.4px;serif;transform:scaleX(1.02406);&quot;&gt;milliards m3/an., d’où&lt;/span&gt;&lt;span style=&quot;left:271.2px;top:634.2px;18.4px;serif;transform:scaleX(1.00054);&quot;&gt;des&lt;/span&gt;&lt;span style=&quot;left:307.2px;top:634.2px;18.4px;serif;transform:scaleX(1.00313);&quot;&gt;risques&lt;/span&gt;&lt;span style=&quot;left:359.6px;top:634.2px;18.4px;serif;transform:scaleX(1.03313);&quot;&gt; majeurs&lt;/span&gt;&lt;span style=&quot;left:445.2px;top:634.2px;18.4px;serif;transform:scaleX(1.00021);&quot;&gt;de&lt;/span&gt;&lt;span style=&quot;left:473.8px;top:634.2px;18.4px;serif;transform:scaleX(1.02728);&quot;&gt;salinisation des eaux,&lt;/span&gt;&lt;span style=&quot;left:655.8px;top:634.2px;18.4px;serif;transform:scaleX(1.00021);&quot;&gt;de&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:655.2px;18.4px;serif;transform:scaleX(0.991529);&quot;&gt;réduction de l’artésianisme,&lt;/span&gt;&lt;span style=&quot;left:295.6px;top:655.2px;18.4px;serif;transform:scaleX(1.00021);&quot;&gt;de&lt;/span&gt;&lt;span style=&quot;left:318.8px;top:655.2px;18.4px;serif;transform:scaleX(1.01681);&quot;&gt;tarissement des exutoires naturels,&lt;/span&gt;&lt;span style=&quot;left:581.6px;top:655.2px;18.4px;serif;transform:scaleX(1.00021);&quot;&gt;de&lt;/span&gt;&lt;span style=&quot;left:604.8px;top:655.2px;18.4px;serif;transform:scaleX(1.02049);&quot;&gt;baisse de&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:676.4px;18.4px;serif;transform:scaleX(1.00114);&quot;&gt;la piézométrie,&lt;/span&gt;&lt;span style=&quot;left:215.4px;top:676.4px;18.4px;serif;transform:scaleX(0.999639);&quot;&gt;d’&lt;/span&gt;&lt;span style=&quot;left:230.8px;top:676.4px;18.4px;serif;transform:scaleX(1.0019);&quot;&gt;augmentation des rabatt&lt;/span&gt;&lt;span style=&quot;left:425.6px;top:676.4px;18.4px;serif;transform:scaleX(1.00018);&quot;&gt;ements ou&lt;/span&gt;&lt;span style=&quot;left:523.8px;top:676.4px;18.4px;serif;transform:scaleX(0.999639);&quot;&gt;d’&lt;/span&gt;&lt;span style=&quot;left:539.2px;top:676.4px;18.4px;serif;transform:scaleX(1.00413);&quot;&gt;interférences&lt;/span&gt;&lt;span style=&quot;left:648.6px;top:676.4px;18.4px;serif;transform:scaleX(1.00054);&quot;&gt;des&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:697.4px;18.4px;serif;transform:scaleX(0.99763);&quot;&gt;périmètres de captage&lt;/span&gt;&lt;span style=&quot;left:261px;top:697.4px;18.4px;serif;transform:scaleX(1.00279);&quot;&gt;entre pays...Ce qui menace à terme la durabilité du&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:718.6px;18.4px;serif;transform:scaleX(0.999093);&quot;&gt;développement socio&lt;/span&gt;&lt;span style=&quot;left:238.39998833333334px;top:718.5999983333332px;18.4px;serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:244.2px;top:718.6px;18.4px;serif;transform:scaleX(0.997723);&quot;&gt;économique engagé dans l’ensemble de la zone.&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:739.6px;18.4px;serif;transform:scaleX(0.983108);&quot;&gt;Pour parer au&lt;/span&gt;&lt;span style=&quot;left:197.4px;top:739.6px;18.4px;serif;transform:scaleX(0.995239);&quot;&gt;mieux&lt;/span&gt;&lt;span style=&quot;left:243.2px;top:739.6px;18.4px;serif;transform:scaleX(0.971426);&quot;&gt; à ces risques&lt;/span&gt;&lt;span style=&quot;left:351.6px;top:739.6px;18.4px;serif;transform:scaleX(0.973048);&quot;&gt; et surtout pour mieux s’en&lt;/span&gt;&lt;span style=&quot;left:574.8px;top:739.6px;18.4px;serif;transform:scaleX(0.997402);&quot;&gt;prémunir&lt;/span&gt;&lt;span style=&quot;left:642.2px;top:739.6px;18.4px;serif;transform:scaleX(0.962323);&quot;&gt;, un&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:760.6px;18.4px;serif;transform:scaleX(1.01299);&quot;&gt;processus de c&lt;/span&gt;&lt;span style=&quot;left:190.4px;top:760.6px;18.4px;serif;transform:scaleX(1.01523);&quot;&gt;oopération a été initié&lt;/span&gt;&lt;span style=&quot;left:358.2px;top:760.6px;18.4px;serif;transform:scaleX(1.00798);&quot;&gt;depuis 1998&lt;/span&gt;&lt;span style=&quot;left:453.6px;top:760.6px;18.4px;serif;transform:scaleX(1.009);&quot;&gt;sous l’égide de l’observatoire&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:781.8px;18.4px;serif;transform:scaleX(1.01382);&quot;&gt;du Sa&lt;/span&gt;&lt;span style=&quot;left:124.6px;top:781.8px;18.4px;serif;transform:scaleX(1.00021);&quot;&gt;ha&lt;/span&gt;&lt;span style=&quot;left:142px;top:781.8px;18.4px;serif;transform:scaleX(1.00894);&quot;&gt;ra septentrional&lt;/span&gt;&lt;span style=&quot;left:262.4px;top:781.8px;18.4px;serif;transform:scaleX(0.998477);&quot;&gt;(OSS)&lt;/span&gt;&lt;span style=&quot;left:313.6px;top:781.8px;18.4px;serif;transform:scaleX(1.01272);&quot;&gt;en partenariat avec les institutions en charge d&lt;/span&gt;&lt;span style=&quot;left:657.8px;top:781.8px;18.4px;serif;transform:scaleX(1.00084);&quot;&gt;es&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:802.8px;18.4px;serif;transform:scaleX(1.00142);&quot;&gt;ressources en eau dans les 3 pays.&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:824px;18.4px;serif;transform:scaleX(1.00224);&quot;&gt;L’importance de cet immense réservoir pour le développement de la zone SA&lt;/span&gt;&lt;span style=&quot;left:652.8px;top:824px;18.4px;serif;transform:scaleX(0.998853);&quot;&gt;SS&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:845px;18.4px;serif;transform:scaleX(1.00028);&quot;&gt;et la nécessité de sa gestion durable et concertée a amené à une entente pour&lt;/span&gt;&lt;span style=&quot;left:643.2px;top:845px;18.4px;serif;transform:scaleX(0.994858);&quot;&gt; son&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:866px;18.4px;serif;transform:scaleX(1.02314);&quot;&gt;étude en&lt;/span&gt;&lt;span style=&quot;left:161.2px;top:866px;18.4px;serif;transform:scaleX(1.01391);&quot;&gt;plusieurs phases&lt;/span&gt;&lt;span style=&quot;left:292.4px;top:866px;18.4px;serif;transform:scaleX(1.01723);&quot;&gt;: la caractérisation hydrogéologique du système&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:887.2px;18.4px;serif;transform:scaleX(0.984658);&quot;&gt;aquifère et sa modélisation, l’identification des risques environnementaux et&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:908.2px;18.4px;serif;transform:scaleX(1.00303);&quot;&gt;l’inclusion de l’as&lt;/span&gt;&lt;span style=&quot;left:215.2px;top:908.2px;18.4px;serif;transform:scaleX(1.00322);&quot;&gt;pect socio&lt;/span&gt;&lt;span style=&quot;left:289.59999166666665px;top:908.1999633333332px;18.4px;serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:295.4px;top:908.2px;18.4px;serif;transform:scaleX(0.999605);&quot;&gt;économique dans des scénarios de développement&lt;/span&gt;&lt;span style=&quot;left:664.9999999999999px;top:908.1999633333332px;18.4px;serif;&quot;&gt;.&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:929.4px;18.4px;serif;transform:scaleX(0.957894);&quot;&gt;Les ressources en eau du SASS sont très faiblement renouvelables,&lt;/span&gt;&lt;span style=&quot;left:601.2px;top:929.4px;18.4px;serif;transform:scaleX(0.999301);&quot;&gt;environ&lt;/span&gt;&lt;span style=&quot;left:663.9999899999999px;top:929.3999649999998px;18.4px;serif;&quot;&gt;1&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:950.4px;18.4px;serif;transform:scaleX(1.01049);&quot;&gt;milliard de&lt;/span&gt;&lt;span style=&quot;left:169.2px;top:950.4px;18.4px;serif;transform:scaleX(1.0059);&quot;&gt;m3/an, vis&lt;/span&gt;&lt;span style=&quot;left:246.39999333333333px;top:950.3999749999999px;18.4px;serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:252.19998666666666px;top:950.3999749999999px;18.4px;serif;&quot;&gt;à&lt;/span&gt;&lt;span style=&quot;left:260.3999833333333px;top:950.3999749999999px;18.4px;serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:266.2px;top:950.4px;18.4px;serif;transform:scaleX(1.01203);&quot;&gt;vis des prélèvements actu&lt;/span&gt;&lt;span style=&quot;left:457.2px;top:950.4px;18.4px;serif;transform:scaleX(1.01724);&quot;&gt;els estimés à 2&lt;/span&gt;&lt;span style=&quot;left:566.00001px;top:950.3999749999999px;18.4px;serif;&quot;&gt;,&lt;/span&gt;&lt;span style=&quot;left:570.6px;top:950.4px;18.4px;serif;transform:scaleX(1.01242);&quot;&gt;5 milliards de&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:971.4px;18.4px;serif;transform:scaleX(1.02253);&quot;&gt;m3/an. La prise en compte de ce&lt;/span&gt;&lt;span style=&quot;left:326.8px;top:971.4px;18.4px;serif;transform:scaleX(1.01416);&quot;&gt;tte donné&lt;/span&gt;&lt;span style=&quot;left:395.7999933333333px;top:971.3999849999999px;18.4px;serif;&quot;&gt;e&lt;/span&gt;&lt;span style=&quot;left:409.4px;top:971.4px;18.4px;serif;transform:scaleX(1.01697);&quot;&gt;a été déterminante pour pousser les&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:992.6px;18.4px;serif;transform:scaleX(1.03258);&quot;&gt;scientifiques à établir la meilleure modélisation conceptuelle possible du&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:1013.6px;18.4px;serif;transform:scaleX(0.983934);&quot;&gt;système qui soit à même de permettre d’envisager différents scénarios&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:1034.8px;18.4px;serif;transform:scaleX(1.00317);&quot;&gt;d’exploitation&lt;/span&gt;&lt;span style=&quot;left:186.4px;top:1034.8px;18.4px;serif;transform:scaleX(1.03438);&quot;&gt; de la ressource tout en tenant compte des perspectives de&lt;/span&gt; &lt;span style=&quot;left:82.6px;top:140px;18.4px;serif;transform:scaleX(0.999093);&quot;&gt;développement socio&lt;/span&gt;&lt;span style=&quot;left:238.39998833333334px;top:139.99999166666666px;18.4px;serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:244.2px;top:140px;18.4px;serif;transform:scaleX(0.999337);&quot;&gt;économique de chacun des 3 pays.&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:161px;18.4px;serif;transform:scaleX(0.980248);&quot;&gt;Les données actuelles, quoique rassurantes, ne signifient pas l’inexistence&lt;/span&gt;&lt;span style=&quot;left:652.8px;top:161px;18.4px;serif;transform:scaleX(0.927295);&quot;&gt;, à&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:182.2px;18.4px;serif;transform:scaleX(1.02511);&quot;&gt;court ou moyen terme,&lt;/span&gt;&lt;span style=&quot;left:281.8px;top:182.2px;18.4px;serif;transform:scaleX(1.03613);&quot;&gt; d’un risque de conflit autour de ces eaux&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:203.2px;18.4px;serif;transform:scaleX(1.01449);&quot;&gt;transfrontalières. En effet, le problème mérite d’être analy&lt;/span&gt;&lt;span style=&quot;left:517px;top:203.2px;18.4px;serif;transform:scaleX(1.01386);&quot;&gt;sé à travers plusieurs&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:224.2px;18.4px;serif;transform:scaleX(1.00213);&quot;&gt;indicateurs qui ont un impact sur ce risque.&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:245.4px;18.4px;serif;transform:scaleX(0.960606);&quot;&gt;L’objectif de cette note est d’évaluer le risque de conflit autour des eaux du&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:266.4px;18.4px;serif;transform:scaleX(0.988725);&quot;&gt;SASS à travers un indice global exprimé numériquement sur la base de la&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:287.6px;18.4px;serif;transform:scaleX(0.929471);&quot;&gt;combinaison de poids et de cotes de p&lt;/span&gt;&lt;span style=&quot;left:371.6px;top:287.6px;18.4px;serif;transform:scaleX(0.976477);&quot;&gt;lusieurs indicat&lt;/span&gt;&lt;span style=&quot;left:485.6px;top:287.6px;18.4px;serif;transform:scaleX(0.952267);&quot;&gt;eurs qui ont, directement&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:308.6px;18.4px;serif;transform:scaleX(1.00032);&quot;&gt;ou indirectement&lt;/span&gt;&lt;span style=&quot;left:207px;top:308.6px;18.4px;serif;transform:scaleX(1.00207);&quot;&gt;, un impact sur le risque de conflit.&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:329.6px;18.4px;serif;transform:scaleX(1.01533);&quot;&gt;L’indice global de risque de conflit&lt;/span&gt;&lt;span style=&quot;left:344.6px;top:329.6px;18.4px;serif;transform:scaleX(1.00985);&quot;&gt; obtenu pour le cas du SASS semble refléter&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:350.8px;18.4px;serif;transform:scaleX(0.991263);&quot;&gt;correctement la situation qui&lt;/span&gt;&lt;span style=&quot;left:313.1999966666666px;top:350.79995999999994px;18.4px;serif;&quot;&gt;y&lt;/span&gt;&lt;span style=&quot;left:330.6px;top:350.8px;18.4px;serif;transform:scaleX(0.995445);&quot;&gt;prévaut actuellement.&lt;/span&gt;&lt;span style=&quot;left:501.4px;top:350.8px;18.4px;serif;transform:scaleX(0.982307);&quot;&gt;La comparaison de ce&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:371.8px;18.4px;serif;transform:scaleX(1.00274);&quot;&gt;résul&lt;/span&gt;&lt;span style=&quot;left:118.6px;top:371.8px;18.4px;serif;transform:scaleX(1.00842);&quot;&gt;tat avec ceux obtenus pour les eaux transfrontalières du bassin du Jourdain&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:393px;18.4px;serif;transform:scaleX(1.00929);&quot;&gt;(risque élevé) et ceux du système aquifère du Guarani (risque faible), confor&lt;/span&gt;&lt;span style=&quot;left:659.8px;top:393px;18.4px;serif;transform:scaleX(1.00569);&quot;&gt;te&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:414px;18.4px;serif;transform:scaleX(1.00108);&quot;&gt;l’échelle des valeurs adoptée dans&lt;/span&gt;&lt;span style=&quot;left:333.8px;top:414px;18.4px;serif;transform:scaleX(0.999531);&quot;&gt; cette méthode d’indexation numérique&lt;/span&gt;&lt;span style=&quot;left:622.4000033333333px;top:414.00003333333336px;18.4px;serif;&quot;&gt;.&lt;/span&gt;</style></abstract><issue><style face="normal" font="default" size="100%">n°22</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Azizi Yacine</style></author><author><style face="normal" font="default" size="100%">Boumezbeur Abderrahmane</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">Boucenna Fatih</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Sinkholes stability assessment in Cheria area, NE Algeria, ISSN 1112-3680</style></title><secondary-title><style face="normal" font="default" size="100%">Larhyss Journal</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2015</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://larhyss.net/ojs/index.php/larhyss/article/view/258</style></url></web-urls></urls><pages><style face="normal" font="default" size="100%">pp. 123-132</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;span style=&quot;left:82.6px;top:539.2px;18.4px;serif;transform:scaleX(1.01585);&quot;&gt;This research work deals with the problem of karst sinkhole collapse occurring&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:560.2px;18.4px;serif;transform:scaleX(0.941023);&quot;&gt;in the last few years in Cheria area. This newly revealed phenomenon is of a&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:581.2px;18.4px;serif;transform:scaleX(1.01725);&quot;&gt;major constrain in la&lt;/span&gt;&lt;span style=&quot;left:237.2px;top:581.2px;18.4px;serif;transform:scaleX(1.01331);&quot;&gt;nd use planning and urbanization, it has&lt;/span&gt;&lt;span style=&quot;left:534.2px;top:581.2px;18.4px;serif;transform:scaleX(1.00814);&quot;&gt; become necessary&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:602.4px;18.4px;serif;transform:scaleX(1.00508);&quot;&gt;to&lt;/span&gt;&lt;span style=&quot;left:107.6px;top:602.4px;18.4px;serif;transform:scaleX(1.02355);&quot;&gt;assess the stability of these underground feature&lt;/span&gt;&lt;span style=&quot;left:496.8px;top:602.4px;18.4px;serif;transform:scaleX(1.0218);&quot;&gt;s before any planning&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:623.4px;18.4px;serif;transform:scaleX(1.00343);&quot;&gt;operation&lt;/span&gt;&lt;span style=&quot;left:152.4px;top:623.4px;18.4px;serif;transform:scaleX(1.01949);&quot;&gt;. Laboratory testing and field work were undertaken in order to&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:644.6px;18.4px;serif;transform:scaleX(0.96736);&quot;&gt;determine both intact rock and rock mass properties&lt;/span&gt;&lt;span style=&quot;left:483.4px;top:644.6px;18.4px;serif;transform:scaleX(0.958896);&quot;&gt;. All the rock mechanics&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:665.6px;18.4px;serif;transform:scaleX(0.995777);&quot;&gt;testing and measurement were undertaken according to the ISRM&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:686.6px;18.4px;serif;transform:scaleX(0.99766);&quot;&gt;recommendations.&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:707.8px;18.4px;serif;transform:scaleX(1.02358);&quot;&gt;It has been found that under imposed loading, the stability of the karst cavities&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:728.8px;18.4px;serif;transform:scaleX(0.978507);&quot;&gt;depends on the geo&lt;/span&gt;&lt;span style=&quot;left:248.19999666666664px;top:728.7999899999999px;18.4px;serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:254px;top:728.8px;18.4px;serif;transform:scaleX(0.985295);&quot;&gt;mechanical parameters (Rock Masse Rating; RMR,&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:750px;18.4px;serif;transform:scaleX(0.998381);&quot;&gt;Geo&lt;/span&gt;&lt;span style=&quot;left:113.2px;top:750px;18.4px;serif;transform:scaleX(0.959461);&quot;&gt;logical Strength Index; GSI, and Young Modulus; E) of the host rock as&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:771px;18.4px;serif;transform:scaleX(1.01786);&quot;&gt;well as the depth and dimensions of the gallery. It increases with RMR, GSI, E&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:792px;18.4px;serif;transform:scaleX(1.0385);&quot;&gt;and depth and decreases as the cavity becomes wider. Furthermore, the&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:813.2px;18.4px;serif;transform:scaleX(1.01708);&quot;&gt;calculation results show that a rati&lt;/span&gt;&lt;span style=&quot;left:338.2px;top:813.2px;18.4px;serif;transform:scaleX(1.01535);&quot;&gt;o (roof thickness to gallery width) of 0.3 and&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:834.2px;18.4px;serif;transform:scaleX(1.00218);&quot;&gt;more indicate, a stable conditions.&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:855.4px;18.4px;serif;transform:scaleX(1.00384);&quot;&gt;The results obtained in this work allow identifying and assessing the stability of&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:876.4px;18.4px;serif;transform:scaleX(0.986769);&quot;&gt;underground karst cavities. The methodology followed in this paper can be&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:897.6px;18.4px;serif;transform:scaleX(1.02415);&quot;&gt;taken as a roa&lt;/span&gt;&lt;span style=&quot;left:185.8px;top:897.6px;18.4px;serif;transform:scaleX(1.01795);&quot;&gt;d map in the establishment of a hazard map related to the studied&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:918.6px;18.4px;serif;transform:scaleX(0.979298);&quot;&gt;phenomenon. This map will be a useful tool for the future urban extension&lt;/span&gt;&lt;span style=&quot;left:82.6px;top:939.6px;18.4px;serif;transform:scaleX(1.00132);&quot;&gt;planning in Cherea area.&lt;/span&gt;</style></abstract><issue><style face="normal" font="default" size="100%">n°21</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">Bilalite Halima</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Pollution des eaux souterraines par le flux azoté sous un climat semi-aride, cas de la plaine septentrionale de Zana-Chott Saboun, Est algérien.</style></title><secondary-title><style face="normal" font="default" size="100%">International Journal of Environment &amp; Water</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2015</style></year></dates><volume><style face="normal" font="default" size="100%">Vol 3</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><issue><style face="normal" font="default" size="100%">Issue 1</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Malika</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Impact de la mobilisation des ressources hydriques dans les zones semi- arides sur le développement durable, Cas du bassin de Timgad, Algérie nord oriental</style></title><secondary-title><style face="normal" font="default" size="100%">International Journal of Environment and Water</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2015</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://armspark.msem.univ-montp2.fr/medfriend/Hammamet2015/8-ManEnvironment/ATHAMENA_article.doc</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Vol.2</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align:justify&quot;&gt;
	&lt;span style=&quot;line-height:150%&quot;&gt;&lt;i&gt;&lt;span lang=&quot;FR&quot;&gt;&lt;span style=&quot;line-height:150%&quot;&gt;La retenue collinaire est un ouvrage destiné généralement à améliorer une agriculture existante par l’irrigation de petits périmètres et par conséquent améliorer les terres irriguées, elle peut avoir d’autres objectifs. &lt;/span&gt;&lt;/span&gt;&lt;/i&gt;&lt;i&gt;&lt;span lang=&quot;FR&quot;&gt;&lt;span style=&quot;line-height:150%&quot;&gt;L’étude de faisabilité de tout terrain (région) reste fondamentale avant d’entreprendre tout projet de recherche appliquée. Notre travail proposé revêt une importance socio-économique pour la région de Timgad. Les résultats de ce travail constituent un apport scientifique utilisable aussi bien par les opérateurs socio-économiques que les décideurs pour tout plan d’aménagement. Dans la région étudiée, Les ressources hydriques sont en étroite relation avec les formations géologiques de la région, donc l’analyse de ces derniers est primordial. L’objectif principal de l’implantation de la retenue de Foum Toub est de contribuer à l’irrigation de la plaine de Foum Toub, de régulariser le débit de l’Oued Foum Toub et de minimiser le phénomène d’envasement du barrage de Koudiet Lemdaour. Pour cela, les sites retenus pour la construction de cet ouvrage sont représentés par un substratum imperméable. Les matériaux meubles, favorable pour servir de zones d’emprunt sont localisés dans les dépressions avoisinantes ainsi que les grès qui peuvent être utilisés comme matériaux de construction de la digue. &lt;/span&gt;&lt;/span&gt;&lt;/i&gt;&lt;/span&gt;
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">Issue 4</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Boudoukha Abderrahmane</style></author><author><style face="normal" font="default" size="100%">Djenba Samir</style></author><author><style face="normal" font="default" size="100%">Jean-Sylvain Magagnosc</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation géologique et géotechnique des glissements de la ville de Bougaa. Est Algérien, ISSN 1112-3338</style></title><secondary-title><style face="normal" font="default" size="100%">courrier de savoir </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://pdfs.semanticscholar.org/6e67/266c856297aafe31a4861faea99507a79ea9.pdf</style></url></web-urls></urls><pages><style face="normal" font="default" size="100%">pp.63-67</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;span style=&quot;left:70.7998px;top:601.563px;16.8px;sans-serif;transform:scaleX(0.903164);&quot;&gt;La région de Bougaa est affectée par un glissement déplaçant un volume considérable de matériaux dé&lt;/span&gt;&lt;span style=&quot;left:763.6px;top:601.563px;16.8px;sans-serif;transform:scaleX(0.896679);&quot;&gt;tritiques formés par des &lt;/span&gt;&lt;span style=&quot;left:70.7998px;top:620.763px;16.8px;sans-serif;transform:scaleX(0.899913);&quot;&gt;colluvions, des éboulis à gros blocs et des éboulis de pente argilo&lt;/span&gt;&lt;span style=&quot;left:506.4px;top:620.763px;16.8px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:512px;top:620.763px;16.8px;sans-serif;transform:scaleX(0.933944);&quot;&gt;limoneux &lt;/span&gt;&lt;span style=&quot;left:580px;top:620.763px;16.8px;sans-serif;transform:scaleX(0.890049);&quot;&gt;rougeâtre reposant sur un substratum imperméable &lt;/span&gt;&lt;span style=&quot;left:70.7998px;top:639.963px;16.8px;sans-serif;transform:scaleX(0.893021);&quot;&gt;d’argilite schisteuse. Ce glissement est façonné dans des formations géologiques particulièrement se&lt;/span&gt;&lt;span style=&quot;left:780.4px;top:639.963px;16.8px;sans-serif;transform:scaleX(0.861645);&quot;&gt;nsibles à ce type de &lt;/span&gt;&lt;span style=&quot;left:70.7998px;top:659.163px;16.8px;sans-serif;transform:scaleX(0.922349);&quot;&gt;mouvement à cause de l'hétérogénéité de leurs faciès, de l'imperméabilité de certaines&lt;/span&gt;&lt;span style=&quot;left:663.6px;top:659.163px;16.8px;sans-serif;transform:scaleX(0.925478);&quot;&gt; couches et de l’effet de la tectonique &lt;/span&gt;&lt;span style=&quot;left:70.7998px;top:678.363px;16.8px;sans-serif;transform:scaleX(0.899453);&quot;&gt;cassante et de la karstification. Le but de cette étude est de caractériser ces glissements à l’aide&lt;/span&gt;&lt;span style=&quot;left:769.6px;top:678.363px;16.8px;sans-serif;transform:scaleX(0.903288);&quot;&gt; d’outils géologiques, &lt;/span&gt;&lt;span style=&quot;left:70.7998px;top:697.563px;16.8px;sans-serif;transform:scaleX(0.916535);&quot;&gt;géotechniques et géomorphologiques. Le rôle des eaux d’infiltration est primordial dans le dé&lt;/span&gt;&lt;span style=&quot;left:706.8px;top:697.563px;16.8px;sans-serif;transform:scaleX(0.902806);&quot;&gt;clenchement de ces glissements &lt;/span&gt;&lt;span style=&quot;left:70.7998px;top:716.763px;16.8px;sans-serif;transform:scaleX(0.964588);&quot;&gt;où la lithologi&lt;/span&gt;&lt;span style=&quot;left:169.6px;top:716.763px;16.8px;sans-serif;transform:scaleX(0.953006);&quot;&gt;e, la disposition structurale,&lt;/span&gt;&lt;span style=&quot;left:362.4px;top:716.763px;16.8px;sans-serif;transform:scaleX(0.970182);&quot;&gt;le climat&lt;/span&gt;&lt;span style=&quot;left:422.8px;top:716.763px;16.8px;sans-serif;transform:scaleX(0.932062);&quot;&gt; sont des facteurs favorables. &lt;/span&gt;&lt;span style=&quot;left:628.8px;top:716.763px;16.8px;sans-serif;transform:scaleX(0.943222);&quot;&gt;La présence de pentes &amp;gt; 20 %, de sources &lt;/span&gt;&lt;span style=&quot;left:70.7998px;top:735.963px;16.8px;sans-serif;transform:scaleX(0.906902);&quot;&gt;émergeant du réservoir karstique de Guergour, créant des zones humides qui permettent le déclenche&lt;/span&gt;&lt;span style=&quot;left:761.6px;top:735.963px;16.8px;sans-serif;transform:scaleX(0.885972);&quot;&gt;ment du mouvement du &lt;/span&gt;&lt;span style=&quot;left:70.7998px;top:755.163px;16.8px;sans-serif;transform:scaleX(0.898156);&quot;&gt;sol dans cette région.&lt;/span&gt;</style></abstract><issue><style face="normal" font="default" size="100%">N°18</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation géologique et apport de la géophysique pour la mobilisation des ressources hydriques dans le bassin de ain Djasser (Sud sétifien, Algerie NE)</style></title><secondary-title><style face="normal" font="default" size="100%">Colloque international Eau–Société–Climat’2017 (ESC-2017)  Hammamet, Tunis</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Sellam H</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation hydrochimique de l&amp;rsquo;aquifère alluvial de la plaine de Ain Djasser, Wilaya de Batna. Mémoire de Master, Université Hadj Lakhdar, Batna</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fartas FZ</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Suivi piézométrique et essais de pompage dans la plaine d&amp;rsquo;Ain Djasser, Wilaya de Batna. Mémoire de Master, Université Hadj Lakhdar, Batna - Encadreur principal.</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Mechri Ali</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Suivi piézométrique et hydrochimie dans la plaine de Ain Djasser, Wilaya de Batna. Mémoire de Master, Université Hadj Lakhdar, Batna .</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Tafrount A</style></author><author><style face="normal" font="default" size="100%">Benmenzer L </style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à l&amp;rsquo;étude géologique et géotechnique du barrage d&amp;rsquo;oued mellague (Tébessa), digue et matériaux de construction.</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Abid A</style></author><author><style face="normal" font="default" size="100%">Benaldjia H </style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à l&amp;rsquo;étude géologique et géotechnique du site du projet de la cimenterie BISKRIA, Biskra.</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Bensakhria D</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Fonctionnement de la station de traitement d&amp;rsquo;oued EL ATHMANIA (MILA) et la qualité physico-chimique et bactériologique des eaux en amont (brutes) et en avale (après traitement).</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Aya B </style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à L&amp;rsquo;étude de la qualité physico-chimique des eaux Destinées à l&amp;rsquo;AEP de la ville D&amp;rsquo;EL-OUED.</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Laabed C </style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à l&amp;rsquo;étude du fluor dans les eaux souterraines de la région de Hassi Messaoud.</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Drias Tarek</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Cartography of the vulnerability to pollution, Application to alluvial aquifer of Tebessa-Morsott - Eastern  Algeria </style></title><secondary-title><style face="normal" font="default" size="100%">International Multidisciplinary Academic Conference 11 to 13 May, Paris, France </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Malika</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Risque de pollution des eaux souterraines de la plaine de Zana, Est Algérien</style></title><secondary-title><style face="normal" font="default" size="100%">3émé colloque international Eau-Climat, REGARD CROISES NORD- SUD] Ressources en Eau &amp; Changement Climatique en Région Méditerranéenne 21, 22 &amp; 23 Octobre </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><pub-location><style face="normal" font="default" size="100%">Hammamet (Tunisie)</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Malika</style></author><author><style face="normal" font="default" size="100%">Marmi Ramdane</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">caractérisation géologique, hydrologique et hydrogéologique du bassin de timgad (Aurès, Algérie NE),  pour la mobilisation des ressources hydrique</style></title><secondary-title><style face="normal" font="default" size="100%">3émé colloque international Eau-Climat, REGARD CROISES NORD- SUD] Ressources en Eau &amp; Changement Climatique en Région Méditerranéenne 21, 22 &amp; 23 Octobre Hammamet (Tunisie)</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><pub-location><style face="normal" font="default" size="100%"> Hammamet (Tunisie)</style></pub-location><volume><style face="normal" font="default" size="100%">Vol. 5</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><issue><style face="normal" font="default" size="100%">No. 1</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Zouaoui Siham</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">Bouabid Abd Ennasser</style></author><author><style face="normal" font="default" size="100%">Naidji. A. N</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Conditions hydrogéologiques et hydrochimiques de l&amp;rsquo;oasis de Tolga (Nord-Est Algérien). Ressources en eau &amp;amp; changements climatiques en région méditerranéenne</style></title><secondary-title><style face="normal" font="default" size="100%"> 3ème colloque international Eau-Climat’2014 : REGARDS CROISES NORD-SUD. Hammamet (Tunisie), 21, 22 &amp; 23 Octobre</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><pub-location><style face="normal" font="default" size="100%">Hammamet, Tunisie</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude de la salinité des eaux souterraines dans les zones arides Cas de l&amp;rsquo;aquifère d&amp;rsquo;El-Outaya Région Nord ouest de Biskra  &amp;ndash; Algerie.</style></title><secondary-title><style face="normal" font="default" size="100%">The 5th International conference of Geomatics of Middle East and North Africa. The Euro-Arab Organization for Environment, Water and Desert Researches. Amman Jordan 23-27 mars</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><pub-location><style face="normal" font="default" size="100%">Amman Jordan</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Mansouri Zineb</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Evaluation of the groundwater vulnerability to pollution of the Ksar Belezma aquifer (Algeria Northeast). September 2014</style></title><secondary-title><style face="normal" font="default" size="100%">IAHS Conference, Marrakech, Morocco</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><pub-location><style face="normal" font="default" size="100%">Marrakech, Morocco</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Rihani A</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Hydrogeologic study of Bouzina watershed (Algeria Northeast). September 2014.</style></title><secondary-title><style face="normal" font="default" size="100%">IAHS Conference, Marrakech, Morocco</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><pub-location><style face="normal" font="default" size="100%">Marrakech, Morocco</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Malika</style></author><author><style face="normal" font="default" size="100%">Marmi Ramdane</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation géologique, hydrologique et hydrogéologique du bassin de timgad (Aurès, Algérie NE), pour la mobilisation des ressources hydrique</style></title><secondary-title><style face="normal" font="default" size="100%">3émé colloque international Eau-Climat, REGARD CROISES [NORD- SUD] Ressources en Eau &amp; Changement Climatique en Région Méditerranéenne Hammamet (Tunisie)</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><pub-location><style face="normal" font="default" size="100%"> Hammamet (Tunisie)</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Zouaoui Siham</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">Bouabid AN</style></author><author><style face="normal" font="default" size="100%">Nadji R</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Conditions hydrogéologiques et hydrochimiques de l&amp;rsquo;oasis de Tolga (Nord-Est Algérien). Ressources en eau &amp;amp; changements climatiques en région méditerranéenne. 21, 22 &amp;amp; 23 Octobre</style></title><secondary-title><style face="normal" font="default" size="100%">3ème colloque international Eau-Climat: REGARDS CROISES NORD-SUD. Hammamet (Tunisie)</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><pub-location><style face="normal" font="default" size="100%">Hammamet (Tunisie)</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Analysis of the risk of conflict around the transboundary water resources of the Northern Saharian Aquifer System (NSAS). 19-21 November</style></title><secondary-title><style face="normal" font="default" size="100%">GEOMATE international conference, Brisbane, Australia </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><pub-location><style face="normal" font="default" size="100%">Brisbane, Australia, </style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Les eaux transfrontalières du Système Aquifère du Sahara Septentrional (SASS) : Estimation du risque de conflit. 21-23 Octobre 2014.</style></title><secondary-title><style face="normal" font="default" size="100%">3rd International conference Eau-Climat 2014, Hammamet, Tunisie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><pub-location><style face="normal" font="default" size="100%">Hammamet, Tunisie</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Djenba Samir</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation géologique et géotechnique des glissements de la ville de Bougaa. Est algérien, Mars 2014</style></title><secondary-title><style face="normal" font="default" size="100%">Courrier du Savoir</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.google.dz/url?sa=t&amp;rct=j&amp;q=&amp;esrc=s&amp;source=web&amp;cd=1&amp;cad=rja&amp;uact=8&amp;ved=2ahUKEwi_xq7m78PgAhVGxYUKHd-NBXkQFjAAegQIABAC&amp;url=http%3A%2F%2Frevues.univ-biskra.dz%2Findex.php%2Fcds%2Farticle%2Fview%2F650%2F604&amp;usg=AOvVaw18Us5RIOfsC2lfNU6ndlpe</style></url></web-urls></urls><pages><style face="normal" font="default" size="100%">pp 63-67</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Bougaa region is affected by a shift moving a considerable amount of detritus formed by colluvial deposits, scree to boulders and scree slope reddish clay loam resting on a substratum of impermeable shale shale. This shift is shaped in geological formations particularly sensitive to this type of movement because of the heterogeneity of their facies, the impermeability of certain layers and the effect of tectonics and karstification. The purpose of this study is to characterize these shifts using tools geological, geotechnical and geomorphological features. The role of seepage is essential in triggering these shifts where lithology, structural arrangement, the climate is favorable factors. The presence of slopes&amp;gt; 20%, emerging sources of karst reservoir Guergour, creating wetlands that allow triggering of ground motion in this region.</style></abstract><issue><style face="normal" font="default" size="100%">N°18</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Malika</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Importance des ressources hydriques et leurs impacts sur le développement durable dans le bassin de Timgad (Algérie nord orientale), ISSN 2170-1318,Décembre 2014</style></title><secondary-title><style face="normal" font="default" size="100%">Journal of Arid And Environment (AJAE)</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://revues.univ-ouargla.dz/index.php/volume-4-numero-2-2014/2159-importance-des-ressources-hydriques-et-leurs-impacts-sur-le-developpement-durable-dans-le-bassin-de-timgad-algerie-nord-orientale-djaiz-fouad1-athamena-malika2-athamena-ali3-1-departemen</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">vol. 4</style></volume><pages><style face="normal" font="default" size="100%">pp 78-87</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;i&gt;&lt;span style=&quot;10pt;&quot;&gt;Located in the Aures mountains Foum Toub is characterized by an annual average rainfall of&amp;nbsp; 800mm. The hydrology subordinate to the terrain is the direct consequence of surface waters and of snow melting from the heights of Chelia Mountain. The aim of the implantation of the Foum Toub backwater is to minimize the siltation phenomenon at the upstream of the Koudiate El Mdaour dam, to regularize the Rebaa creek flow which runs from south to north and to contribute to the irrigation of the Foum Toub plain. This study puts the emphasis on the mobilization of surface water resources, a policy of the Ministry of Agriculture and Rural Development with a view to rationalize the use and planning of this vital factor, i.e. water. The site selected for the construction of this structure is characterized by a waterproof marly substratum, favourable for implanting the dike and the basin. The clay-silty-gravelly material furniture localized in the depressions as well as sandstones are used as areas for the construction materials of this structure. Stability is one of the most important parameters to take into account for the choice of the site, so as to avoid any problem linked to the withdrawal-swelling phenomena on the banks of creek. However, the sliding possibility, however weak it is, can be generated on the left bank of the creek within deposit and recent silt. The choice of the site for the implantation of this hydraulic structure remains subject to laboratory tests.&lt;/span&gt;&lt;/i&gt;</style></abstract><issue><style face="normal" font="default" size="100%">n° 2</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude de la salinité des eaux souterraines dans les zones arides Cas de l&amp;rsquo;aquifère d&amp;rsquo;El-Outaya Région Nord ouest de Biskra &amp;ndash; ALGERIE; ISSN 2052-3408,</style></title><secondary-title><style face="normal" font="default" size="100%">International Journal of Environment &amp; Water </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://ijew.ewdr.org/component/k2/item/261-case-of-aquifer-of-el-outaya-north-west-of-biskra-algeria.html</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Vol 3</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Le bassin d’El-Outaya se trouve dans la wilaya de BISKRA, une zone aride au sud algérien à environ 500 Km au sud de la capital Alger. Il constitue une ressource importante pour l'eau d'irrigation en plus d’un barrage à l’amont. La population de la plaine dépasse 11 000 habitants, leur activité principale est l'agriculture.&lt;br&gt;La plaine étudiée correspond à un bassin subsident orienté sensiblement E.NE – W.SW et situé entre deux anticlinaux. Il se trouve au nord de l’anticlinal du Dj.Bou Rhezel (Biskra) et au sud du dôme de Dj. El Melah. Il a fonctionné comme un bassin de sédimentation pendant tout le Néogène. Il est constitué à la base par un miocène laguno-marin, recouvert par du messinien (pontien) gréseux fluviatile, puis par des poudingues pliocènes. Les termes supérieurs, plus particulièrement pliocènes, sont fortement inclinés vers le centre du bassin où ils disparaissent sous une épaisseur considérable du Quaternaire.&lt;br&gt;Le dépouillement des analyses chimiques a aboutit à trois faciès chimiques: Le faciès chloruré sodique, le faciès sulfaté magnésien et le faciès sulfaté sodique.&lt;br&gt;Le suivi des variables chimiques dominant selon les axes des écoulements souterrains permet de suivre l’évolution des faciès dans aquifère ainsi que l’origine de chaque faciès.</style></abstract><issue><style face="normal" font="default" size="100%">Issue 1</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Boudjema Abderrezak</style></author><author><style face="normal" font="default" size="100%">Hacini Messaoud</style></author><author><style face="normal" font="default" size="100%">Guettaia Sabrine</style></author><author><style face="normal" font="default" size="100%">Zahrouna Abderrezak</style></author><author><style face="normal" font="default" size="100%">Baba Sy Lamine</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Modeling Groundwater Flow of the Mio-Pliocene Aquifer in the El-Outaya Plain, Biskra (Algeria) ISSN 2307-4531, (Print &amp;amp; Online).</style></title><secondary-title><style face="normal" font="default" size="100%">International Journal of Sciences: Basic and Applied Research (IJSBAR)</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.google.com/url?sa=t&amp;rct=j&amp;q=&amp;esrc=s&amp;source=web&amp;cd=1&amp;cad=rja&amp;uact=8&amp;ved=2ahUKEwjcn76xvsLgAhWB2qQKHcRnCwAQFjAAegQIBBAC&amp;url=http%3A%2F%2Fgssrr.org%2Findex.php%3Fjournal%3DJournalOfBasicAndApplied%26page%3Darticle%26op%3Ddownload%26path%255B%255D%</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Vol 17</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;
	El Outaya plain is located on the southern flank of the Aures Mountains, as part of the Saharan Atlas. It has an arid climate (less than 200 mm of rainfall / year). The Mio-Pliocene aquifer associated with this plain is an important resource for irrigation and drinking water.
&lt;/p&gt;

&lt;p&gt;
	Achieving the first hydrodynamic model of the Mio-Pliocene ground water in El Outaya plain, with different operating scenarios and using the Visual Mod-flow code, shall contribute to the development of an action plan for a rational management of water resources.&lt;br&gt;In addition, the model was calibrated to steady state conditions and then transient state conditions in order to prepare conductivity and porosity maps that characterize the spatial variability, in relation with the geological heterogeneity of the aquifer. Different operating scenarios indicated that the northern part of the plain is fairly vulnerable to feeding and exploitation conditions.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">No 2 </style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude de la salinité des eaux souterraines dans les zones arides Cas de l&amp;rsquo;aquifère d&amp;rsquo;El-Outaya Région Nord ouest de Biskra &amp;ndash; ALGERIE, 2014. ISSN 2052-3408.</style></title><secondary-title><style face="normal" font="default" size="100%"> International Journal of Environment &amp; Water</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><volume><style face="normal" font="default" size="100%">Vol 3</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><issue><style face="normal" font="default" size="100%">Issue 1</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Azizi Yacine</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">Hemila Med Laid</style></author><author><style face="normal" font="default" size="100%">Boumezbeur Abderrahmane</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Karst Sinkholes Stability Assessment in Cheria Area, NE Algeria. Geotechnical and Geological Engineering Review, April 2014</style></title><secondary-title><style face="normal" font="default" size="100%">Springer</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://www.springerprofessional.de/karst-sinkholes-stability-assessment-in-cheria-area-ne-algeria/5004782.html </style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Volume 32</style></volume><pages><style face="normal" font="default" size="100%">pp 363-374</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">This research work deals with the problem of karst sinkhole collapse occurring in the last few years in Cheria area (NE Algeria). This newly revealed phenomenon is of a major constrain in land use planning and urbanization, it has become necessary to locate and assess the stability of these underground features before any planning operation. Several exploration methods for the localization of underground cavities have been considered. Geological survey, discontinuity analysis, resistivity survey [ground penetrating radar has not been used as most of the Mio-Plio-Quaternary filling deposit covering Eocene limestone contains clay layers which limits the applicability of the method (Roth et al. in Eng Geol 65:225–232, &lt;cite&gt;&lt;a href=&quot;https://www.springerprofessional.de/karst-sinkholes-stability-assessment-in-cheria-area-ne-algeria/5468096?redirect=1#CR25&quot;&gt;2002&lt;/a&gt;&lt;/cite&gt;)] and borehole drilling were undertaken in order to locate underground cavities and assess their depth, geometry, dimensions, etc. Laboratory testing and field work were also undertaken in order to determine both intact rock and rock mass properties. All the rock mechanics testing and measurement were undertaken according to the ISRM recommendations. It has been found that under imposed loading, the stability of the karst cavities depends on the geo-mechanical parameters (RMR, Rock Mass Rating; GSI, Geological Strength Index; E, Young modulus) of the host rock as well as the depth and dimensions of the gallery. It increases with RMR, GSI, E and depth and decreases as the cavity becomes wider. Furthermore, the calculation results show that a ratio (roof thickness to gallery width) of 0.3 and more indicate, a stable conditions. The results obtained in this work allow identifying and assessing the stability of underground karst cavities. The methodology followed in this paper can be taken as a road map in the establishment of a hazard map related to the studied phenomenon. This map will be a useful tool for the future urban extension planning in Cheria area.</style></abstract><issue><style face="normal" font="default" size="100%">Issue 2</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Drias Tarek</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Cartography of the vulnerability to pollution, Application to alluvial aquifer of Tabessa-Morsott - Eastern Algeria.</style></title><secondary-title><style face="normal" font="default" size="100%">Review of strategic and international studies</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><volume><style face="normal" font="default" size="100%">Volume VI</style></volume><pages><style face="normal" font="default" size="100%"> pp 96-107.</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><issue><style face="normal" font="default" size="100%">Number 1</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Djenba Samir</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Geological and geotechnical characteristics of the soils in the region of Setif </style></title><secondary-title><style face="normal" font="default" size="100%">publication internationale European scientific journal</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Djenba Samir</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Geological and geotechnical characteristics of the soils in the region of Setif</style></title><secondary-title><style face="normal" font="default" size="100%"> 1 st annuel international interdiscplinary conference avril Azores Portugal</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Bentahar Fahima</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Lithostratigraphie des calcaires aptien du Dj Bouroumane (Algerie oriental nord)</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Malika</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Accident probablement responsable de la présence des sources thermales, Cas de la source thermale de Guergima, Batna Est Algérien</style></title><secondary-title><style face="normal" font="default" size="100%">The 5th Tunisian days of Applied Geology.JTGA. 2013. International Conference of Applied geology and Geomatics. ICNHG, 2013. Hammamet, Tunisia 17-20 May</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Malika</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">La contribution de la géophysique dans les études thermales, cas des sources des monts des Aures</style></title><secondary-title><style face="normal" font="default" size="100%">Colloque International sur les applications géophysiques de Sub surface – CIAGS- 26 27 Octobre 2013. Laboratoire de géologie et d’environnement/ FSTGAT/Uni. De Constantine 1</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Malika</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Géothermie des eaux souterraines cas de la source thermale de Guergima, Batna est-algérien </style></title><secondary-title><style face="normal" font="default" size="100%">Séminaire international sur  l’hydrogéologie et l’environnement SIHE 2013, Ouargla 5-7 Novembre </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Malika</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Importance de la mobilisation des ressources hydriques et l&amp;rsquo;impact sur le développement durable dans le bassin de Timgad Algérie nord orientale</style></title><secondary-title><style face="normal" font="default" size="100%">The 5th Tunisian days of Applied Geology.JTGA. 2013. International Conference of Applied geology and Geomatics. ICNHG, 2013. Hammamet, Tunisia 17-20 May</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Marmi Ramdane</style></author><author><style face="normal" font="default" size="100%">BOUMEZBEUR A</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Risque naturel liée au mouvements des terrains affaissables dans une zone urbaine &amp;ndash;Batna</style></title><secondary-title><style face="normal" font="default" size="100%">The 5th Tunisian days of Applied Geology.JTGA. 2013. International Conference of Applied geology and Geomatics. ICNHG, 2013. Hammamet, Tunisia 17-20 May</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Inal Ahmed</style></author><author><style face="normal" font="default" size="100%">Marmi Ramdane</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">L&amp;rsquo;apport de la géophysique à la géométrie des couches profondes et les aquifères potentiels du bassin de timgad (Atlas Saharien Algérien Oriental)</style></title><secondary-title><style face="normal" font="default" size="100%">2ème Colloque International sur La Gestion Intégrée des Ressources en Eau GIRE’2013 22-23 Octobre 2013/ / Dép. Sc. de la Terre et de l'Univers / Faculté des Sciences - Université Hadj Lakhdar - Batna</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">BOUMEZBEUR A</style></author><author><style face="normal" font="default" size="100%">Marmi Ramdane</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Les mouvements des sols,Géorisques et Urbanisation</style></title><secondary-title><style face="normal" font="default" size="100%">2ème Colloque International sur La Gestion Intégrée des Ressources en Eau GIRE’2013 22-23Octobre 2013/ / Dép. Sc. de la Terre et de l'Univers / Faculté des Sciences - Université Hadj Lakhdar – Batna</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Mohamedi A</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à l&amp;rsquo;étude hydrogéologique de la plaine de Tadjenent. Wilaya de Mila. Mémoire de Master, Université Hadj Lakhdar, Batna</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Mensouri. Z</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation hydrodynamique de l&amp;rsquo;aquifère alluvial de la plaine de Ain Djasser, Wilaya de Batna. Mémoire de Master, Université Hadj Lakhdar, Batna</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Maache T</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Qualité des eaux du barrage de Koudiet Medaouer et aptitude à l&amp;rsquo;irrigation des terres agricoles de la plaine de chemora. Mémoire de Master, Université Hadj Lakhdar</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Bilalite Halima</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation hydrochimique de l&amp;rsquo;aquifère alluvial de la plaine de Zana, Wilaya de Batna. Mémoire de Master, Université Hadj Lakhdar, Batna</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Labchek S</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation hydrodynamique de l&amp;rsquo;aquifère alluvial de la plaine de Zana, Wilaya de Batna. Mémoire de Master, Université Hadj Lakhdar, Batna</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Bouzzafa A</style></author><author><style face="normal" font="default" size="100%">Benyekken D </style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude de la stabilité de la digue du barrage Bouzina. Univ Batna</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Zkara Ibtissem</style></author><author><style face="normal" font="default" size="100%">Snina S</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à l&amp;rsquo;étude géologique et géotechnique du barrage Tabellout. Univ de Batna</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Selem R</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Fonctionnement de la station de traitement de Timgad (W) de Batna et étude de la qualité physic-chimique des eaux en amont et en aval. Univ de Batna.</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Zid.G</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Fonctionnement de la STEP d&amp;rsquo;oued Souf et l&amp;rsquo;étude de l&amp;rsquo;effluent en amont et en aval.</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Drias Tarek</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Cartographie de la vulnérabilité à la pollution de la nappe alluviale de Tébessa-Morsott (BV d&amp;rsquo;oued ksob), extrême Est Algérie</style></title><secondary-title><style face="normal" font="default" size="100%">2ème colloque international sur la gestion intégrée des ressources en eau. 22-23 Octobre 2013. Batna. Algérie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Marmi Ramdane</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Le Bassin néogène de Timgad et son aspect structural (atlas saharien algérien oriental)</style></title><secondary-title><style face="normal" font="default" size="100%">3eme colloque international. Les géosciences au service du DEVELOPPEMENT DURABLE. 20-21 NOVEMBRE, TEBESSA –ALGERIE</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><pub-location><style face="normal" font="default" size="100%">TEBESSA –ALGERIE</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Zouaoui Siham</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude hydrogéologique de l&amp;rsquo;&amp;rsquo;oasis de Tolga (Région de Biskra, NE Algérien). Modes d&amp;rsquo;exploitations des réserves et incidences de l&amp;rsquo;usage agricole</style></title><secondary-title><style face="normal" font="default" size="100%">2ème colloque international sur la gestion intégrée des ressources en Eau ; GIRE’2013. Batna (Algérie), 22 et 23 Octobre</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude des faciès chimiques des eaux souterraines de la plaine  d&amp;rsquo;El-Outaya  au sud algérien. Types et évolution dans l&amp;rsquo;espace aquifère</style></title><secondary-title><style face="normal" font="default" size="100%">The 5th Tunisian Days of Applied Geology -- Hammamet, Tunisie, May 17th - 19th</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude du phénomène d&amp;rsquo;eutrophisation dans les eaux du barrage de Koudiet Medouar, Timgad, Wilaya de Batna (Est &amp;ndash; Algérien)</style></title><secondary-title><style face="normal" font="default" size="100%">2ème Colloque International sur La Gestion Intégrée des Ressources en Eau GIRE’2013 22-23 Octobre / Dép. Sc. de la Terre et de l'Univers / Faculté des Sciences - Université Hadj Lakhdar - Batna.</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Inal Ahmed</style></author><author><style face="normal" font="default" size="100%">Marmi Ramdane</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">L&amp;rsquo;apport de la géophysique a la géométrie des couches profondes et les aquifères potentiels du bassin de timgad (Atlas Saharien Algérien Oriental)</style></title><secondary-title><style face="normal" font="default" size="100%">2ème Colloque International sur La Gestion Intégrée des Ressources en Eau GIRE’2013 22-23 Octobre / Dép. Sc. de la Terre et de l'Univers / Faculté des Sciences - Université Hadj Lakhdar - Batna</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Rihani A</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Aperçu sur les ressources en eau souterraines du bassin versant d&amp;rsquo;Oued Labiod (Massif des Aurès). Com</style></title><secondary-title><style face="normal" font="default" size="100%">Poster GIRE </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://gire-batna.netai.net/GIRE2013/gire2013.html </style></url></web-urls></urls><pub-location><style face="normal" font="default" size="100%">Batna</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Benagoune F</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Apport de la modélisation géologique 3D dans la compréhension du mode de fonctionnement des sources d&amp;#39;eau de la terminaison périclinale orientale du grand pli atlasique du Ravin Bleu (NE algérien). Cas de la source de Djerma. Com</style></title><secondary-title><style face="normal" font="default" size="100%">Poster GIRE, ID 913</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://gire-batna.netai.net/GIRE2013/Posters/ID%20913.pdf </style></url></web-urls></urls><pub-location><style face="normal" font="default" size="100%">Batna</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Zouaoui Siham</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude hydrogéologique de l&amp;#39;Oasis de Tolga (région de Biskra - NE algérien). Mode d&amp;#39;exploitation des réserves et incidences de l&amp;#39;usage agricole. Com</style></title><secondary-title><style face="normal" font="default" size="100%">Poster GIRE, ID 666</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://gire-batna.netai.net/GIRE2013/Posters/ID%20666.pdf </style></url></web-urls></urls><pub-location><style face="normal" font="default" size="100%">Batna</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Zouaoui Siham</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude hydrogéologique de l&amp;rsquo;&amp;rsquo;oasis de Tolga (Région de Biskra, NE Algérien). Modes d&amp;rsquo;exploitations des réserves et incidences de l&amp;rsquo;usage agricole. 22 et 23 Octobre 2013</style></title><secondary-title><style face="normal" font="default" size="100%">2ème colloque international sur la gestion intégrée des ressources en Eau, GIRE, Batna (Algérie)</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><pub-location><style face="normal" font="default" size="100%">Batna</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Inal Ahmed</style></author><author><style face="normal" font="default" size="100%">Marmi Ramdane</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">L&amp;rsquo;apport de la géophysique a la géométrie des couches profondes et les aquifères potentiels du bassin de timgad (Atlas Saharien Algérien Oriental). 22-23 Octobre 2013</style></title><secondary-title><style face="normal" font="default" size="100%">2ème Colloque International sur La Gestion Intégrée des Ressources en Eau GIRE,Dép. Sc.de la Terre et de l'Univers / Faculté des Sciences - Université Hadj Lakhdar - Batna</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><pub-location><style face="normal" font="default" size="100%">Batna</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">BOUMEZBEUR A</style></author><author><style face="normal" font="default" size="100%">Marmi Ramdane</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Les mouvements des sols, Géorisques et Urbanisation. 2ème Colloque International sur La Gestion Intégrée des Ressources en Eau, 22-23 Octobre 2013</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><publisher><style face="normal" font="default" size="100%">GIRE, Dép. Sc. de la Terre et de l'Univers / Faculté des Sciences - Université Hadj Lakhdar – Batna. </style></publisher><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">AZIZI Y</style></author><author><style face="normal" font="default" size="100%">BOUMEZBEUR A</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">Boucenna Fatih</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">KARST SINKHOLES STABILITY ASSESSMENT IN CHERIA AREA, NE ALGERIA. Com</style></title><secondary-title><style face="normal" font="default" size="100%">Orale GIRE 2013 ID 514, Batna</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://gire-batna.netai.net/GIRE2013/Orales/ID%20514.pdf </style></url></web-urls></urls><pub-location><style face="normal" font="default" size="100%"> Batna</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Evaluation du risque de conflit autour des eaux transfrontalières du système aquifère du Sahara septentrional (SASS).  Com</style></title><secondary-title><style face="normal" font="default" size="100%">Orale ID 921, GIRE, Batna</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://gire-batna.netai.net/GIRE2013/Orales/ID%20921.pdf </style></url></web-urls></urls><pub-location><style face="normal" font="default" size="100%">Batna</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">The artificial recharge of the aquifers by considering the groundwater vulnerability to pollution. Com. 22 et 23 Octobre 2013.</style></title><secondary-title><style face="normal" font="default" size="100%"> Orale ID 919, GIRE, Batna</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://gire-batna.netai.net/GIRE2013/Orales/ID%20919.pdf</style></url></web-urls></urls><pub-location><style face="normal" font="default" size="100%">Batna</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Assessment of the risk of conflict around the transboundary water resources of the Northern Saharan Aquifer System. Com. 22-23 may</style></title><secondary-title><style face="normal" font="default" size="100%">Orale IJAS conference,Toronto</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><pub-location><style face="normal" font="default" size="100%">Toronto</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Qualité des eaux souterraines dans l&amp;rsquo;Atlas saharien: Cas du bassin néogène d&amp;rsquo;El-Outaya (Sud algérien), ISSN 2170-1318 Juin 2013,</style></title><secondary-title><style face="normal" font="default" size="100%"> Algerian Journal of Arid Environment “AJAE“</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://revues.univ-ouargla.dz/index.php/volume3-numero1-journal-2013/1301-qualite-des-eaux-souterraines-dans-l-atlas-saharien-cas-du-bassin-neogene-d-el-outaya-sud-algerien-brinis-nafaa-boudoukha-abderrahmane</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Volume 3</style></volume><pages><style face="normal" font="default" size="100%">pp 89-97</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;em&gt;&lt;span style=&quot;10pt;&quot; lang=&quot;EN-US&quot;&gt;The plain of El-Outaya is located in arid zone of the Saharan Atlas in southern Algeria. The groundwater are characterized by an Important and variability of the salinity. &lt;/span&gt;&lt;/em&gt;&lt;em&gt;&lt;span style=&quot;10pt;&quot; lang=&quot;EN-GB&quot;&gt;The geology indicates that the plain is constituted by evaporitic rocks. The Dj. El Melah (trias) takes a very important place in the geology of the plain by its lithological composition and its abnormal contacts with the formations around.&lt;span&gt;&amp;nbsp; &lt;/span&gt;Evaporation in the area is very important and consumes the majority of the precipitations.&lt;span&gt;&amp;nbsp; &lt;/span&gt;The heterogeneity of the aquifer of neogene is caused by the presence of clay in variable proportions. The combination between the tools, geological, hydrodynamic, statistical and chemical in the study of the mineralisation allowed us to determine its origin and its evolution in the space.&lt;span&gt;&amp;nbsp; &lt;/span&gt;The analysis of groundwater samples indicates the presence in strong concentrations of &lt;/span&gt;&lt;/em&gt;&lt;em&gt;&lt;span style=&quot;10pt;&quot; lang=&quot;EN-US&quot;&gt;Cl&lt;sup&gt;-&lt;/sup&gt;, SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2-&lt;/sup&gt;, Na&lt;sup&gt;+&lt;/sup&gt; and Mg2&lt;sup&gt;+&lt;/sup&gt;.&lt;/span&gt;&lt;/em&gt;</style></abstract><issue><style face="normal" font="default" size="100%">numéro 1</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Marmi Ramdane</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Le remplissage sédimentaire du bassin de Timgad et aquifères potentiels (atlas saharien Algérien oriental). ISSN 1813-548X.</style></title><secondary-title><style face="normal" font="default" size="100%">Afrique SCIENCE </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://www.afriquescience.info/document.php?id=2929.</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Vol 09</style></volume><pages><style face="normal" font="default" size="100%">pp 66–76</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p class=&quot;resume&quot; lang=&quot;fr-FR&quot;&gt;
	Le bassin de Timgad, orienté suivant une direction sub-latitudinale, appartient à l’Atlas Saharien nord-oriental. Il est bordé au nord par Dj. Bou Arif-Dj. Fedjoudj-Dj. Tarf et au sud par les Monts des Aurès.
&lt;/p&gt;

&lt;p class=&quot;resume&quot; lang=&quot;fr-FR&quot;&gt;
	Il comprend un substratum mésozoïque correspondant à une série marine gréso-carbonatée, surmonté en discordance par des formations du Néogène. Ces derniers sont représentés &amp;nbsp;essentiellement par des sédiments détritiques où dominent les dépôts silicoclastiques. La puissance de toute la série dépasse les 1000 mètres. Le contact, entre les deux séries &amp;nbsp;lithostratigraphiques, mésozoïque et néogènes, est souligné par une discordance majeure marquée tantôt par des conglomérats polygéniques, tantôt par des niveaux calcaires souvent gréseux. Le Plio-Quaternaire, représenté surtout par des sédiments détritiques grossiers, surmonte en discordance les séries antérieures.
&lt;/p&gt;

&lt;p class=&quot;resume&quot; lang=&quot;fr-FR&quot;&gt;
	Du point de vue structurale, le bassin est affecté par une tectonique polyphasée qui l’a compartimenté en blocs dont les accidents transverses NW-SE et NE-SW sont nettement exprimés. La phase compressive, située à la limite pliocène-quaternaire, serait à l’origine du modelé du relief actuel.
&lt;/p&gt;

&lt;p class=&quot;resume&quot; lang=&quot;fr-FR&quot;&gt;
	L’étude géophysique, consistant en l’exploitation &amp;nbsp;des profils sismiques et des coupes géo électriques, a permis de mettre en évidence d’une part la géométrie profonde des différents accidents dans le bassin et les aquifères potentiels d’autre part. Une formation relativement résistante, correspond à un intervalle gréseux du Miocène, revêt un intérêt particulier sur le plan hydrogéologique.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">Issue 3</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Marmi R</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Le remplissage sédimentaire du bassin de Timgad et aquifères potentiels (Atlas saharien Algérien oriental)&amp;raquo;.1 septembre 2013, ISSN 1813-548X.</style></title><secondary-title><style face="normal" font="default" size="100%"> Afrique Science</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://www.afriquescience.info/document.php?id=2929.</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Vol.09</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p class=&quot;resume&quot; lang=&quot;fr-FR&quot;&gt;
	Le bassin de Timgad, orienté suivant une direction sub-latitudinale, appartient à l’Atlas Saharien nord-oriental. Il est bordé au nord par Dj. Bou Arif-Dj. Fedjoudj-Dj. Tarf et au sud par les Monts des Aurès.
&lt;/p&gt;

&lt;p class=&quot;resume&quot; lang=&quot;fr-FR&quot;&gt;
	Il comprend un substratum mésozoïque correspondant à une série marine gréso-carbonatée, surmonté en discordance par des formations du Néogène. Ces derniers sont représentés &amp;nbsp;essentiellement par des sédiments détritiques où dominent les dépôts silicoclastiques. La puissance de toute la série dépasse les 1000 mètres. Le contact, entre les deux séries &amp;nbsp;lithostratigraphiques, mésozoïque et néogènes, est souligné par une discordance majeure marquée tantôt par des conglomérats polygéniques, tantôt par des niveaux calcaires souvent gréseux. Le Plio-Quaternaire, représenté surtout par des sédiments détritiques grossiers, surmonte en discordance les séries antérieures.
&lt;/p&gt;

&lt;p class=&quot;resume&quot; lang=&quot;fr-FR&quot;&gt;
	Du point de vue structurale, le bassin est affecté par une tectonique polyphasée qui l’a compartimenté en blocs dont les accidents transverses NW-SE et NE-SW sont nettement exprimés. La phase compressive, située à la limite pliocène-quaternaire, serait à l’origine du modelé du relief actuel.
&lt;/p&gt;

&lt;p class=&quot;resume&quot; lang=&quot;fr-FR&quot;&gt;
	L’étude géophysique, consistant en l’exploitation &amp;nbsp;des profils sismiques et des coupes géo électriques, a permis de mettre en évidence d’une part la géométrie profonde des différents accidents dans le bassin et les aquifères potentiels d’autre part. Une formation relativement résistante, correspond à un intervalle gréseux du Miocène, revêt un intérêt particulier sur le plan hydrogéologique.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%"> N°03</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude géologique du bassin de Timgad</style></title><secondary-title><style face="normal" font="default" size="100%">La Géologie du Sahara: Ressources minérales, en hydrocarbures et en eau ; 03, 04 et 05 Décembre à l’université KASDI Merbah-Ouargla</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2012</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Marmi Ramdane</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation géologique et hydrogéologique du bassin de Timgad</style></title><secondary-title><style face="normal" font="default" size="100%">La Géologie du Sahara: Ressources minérales, en hydrocarbures et en eau ; 03, 04 et 05 Décembre à l’université KASDI Merbah-Ouargla</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2012</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Kerboub A</style></author><author><style face="normal" font="default" size="100%">Labchek S</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Cartographie géotechnique du POS N&amp;deg; 08. N&amp;rsquo;gaous. Batna</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2012</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Righat Z</style></author><author><style face="normal" font="default" size="100%">Morghad B </style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractéristiques géologiques, hydrogéologiques et géotechniques de la localité d&amp;rsquo;El-Hdeb (W) ouargla. Univ de Batna.</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2012</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Benmansour S</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Yahaoui Abedel Ouahab</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">analyse microfaciologique et découpage séquentiel de la série cénomanienne de la coupe de Mennchar Ali Guera (nord-est Algérie)</style></title><secondary-title><style face="normal" font="default" size="100%">La Géologie du Sahara: Ressources minérales, en hydrocarbures et en eau&quot; ; 03, 04 et 05 Décembre à l’université KASDI Merbah-Ouargla </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2012</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Bouchagoura I</style></author><author><style face="normal" font="default" size="100%">Rouabhia A</style></author><author><style face="normal" font="default" size="100%">Djabri Larbi</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Mise en évidence de la qualité des eaux de la nappe alluviale de tebessa (Est algérien)</style></title><secondary-title><style face="normal" font="default" size="100%">Troisième Forum de l’eau, Tunisie 26 -28 mars </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2012</style></year></dates><pub-location><style face="normal" font="default" size="100%">Tunisie</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude de la qualité des eaux souterraines utilisées pour l&amp;rsquo;irrigation de la plaine d&amp;rsquo;El-Outaya au sud Algérien</style></title><secondary-title><style face="normal" font="default" size="100%">2eme colloque international sur la géologie du Sahara Algérien: Ressources minérales, en hydrocarbures et en eaux, Ouargla, Décembre </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2012</style></year></dates><pub-location><style face="normal" font="default" size="100%">Ouargla, Alger</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author><author><style face="normal" font="default" size="100%">Hamel Ahmed</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude de la qualité chimique des eaux souterraines dans les Aurès (Cas de la vallée de l&amp;rsquo;oued Abiod), Algérie</style></title><secondary-title><style face="normal" font="default" size="100%">2eme colloque international sur la géologie du Sahara Algérien: Ressources minérales, en hydrocarbures et en eaux, Ouargla, Décembre </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2012</style></year></dates><pub-location><style face="normal" font="default" size="100%">Ouargla, Alger</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Inal Ahmed</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude géologique du bassin de Timgad 2</style></title><secondary-title><style face="normal" font="default" size="100%">eme colloque international sur la géologie du Sahara Algérien: Ressources minérales, en hydrocarbures et en eaux, Ouargla, Décembre</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2012</style></year></dates><pub-location><style face="normal" font="default" size="100%">Ouargla,Alger</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Bouchagoura I</style></author><author><style face="normal" font="default" size="100%">Djabri Larbi</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Incidence des pluies exceptionnelles de l&amp;rsquo;été 2002 sur la nappe alluviale de Tebessa. Algérie</style></title><secondary-title><style face="normal" font="default" size="100%">2eme colloque international sur la géologie du Sahara Algérien: Ressources minérales, en hydrocarbures et en eaux, Ouargla, Décembre </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2012</style></year></dates><pub-location><style face="normal" font="default" size="100%">Ouargla, Alger</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude géologique du bassin de Timgad</style></title><secondary-title><style face="normal" font="default" size="100%">La Géologie du Sahara: Ressources minérales, en hydrocarbures et en eau 03, 04 et 05 Décembre à l’université KASDI Merbah-Ouargla. </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2012</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Les risques de conflit autour des eaux transfrontalières -Caractérisation du risque par une indexation numérique. 6-7 juin 2012</style></title><secondary-title><style face="normal" font="default" size="100%">Communication orale au colloque  international sur la gestion intégrée des ressources en eau, ABH-CSM, Constantine</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2012</style></year></dates><pub-location><style face="normal" font="default" size="100%">Constantine</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Assessment of the risk of conflict around the transboundary water resources. Cases of the Jordan Basin and the Guarani Aquifer System 7-10 May 2012</style></title><secondary-title><style face="normal" font="default" size="100%">Orale Communication at the Sixteenth International Water Technology Conference (IWTC16), Istanbul – Turkey</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2012</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">www.iwtc.info </style></url></web-urls></urls><pub-location><style face="normal" font="default" size="100%">Istanbul – Turkey</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">The artificial recharge of the aquifers by considering the groundwater vulnerability to pollution. 7-10 May 2012</style></title><secondary-title><style face="normal" font="default" size="100%">Orale Communication at the Sixteenth International Water Technology Conference (IWTC16), Istanbul – Turkey</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2012</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">www.iwtc.info</style></url></web-urls></urls><pub-location><style face="normal" font="default" size="100%">Istanbul – Turkey</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Drias Tarek</style></author><author><style face="normal" font="default" size="100%">Toubal Ahmed Chérif</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Alluvial Flow modeling of the aquifer of Tebessa - Extrem eastern of Algeria 2&lt;sup&gt;nd&lt;/sup&gt; international water forum. (3 to 5 may 2011). Istanbul, Turky.</style></title><secondary-title><style face="normal" font="default" size="100%">2nd international water forum. (3 to 5 may). Istanbul, Turky</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2011</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Inal Ahmed</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Malika</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Impact, importance et mobilisation des ressources hydriques dans le bassin miocène de Timgad</style></title><secondary-title><style face="normal" font="default" size="100%">3ème Edition du Congrès International sur l’eau, Déchets et Environnement (EDE3). 21-22 Novembre Troisième Edition du Congrès International : Eau, Déchets et Environnement (EDE3), Fès- Maroc</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2011</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Lebghil A</style></author><author><style face="normal" font="default" size="100%">Djedai Y</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation du système d&amp;rsquo;auscultation du barrage d&amp;rsquo;Ourkiss (Willaya d&amp;rsquo;Oum El Bouaghi).</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2011</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Benaicha H</style></author><author><style face="normal" font="default" size="100%">Righi Asma</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à l&amp;rsquo;étude géotechnique du barrage Yabous &amp;ndash;Khenchela. Univ de Batna.</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2011</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Une approche des indicateurs de conflits liés aux  eaux transfrontalières -Développement d&amp;rsquo;une indexation numérique du risque de conflit</style></title><secondary-title><style face="normal" font="default" size="100%">Communication Orale, CIRED’4, Alger, 22-23 Fevrier 2011</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2011</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation chimique des effluents d&amp;rsquo;un complexe de transformation de sel : cas du complexe ENASEL d&amp;rsquo;El-Outaya au sud &amp;ndash;Est algérien </style></title><secondary-title><style face="normal" font="default" size="100%">Troisième congrès international sur l’eau, déchet et environnement, Maroc : 21 et 22 Nov </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2011</style></year></dates><pub-location><style face="normal" font="default" size="100%">Maroc </style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Inal Ahmed</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">Athamena. S</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Impact, importance et mobilisation des ressources hydriques dans le bassin miocène de Timgad  </style></title><secondary-title><style face="normal" font="default" size="100%">3ème Edition du Congrès  International sur l’eau, Déchets et Environnement (EDE3). 21-22 Novembre. Troisième Edition du Congrès International : Eau, Déchets et Environnement (EDE3), Fès- Maroc</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2011</style></year></dates><pub-location><style face="normal" font="default" size="100%">Fès- Maroc</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">Da Silva HL</style></author><author><style face="normal" font="default" size="100%">Lepri LR</style></author><author><style face="normal" font="default" size="100%">Franco ILC</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Assessment of the risk of conflict around the water resources of the Guarani aquifer system. Com 25-29 septembre 2011</style></title><secondary-title><style face="normal" font="default" size="100%">Orale, XIVth World Water Congress of IWRA, Porto de Galinhas</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2011</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%"> http://worldwatercongress.com/programa_wwc_silusba_site.pdf</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Classification statistique et hydrochimique des eaux souterraines de la plaine d&amp;#39;El-Outaya. (W) de Biskra. Algérie. Mars 2011, .</style></title><secondary-title><style face="normal" font="default" size="100%">Publication au courrier du savoir, Univ-Biskra</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2011</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.google.dz/url?sa=t&amp;rct=j&amp;q=&amp;esrc=s&amp;source=web&amp;cd=1&amp;cad=rja&amp;uact=8&amp;ved=2ahUKEwjxuZfk08PgAhVMWxoKHTWGD-4QFjAAegQIARAC&amp;url=http%3A%2F%2Frevues.univ-biskra.dz%2Findex.php%2Fcds%2Farticle%2Fview%2F463%2F430&amp;usg=AOvVaw1mnRGClc7vjxfQx5pyZijR</style></url></web-urls></urls><pages><style face="normal" font="default" size="100%">pp 41-46</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">The plain of El-Outaya is in arid zone in southern Algeria. The groundwater are characterized by an Important and variability&lt;br&gt;in its salinity. This work is presented to improve knowledge on these waters by proceeding to their statistical and&lt;br&gt;hydrochemical classifications. Method C.A.H (hierarchical ascending classification) takes of three tendencies based on the&lt;br&gt;importance of the mineralization. The salt rocks are responsible of this height salinity. Concerning the hydrochemical&lt;br&gt;synthesis, the statistical information is confirmed. There is three dominant groups.</style></abstract><issue><style face="normal" font="default" size="100%">N°11</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Marmi Ramdane</style></author><author><style face="normal" font="default" size="100%">Benabbas C</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Découverte de nouveaux gisements de Mammifères dans le Constantinois (Algérie nord-orientale) : Intérêt biostratigraphique</style></title><secondary-title><style face="normal" font="default" size="100%">1er Congrès International sur la Géologie du Maghreb 5 GéoMag 1), Tlemcen 10-12 novembre</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2010</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Inal Ahmed</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Importance des carrières dans la vie socio-économique et leurs impacts sur l&amp;rsquo;environnement (Batna-Ain Touta)</style></title><secondary-title><style face="normal" font="default" size="100%">1er Congrès sur la Géologie du Maghreb. 10-12 Novembre Tlemcen, Algérie.</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2010</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Bounouara M</style></author><author><style face="normal" font="default" size="100%">Hani F</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Étude géotechnique du POS de Bardo. Constantine</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2010</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Touka A</style></author><author><style face="normal" font="default" size="100%">Rahmani A </style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation du système d&amp;rsquo;auscultation du barrage Beni Haroun &amp;ndash;MILA. Univ de Batna</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2010</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Laib Y</style></author><author><style face="normal" font="default" size="100%">Touka A</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude des caractéristiques des granulats des carrières sur l&amp;rsquo;axe Ain Touta &amp;ndash;Batna. Univ de Batna</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2010</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Zouaoui Siham</style></author><author><style face="normal" font="default" size="100%">Boumazbeur. A. R</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Zouaoui.S, Boumazbeur.A.R : Etude géologique et géotechnique des glissements de terrains dans le bassin néogène de Mila : Glissement de SIBARI</style></title><secondary-title><style face="normal" font="default" size="100%">1ère séminaire Euro-Méditerranéen. LRNAT’2010’. Batna (Algérie).27.28.29Avril </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2010</style></year></dates><pub-location><style face="normal" font="default" size="100%"> Batna , Algérie</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author><author><style face="normal" font="default" size="100%">Djabri Larbi</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Arguments hydrogéochimiques  de  l&amp;#39;origine  évaporitique  des  eaux  de  l&amp;#39;aquifère  néogène d&amp;#39;El-Outaya,  Biskra  -Algérie-</style></title><secondary-title><style face="normal" font="default" size="100%">5eme conférence internationale sur les ressources en eau dans le bassin méditerranéen WATMED 5, Lille France , Mai </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2010</style></year></dates><pub-location><style face="normal" font="default" size="100%"> Lille France</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Azizi Yacine</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%"> Caractérisation du système d&amp;#39;auscultation du barrage réservoir d&amp;#39;Oued Athmania wilaya de Mila (Algérie nord orientale)</style></title><secondary-title><style face="normal" font="default" size="100%">1er colloque international sur la géologie du Sahara Algérien: Ressources minérales, en hydrocarbures et en eaux, Ouargla, Décembre </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2010</style></year></dates><pub-location><style face="normal" font="default" size="100%">Ouargla, Alger</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Inal Ahmed</style></author><author><style face="normal" font="default" size="100%">Cheriet Manel</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Importance des carrières dans la vie socio-économique et leurs impact sur l&amp;#39;environnement (Batna&amp;ndash;Ain Touta)</style></title><secondary-title><style face="normal" font="default" size="100%">1er Congrès  sur la Géologie du Maghreb; Tlemcen </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2010</style></year></dates><pub-location><style face="normal" font="default" size="100%">Tlemcen, Alger</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Choice of the artificial recharge zones and the groundwater Vulnerability to pollution.  2-5 juin 2010</style></title><secondary-title><style face="normal" font="default" size="100%">Communication Orale, GEOMED Conference, Kemer, Turquie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2010</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://web.deu.edu.tr/geomed2010/WebEN/index.html</style></url></web-urls></urls><pub-location><style face="normal" font="default" size="100%">Kemer, Turquie</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Drias Tarek</style></author><author><style face="normal" font="default" size="100%">Toubal Ahmed Chérif</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation hydrodynamique d&amp;rsquo;un aquifère hétérogène sous climat semi-aride. Exemple de la plaine de Tébessa.</style></title><secondary-title><style face="normal" font="default" size="100%">Bulletin du service géologique de l’ANGCM</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2010</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.asjp.cerist.dz/en/article/3152</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Volume 21</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">La zone étudiée fait partie du sous bassin du Mellègue situé au nord- est de l'Algérie. Cette zone est caractérisée par un climat semi-aride. Le système aquifère y est formé par des alluvions plio-quaternaires reposant sur un substratum marneux d'âge eocène. L étude géostatistique des paramètres hydrodynamiques (charge hydraulique, transmissivité) a permis d’appréhender leur évolution spatiale par la méthode du krigeage par bloc et d’identifier les zones à potentialités aquifères. A cet égard, la carte des transmissivités montre une zone préférentielle dans le secteur d’Aïn Chabro, situé au sud de la plaine. Ce secteur présente les meilleures valeurs de la transmissivité (103 à 5x1(L2 m2/s). L’utilisation d’un modèle bidimensionnel aux différences finies, a permis d’établir le bilan global de la nappe et d’affiner le champ des transmissivités. Celles-ci varieraient plutôt entre KL4 à KL2 m2/s. La démarche méthodologique, associant l’approche probabiliste sous-tendue par la théorie des variables régionalisées à celle déterministe du modèle, conduit à une meilleure connaissance de l’hydrogéologie de cette zone semi aride.</style></abstract><issue><style face="normal" font="default" size="100%">N° 3</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Détermination des sites de recharge artificielle de l&amp;rsquo;aquifère alluvial de la plaine d&amp;rsquo;El Madher (Région de Batna, Nord-Est algérien).</style></title><secondary-title><style face="normal" font="default" size="100%">Bulletin du Service Géologique National de l'ANGCM</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2010</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://www.energy.gov.dz/francais/index.php?page=478</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Vol. 21</style></volume><pages><style face="normal" font="default" size="100%">pp. 329-347</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><issue><style face="normal" font="default" size="100%">n°3</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author><author><style face="normal" font="default" size="100%">Djabri Larbi</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Evolution des Facies Chimiques des Eaux Souterraines dans da Plaine D&amp;rsquo;el-Outaya, Biskra, Algérie. Dec. 2010.</style></title><secondary-title><style face="normal" font="default" size="100%">Journal International Environmental Conflict Management, Santa Catarina – Brazil</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2010</style></year></dates><volume><style face="normal" font="default" size="100%">Vol 1</style></volume><pages><style face="normal" font="default" size="100%">pp. 98-105</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><issue><style face="normal" font="default" size="100%">N°1</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Les conflits transfrontaliers sur l&amp;rsquo;eau : Tendances actuelles. Sécheresse, Janvier-mars 2010, John Libbey Eurotext Paris</style></title><secondary-title><style face="normal" font="default" size="100%">Sécheresse</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2010</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://www.secheresse.info/spip.php?article10060</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Vol. 21</style></volume><pages><style face="normal" font="default" size="100%">pp. 22-27</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;div class=&quot;texte&quot;&gt;
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			Du fait qu’elle est indispensable, l’eau a été utilisée depuis l’Antiquité comme arme dans les conflits. Par exemple, en 596 av. J.-C., lors du siège de la cité de Tyr, Nabuchodonosor avait détruit une partie de l’aqueduc qui l’approvisionnait. En 1938, afin d’inonder les zones menacées par l’armée japonaise, Tchang Kaï-Chek ordonne la destruction des digues d’écrêtement des crues sur une partie du fleuve Jaune. L’inondation détruisit une partie des forces d’invasion, mais noya également des milliers de Chinois. D’autres violations, qui se sont déroulées pendant la seconde guerre mondiale ou la durant la guerre du Vietnam, avaient trait aux équipements hydroélectriques et aux digues qui étaient prises comme cibles lors des bombardements. Dans d’autres cas, c’est l’insuffisance de la ressource qui est la cause de tensions extrêmes et de stratégies expansionnistes, comme c’est le cas de l’éternel conflit transfrontalier entre Israël et les pays arabes voisins, autour des eaux du Jourdain. À l’échelle locale, voire parcellaire, le principal argument de conflit relève de l’usage qui concerne notamment l’irrigation des terres et le respect des quotas imposés par des règles ancestrales. Cet ingrédient prend une autre dimension lorsqu’il est mêlé à l’espace politique ou ethnique d’une population donnée, et ce même si la ressource est abondante. Même si certaines études alarmistes, telles celles qui concernent particulièrement les zones arides du Proche-Orient, prédisent des conflits violents autour de l’eau, des initiatives reposant sur des considérations juridiques, humanitaires, économiques et scientifiques sont menées par la communauté internationale afin de prévenir le péril que constituent les conflits liés à l’eau en plusieurs endroits sensibles de la planète.&lt;img src=&quot;https://www.jle.com/_/droit/sec/--/resume/free/283760.png&quot; style=&quot;display:block;&quot; width=&quot;1&quot; height=&quot;0&quot; border=&quot;0&quot;&gt;
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</style></abstract><issue><style face="normal" font="default" size="100%">N°1</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Drias Tarek</style></author><author><style face="normal" font="default" size="100%">Toubal Ahmed Chérif</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Heterogeneous aquifer system modelization under semi-arid climate. Geophysical Research Abstracts, EGU2010-178,</style></title><secondary-title><style face="normal" font="default" size="100%">EGU General Assembly</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2010</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">ftp://ftp.gfz-potsdam.de/home/cegit/egu/pdf/EGU2010-178.pdf </style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Vol. 12</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;span style=&quot;left:120px;top:354.469px;16.6043px;sans-serif;transform:scaleX(0.912423);&quot;&gt;The studied zone is a part of the Mellegne’s (North-East of Algeria) under pound, this zone is characterised by its&lt;/span&gt;&lt;span style=&quot;left:120px;top:374.394px;16.6043px;sans-serif;transform:scaleX(0.921716);&quot;&gt;semi-arid climate.&lt;/span&gt;&lt;span style=&quot;left:120px;top:394.319px;16.6043px;sans-serif;transform:scaleX(0.871352);&quot;&gt;The water bearing system is formed by the plio-quaternairy alluviums resting on a marley substratuim of age&lt;/span&gt;&lt;span style=&quot;left:120px;top:414.244px;16.6043px;sans-serif;transform:scaleX(0.870331);&quot;&gt;Eocene.&lt;/span&gt;&lt;span style=&quot;left:120px;top:434.171px;16.6043px;sans-serif;transform:scaleX(0.941556);&quot;&gt;The geostatiscitcs approach of the hydrodynamics parameters (Hydrolic load, transmisivity) allowed the study&lt;/span&gt;&lt;span style=&quot;left:120px;top:454.096px;16.6043px;sans-serif;transform:scaleX(0.95235);&quot;&gt;of their spatial distrubution (casting) by the method of Krigeage by blocks and the identification of zones with&lt;/span&gt;&lt;span style=&quot;left:120px;top:474.021px;16.6043px;sans-serif;transform:scaleX(0.915133);&quot;&gt;water-bearing potentialities.&lt;/span&gt;&lt;span style=&quot;left:120px;top:493.946px;16.6043px;sans-serif;transform:scaleX(0.937062);&quot;&gt;In this respect, the zone of Ain Chabro which, is situated in the South of the plain shows the best values of the&lt;/span&gt;&lt;span style=&quot;left:120px;top:513.871px;16.6043px;sans-serif;transform:scaleX(0.935078);&quot;&gt;transmisivity......&lt;/span&gt;&lt;span style=&quot;left:120px;top:533.796px;16.6043px;sans-serif;transform:scaleX(0.928924);&quot;&gt;The use of a bidimensinnel model in the differences ended in the permanent regime allowed us to establish the&lt;/span&gt;&lt;span style=&quot;left:120px;top:553.722px;16.6043px;sans-serif;transform:scaleX(0.914152);&quot;&gt;global balence sheet (overall assessment) of the tablecloth and to refine the transmisivity field. These would vary&lt;/span&gt;&lt;span style=&quot;left:120px;top:573.647px;16.6043px;sans-serif;transform:scaleX(0.903086);&quot;&gt;more exactley between 10-4 to 10-2 m&lt;/span&gt;&lt;span style=&quot;left:375.88833333333326px;top:570.9979393333333px;11.623px;sans-serif;&quot;&gt;2&lt;/span&gt;&lt;span style=&quot;left:382.53px;top:573.647px;16.6043px;sans-serif;transform:scaleX(0.868413);&quot;&gt;/s.&lt;/span&gt;&lt;span style=&quot;left:120px;top:593.572px;16.6043px;sans-serif;transform:scaleX(0.882508);&quot;&gt;The method associating the probability appraoch of Krigeage to that determining the model has facilited the&lt;/span&gt;&lt;span style=&quot;left:120px;top:613.497px;16.6043px;sans-serif;transform:scaleX(0.926475);&quot;&gt;wedging of the model and clarified the inflitration value&lt;/span&gt;</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Drias Tarek</style></author><author><style face="normal" font="default" size="100%">Toubal Ahmed Chérif</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Hydrodynamical characterization of a heterogeneous aquifer system under semi-arid climate Example of the plain of  Tébessa </style></title><secondary-title><style face="normal" font="default" size="100%">The First international symposium of the petroleum and geological resources in the tethys realm. Cairo, Egypt</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2009</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Impact des ressources hydriques sur le développement durable dans le basin de Timgad-Algérie Nord Orientale</style></title><secondary-title><style face="normal" font="default" size="100%">1er Colloque International sur la Gestion Intégrée des Ressources. en eau. 10 – 11 Novembre Département des Sciences de la Terre – Faculté des Sciences Université de Batna.</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2009</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Yellouz H</style></author><author><style face="normal" font="default" size="100%">Seghiri M </style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude géotechnique du barrage de Ourkis &amp;ndash;Oum El-Bouaghi. Univ de Batna</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2009</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author><author><style face="normal" font="default" size="100%">Djabri Larbi</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Evolution des Facies Chimiques des Eaux Souterraines dans da Plaine D&amp;rsquo;el-Outaya, Biskra, Algérie </style></title><secondary-title><style face="normal" font="default" size="100%">Colloque international gestion intégrée des ressources en eau (GIRE), Batna</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2009</style></year></dates><pub-location><style face="normal" font="default" size="100%">Batna, Alger</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Rihani A</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Hydrogéologie d&amp;rsquo;une vallée Auressienne &amp;ndash; Cas de la Vallée de Bouzina. 10-11 novembre 2009</style></title><secondary-title><style face="normal" font="default" size="100%">Communication affichée, 1er Colloque International sur la Gestion Intégrée des Ressources en eau, Batna </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2009</style></year></dates><pub-location><style face="normal" font="default" size="100%">Batna</style></pub-location><pages><style face="normal" font="default" size="100%">p 71</style></pages><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Messekher I</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Evolution de la piézométrie de la ville de Oued Souf (entre 1993, 2002 et 2007) - Perspectives de la maitrise du phénomène de remontée de la nappe phréatique. 10-11 novembre </style></title><secondary-title><style face="normal" font="default" size="100%">Communication orale, 1er Colloque International sur la Gestion Intégrée des Ressources en eau, Batna </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2009</style></year></dates><pub-location><style face="normal" font="default" size="100%">Batna</style></pub-location><pages><style face="normal" font="default" size="100%">p 47</style></pages><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%"> Retrospective sur les conflits transfrontaliers sur l&amp;rsquo;eau, 10-11 novembre 2009</style></title><secondary-title><style face="normal" font="default" size="100%">Communication orale 1er Colloque International sur la Gestion Intégrée des Ressources en eau, Batna </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2009</style></year></dates><pub-location><style face="normal" font="default" size="100%">Batna</style></pub-location><pages><style face="normal" font="default" size="100%">p 38</style></pages><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution au choix des sites de recharge artificielle de l&amp;rsquo;aquifère alluvial de la plaine d&amp;rsquo;El Madher (région de Batna, nord-est algérien) 10-11 novembre 2009</style></title><secondary-title><style face="normal" font="default" size="100%">Communication orale 1er Colloque International sur la Gestion Intégrée des Ressources en eau, Batna </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2009</style></year></dates><pub-location><style face="normal" font="default" size="100%">Batna</style></pub-location><pages><style face="normal" font="default" size="100%">p 26</style></pages><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Can we classify the conflict risks around the transboundary water resources? Case of the Jordan basin. 04-06 mars 2009</style></title><secondary-title><style face="normal" font="default" size="100%">Communication orale Encontro Internacional de Direito ambiental na Amazonia, Macapá – Amapá, Brazil</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2009</style></year></dates><pub-location><style face="normal" font="default" size="100%">Macapá – Amapá, Brazil</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author><author><style face="normal" font="default" size="100%">Djabri Larbi</style></author><author><style face="normal" font="default" size="100%">Mania Jacky</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">La salinité des eaux souterraines de la zone Est de la plaine d&amp;rsquo;El-Outaya (Région de Biskra, Algérie). .14 fig., 2 tabl.</style></title><secondary-title><style face="normal" font="default" size="100%">Bulletin du Service Géologique National</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2009</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.asjp.cerist.dz/en/article/1921</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Vol.20</style></volume><pages><style face="normal" font="default" size="100%">pp 49-61</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Ce travail a été réalisé en zone aride et concerne la salinité des eaux de la nappe du MioPlio- Quaternaire de la plaine d’El-Outaya (région de Biskra au sud algérien). Cette plaine est le résultat d un remplissage néogène qui repose en discordance sur tous les terrains antérieurs mésozoïques et paléogènes. Le Trias avec son diapir de sel reste un élément très important dans cette plaine par sa composition lithologique et ses contacts anormaux avec les autres formations. Le contact de l aquifère étudié avec le substratum se fait soit par des conglomérats, soit par des argiles. L’hétérogénéité de la nappe du Mio-Pliocène se caractérise par la présence d argile dans des proportions variables. L’évaporation dans la région est très intense et consomme la majorité des précipitations. La combinaison entre les outils, géologique, géophysique, statistique et chimique dans l’étude du problème de la salinité permet de déterminer l’origine et l évolution dans l’espace de cette dernière. Les analyses effectuées indiquent la présence en fortes concentrations des éléments CT, S042\ Na + et Mg+. Dans la partie nord et ouest, les eaux sont caractérisées par un faciès chloruré sodique (influence de la halite), à Test, le faciès sulfaté magnésien domine (influence du gypse). Entre ces deux faciès, on note une zone où les eaux sont mixtes, caractérisées par un faciès sulfaté sodique (échange de base). L’interprétation thermodynamique a permis la détermination de l’influence des minéraux évaporitiques à des degrés variables dans la composition chimique des eaux. Ces minéraux sont à l’origine de la salinité des eaux de la région. Les minéraux carbonatés se trouvent sursaturés dans l’eau.</style></abstract><issue><style face="normal" font="default" size="100%">N°1</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">A numerical method to index the risk of conflict around the transboundary water resources. Validation by a studied case. Water Resources, November 2009, Pleiades Publishing Ltd</style></title><secondary-title><style face="normal" font="default" size="100%">Springer</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2009</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.1134/S0097807809060128</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Vol. 36</style></volume><pages><style face="normal" font="default" size="100%">pp. 731-742</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">The world-wide crisis of water will make that the transboundary water resources will be the object of tensions and litigations increasingly marked. Also, the transboundary conflicts on fresh water intended to the categories of traditional uses are subjected to a growing attention on behalf of national and international organizations. Each case of conflict, related as well to surface water as groundwater, has its accurate characteristics and to appreciate its relative importance, it is necessary to consult a broad documentation based on reports of commissions, organizations or groups of research. According to criteria and data taken into account, the situation is some times appreciated differently.</style></abstract><issue><style face="normal" font="default" size="100%"> N°6</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">The Artificial Recharge and the Groundwater Vulnerability to Pollution-Case of the El Madher Plain (North East of Algeria)</style></title><secondary-title><style face="normal" font="default" size="100%">European Journal of Scientific Research</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2009</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.researchgate.net/publication/287026868_The_artificial_recharge_and_the_groundwater_vulnerability_to_pollution-case_of_the_El_Madher_Plain_North_East_of_Algeria</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Vol.32</style></volume><pages><style face="normal" font="default" size="100%">pp.288-303</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Reduction of water resources has led water managers to search for adequate solutions to respond to increasing demand. Artificial recharge of aquifers by resources drawn from far away is a mobilisation mode adopted especially in arid areas. The cost of this operation is often very high but counterbalanced by the advantages provided by this mean: • mobilisation of this resource in zones were it's very available; • injection by different means in aquifer zones whose characteristics are known; • a storage mode which allows to conserve resources from evaporation, as opposed to storage in dams that are also confronted to deposits that reduces considerably their capacity; • Artificial recharge can also benefit from natural mean of transport when it takes into account the groundwater hydraulic gradient at a time of choosing injection zones. Artificial recharge by direct recharge on permeable zones constitutes the most used mean but such zones are the most vulnerable to pollution. The cartography of the groundwater pollution potential of a given area, combined to repartition of favourable zones to artificial recharge, constitute a tool to decision making concerning the choice of recharge zones that takes into account environmental aspects. This approach is applied to the El Madher plain which is located just at the North of Batna city (North-East of Algeria).</style></abstract><issue><style face="normal" font="default" size="100%">No.3</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">Bennedjai Nassima</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Statistical approach of the physiographical parameters influence on runoffs observed at the exit of basins - a case of Algerian basins. May 2009</style></title><secondary-title><style face="normal" font="default" size="100%">ARPN Journal of Engineering and Applied Science</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2009</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://www.arpnjournals.com/jeas/research_papers/rp_2009/jeas_0509_184.pdf</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Vol. 4</style></volume><pages><style face="normal" font="default" size="100%">pp. 48-53</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;span style=&quot;left:144px;top:410.918px;16.7px;serif;transform:scaleX(0.996238);&quot;&gt;Th&lt;/span&gt;&lt;span style=&quot;left:162.567px;top:410.918px;16.7px;serif;transform:scaleX(0.919515);&quot;&gt;e p&lt;/span&gt;&lt;span style=&quot;left:184.845px;top:410.918px;16.7px;serif;transform:scaleX(0.997315);&quot;&gt;redetermin&lt;/span&gt;&lt;span style=&quot;left:257.071px;top:410.918px;16.7px;serif;transform:scaleX(0.995798);&quot;&gt;atio&lt;/span&gt;&lt;span style=&quot;left:282.087px;top:410.918px;16.7px;serif;transform:scaleX(0.942679);&quot;&gt;n of the runo&lt;/span&gt;&lt;span style=&quot;left:374.918px;top:410.918px;16.7px;serif;transform:scaleX(0.913977);&quot;&gt;ff &lt;/span&gt;&lt;span style=&quot;left:392.566px;top:410.918px;16.7px;serif;transform:scaleX(0.937338);&quot;&gt;in the n&lt;/span&gt;&lt;span style=&quot;left:447.456px;top:410.918px;16.7px;serif;transform:scaleX(0.966912);&quot;&gt;on gaug&lt;/span&gt;&lt;span style=&quot;left:503.173px;top:410.918px;16.7px;serif;transform:scaleX(0.966817);&quot;&gt;ed basin&lt;/span&gt;&lt;span style=&quot;left:560.671px;top:410.918px;16.7px;serif;transform:scaleX(0.951855);&quot;&gt;s con&lt;/span&gt;&lt;span style=&quot;left:597.863px;top:410.918px;16.7px;serif;transform:scaleX(0.995991);&quot;&gt;stitu&lt;/span&gt;&lt;span style=&quot;left:626.583px;top:410.918px;16.7px;serif;transform:scaleX(0.95162);&quot;&gt;tes th&lt;/span&gt;&lt;span style=&quot;left:664.639px;top:410.918px;16.7px;serif;transform:scaleX(0.948791);&quot;&gt;e obj&lt;/span&gt;&lt;span style=&quot;left:699.95px;top:410.918px;16.7px;serif;transform:scaleX(0.995027);&quot;&gt;ectiv&lt;/span&gt;&lt;span style=&quot;left:732.324px;top:410.918px;16.7px;serif;transform:scaleX(0.923778);&quot;&gt;e o&lt;/span&gt;&lt;span style=&quot;left:754.704px;top:410.918px;16.7px;serif;transform:scaleX(0.937814);&quot;&gt;f nu&lt;/span&gt;&lt;span style=&quot;left:783.517px;top:410.918px;16.7px;serif;transform:scaleX(0.979598);&quot;&gt;merous research&lt;/span&gt;&lt;span style=&quot;left:894.477px;top:410.918px;16.7px;serif;transform:scaleX(0.917283);&quot;&gt;es &lt;/span&gt;&lt;span style=&quot;left:84px;top:430.018px;16.7px;serif;transform:scaleX(1.02589);&quot;&gt;because of a lack of data covering them&lt;/span&gt;&lt;span style=&quot;left:355.501px;top:430.018px;16.7px;serif;transform:scaleX(1.0414);&quot;&gt;. Thus, the &lt;/span&gt;&lt;span style=&quot;left:433.175px;top:430.018px;16.7px;serif;transform:scaleX(1.04562);&quot;&gt;use of &lt;/span&gt;&lt;span style=&quot;left:479.657px;top:430.018px;16.7px;serif;transform:scaleX(1.00059);&quot;&gt;mathe&lt;/span&gt;&lt;span style=&quot;left:520.567px;top:430.018px;16.7px;serif;transform:scaleX(0.99643);&quot;&gt;matica&lt;/span&gt;&lt;span style=&quot;left:564.995px;top:430.018px;16.7px;serif;transform:scaleX(1.03161);&quot;&gt;l models &lt;/span&gt;&lt;span style=&quot;left:628.101px;top:430.018px;16.7px;serif;transform:scaleX(0.998726);&quot;&gt;beca&lt;/span&gt;&lt;span style=&quot;left:658.759px;top:430.018px;16.7px;serif;transform:scaleX(1.02445);&quot;&gt;me the suitable ap&lt;/span&gt;&lt;span style=&quot;left:782.802px;top:430.018px;16.7px;serif;transform:scaleX(1.02456);&quot;&gt;proach. Runoffs at &lt;/span&gt;&lt;span style=&quot;left:84px;top:449.218px;16.7px;serif;transform:scaleX(1.00889);&quot;&gt;the ex&lt;/span&gt;&lt;span style=&quot;left:124.787px;top:449.218px;16.7px;serif;transform:scaleX(1.01605);&quot;&gt;it o&lt;/span&gt;&lt;span style=&quot;left:147.015px;top:449.218px;16.7px;serif;transform:scaleX(1.00853);&quot;&gt;f basins, in&lt;/span&gt;&lt;span style=&quot;left:220.548px;top:449.218px;16.7px;serif;transform:scaleX(1.01164);&quot;&gt; add&lt;/span&gt;&lt;span style=&quot;left:249.256px;top:449.218px;16.7px;serif;transform:scaleX(0.996176);&quot;&gt;itio&lt;/span&gt;&lt;span style=&quot;left:271.499px;top:449.218px;16.7px;serif;transform:scaleX(1.01162);&quot;&gt;n to being&lt;/span&gt;&lt;span style=&quot;left:339.154px;top:449.218px;16.7px;serif;transform:scaleX(1.00806);&quot;&gt; influ&lt;/span&gt;&lt;span style=&quot;left:375.236px;top:449.218px;16.7px;serif;transform:scaleX(0.996102);&quot;&gt;enced&lt;/span&gt;&lt;span style=&quot;left:414.113px;top:449.218px;16.7px;serif;transform:scaleX(1.0082);&quot;&gt; logically b&lt;/span&gt;&lt;span style=&quot;left:489.94px;top:449.218px;16.7px;serif;transform:scaleX(1.00448);&quot;&gt;y rainfalls and&lt;/span&gt;&lt;span style=&quot;left:585.988px;top:449.218px;16.7px;serif;transform:scaleX(1.02262);&quot;&gt; th&lt;/span&gt;&lt;span style=&quot;left:603.611px;top:449.218px;16.7px;serif;transform:scaleX(1.00963);&quot;&gt;eir in&lt;/span&gt;&lt;span style=&quot;left:638.799px;top:449.218px;16.7px;serif;transform:scaleX(0.997661);&quot;&gt;ten&lt;/span&gt;&lt;span style=&quot;left:659.219px;top:449.218px;16.7px;serif;transform:scaleX(1.00551);&quot;&gt;sities, th&lt;/span&gt;&lt;span style=&quot;left:715.245px;top:449.218px;16.7px;serif;transform:scaleX(1.00968);&quot;&gt;ey are und&lt;/span&gt;&lt;span style=&quot;left:785.571px;top:449.218px;16.7px;serif;transform:scaleX(1.01142);&quot;&gt;er th&lt;/span&gt;&lt;span style=&quot;left:816.134px;top:449.218px;16.7px;serif;transform:scaleX(1.0071);&quot;&gt;e influence &lt;/span&gt;&lt;span style=&quot;left:894.5px;top:449.218px;16.7px;serif;transform:scaleX(1.00137);&quot;&gt;of &lt;/span&gt;&lt;span style=&quot;left:84px;top:468.418px;16.7px;serif;transform:scaleX(0.989975);&quot;&gt;other factors &lt;/span&gt;&lt;span style=&quot;left:179.435px;top:468.418px;16.7px;serif;transform:scaleX(0.99742);&quot;&gt;wh&lt;/span&gt;&lt;span style=&quot;left:199.871px;top:468.418px;16.7px;serif;transform:scaleX(0.99717);&quot;&gt;ich&lt;/span&gt;&lt;span style=&quot;left:220.285px;top:468.418px;16.7px;serif;transform:scaleX(0.988831);&quot;&gt; cond&lt;/span&gt;&lt;span style=&quot;left:260.734px;top:468.418px;16.7px;serif;transform:scaleX(0.997347);&quot;&gt;itio&lt;/span&gt;&lt;span style=&quot;left:282.997px;top:468.418px;16.7px;serif;transform:scaleX(0.986143);&quot;&gt;n the su&lt;/span&gt;&lt;span style=&quot;left:342.566px;top:468.418px;16.7px;serif;transform:scaleX(0.989733);&quot;&gt;rface d&lt;/span&gt;&lt;span style=&quot;left:392.224px;top:468.418px;16.7px;serif;transform:scaleX(0.996229);&quot;&gt;isch&lt;/span&gt;&lt;span style=&quot;left:419.095px;top:468.418px;16.7px;serif;transform:scaleX(0.99281);&quot;&gt;arge such as&lt;/span&gt;&lt;span style=&quot;left:508.1px;top:468.418px;16.7px;serif;transform:scaleX(0.980881);&quot;&gt; th&lt;/span&gt;&lt;span style=&quot;left:529.117px;top:468.418px;16.7px;serif;transform:scaleX(0.983291);&quot;&gt;e ph&lt;/span&gt;&lt;span style=&quot;left:561.133px;top:468.418px;16.7px;serif;transform:scaleX(0.9966);&quot;&gt;ysio&lt;/span&gt;&lt;span style=&quot;left:588.947px;top:468.418px;16.7px;serif;transform:scaleX(0.996511);&quot;&gt;graph&lt;/span&gt;&lt;span style=&quot;left:626.924px;top:468.418px;16.7px;serif;transform:scaleX(0.987927);&quot;&gt;ical p&lt;/span&gt;&lt;span style=&quot;left:667.323px;top:468.418px;16.7px;serif;transform:scaleX(0.994399);&quot;&gt;aram&lt;/span&gt;&lt;span style=&quot;left:700.354px;top:468.418px;16.7px;serif;transform:scaleX(0.989472);&quot;&gt;eters o&lt;/span&gt;&lt;span style=&quot;left:748.172px;top:468.418px;16.7px;serif;transform:scaleX(0.984435);&quot;&gt;f the b&lt;/span&gt;&lt;span style=&quot;left:798.503px;top:468.418px;16.7px;serif;transform:scaleX(0.996913);&quot;&gt;asin&lt;/span&gt;&lt;span style=&quot;left:825.395px;top:468.418px;16.7px;serif;transform:scaleX(0.986469);&quot;&gt;s, lith&lt;/span&gt;&lt;span style=&quot;left:866.196px;top:468.418px;16.7px;serif;transform:scaleX(0.996912);&quot;&gt;olo&lt;/span&gt;&lt;span style=&quot;left:887.538px;top:468.418px;16.7px;serif;transform:scaleX(1.02485);&quot;&gt;gy, &lt;/span&gt;&lt;span style=&quot;left:84px;top:487.518px;16.7px;serif;transform:scaleX(1.00339);&quot;&gt;veget&lt;/span&gt;&lt;span style=&quot;left:120.226px;top:487.518px;16.7px;serif;transform:scaleX(0.999253);&quot;&gt;ation co&lt;/span&gt;&lt;span style=&quot;left:173.446px;top:487.518px;16.7px;serif;transform:scaleX(1.00039);&quot;&gt;ver an&lt;/span&gt;&lt;span style=&quot;left:214.672px;top:487.518px;16.7px;serif;transform:scaleX(1.00299);&quot;&gt;d eva&lt;/span&gt;&lt;span style=&quot;left:250.361px;top:487.518px;16.7px;serif;transform:scaleX(1.00043);&quot;&gt;pora&lt;/span&gt;&lt;span style=&quot;left:279.922px;top:487.518px;16.7px;serif;transform:scaleX(1.00137);&quot;&gt;tion. T&lt;/span&gt;&lt;span style=&quot;left:324.374px;top:487.518px;16.7px;serif;transform:scaleX(1.00446);&quot;&gt;he ai&lt;/span&gt;&lt;span style=&quot;left:356.454px;top:487.518px;16.7px;serif;transform:scaleX(1.00067);&quot;&gt;m of t&lt;/span&gt;&lt;span style=&quot;left:396.317px;top:487.518px;16.7px;serif;transform:scaleX(0.99958);&quot;&gt;his work is to seek&lt;/span&gt;&lt;span style=&quot;left:520.687px;top:487.518px;16.7px;serif;transform:scaleX(0.997406);&quot;&gt; statistical relatio&lt;/span&gt;&lt;span style=&quot;left:634.53px;top:487.518px;16.7px;serif;transform:scaleX(0.999242);&quot;&gt;ns which&lt;/span&gt;&lt;span style=&quot;left:694.407px;top:487.518px;16.7px;serif;transform:scaleX(0.99979);&quot;&gt; bind&lt;/span&gt;&lt;span style=&quot;left:728.339px;top:487.518px;16.7px;serif;transform:scaleX(0.997965);&quot;&gt; run&lt;/span&gt;&lt;span style=&quot;left:754.807px;top:487.518px;16.7px;serif;transform:scaleX(1.00601);&quot;&gt;off o&lt;/span&gt;&lt;span style=&quot;left:786.786px;top:487.518px;16.7px;serif;transform:scaleX(0.998659);&quot;&gt;bserved&lt;/span&gt;&lt;span style=&quot;left:838.738px;top:487.518px;16.7px;serif;transform:scaleX(0.998545);&quot;&gt; at the ex&lt;/span&gt;&lt;span style=&quot;left:899.489px;top:487.518px;16.7px;serif;transform:scaleX(0.999405);&quot;&gt;it &lt;/span&gt;&lt;span style=&quot;left:84px;top:506.718px;16.7px;serif;transform:scaleX(1.00007);&quot;&gt;of basins to rainfalls and&lt;/span&gt;&lt;span style=&quot;left:248.318px;top:506.718px;16.7px;serif;transform:scaleX(1.00174);&quot;&gt; so&lt;/span&gt;&lt;span style=&quot;left:267.475px;top:506.718px;16.7px;serif;transform:scaleX(0.999128);&quot;&gt;me ph&lt;/span&gt;&lt;span style=&quot;left:308.813px;top:506.718px;16.7px;serif;transform:scaleX(0.994615);&quot;&gt;ysiog&lt;/span&gt;&lt;span style=&quot;left:344.892px;top:506.718px;16.7px;serif;transform:scaleX(0.996995);&quot;&gt;raph&lt;/span&gt;&lt;span style=&quot;left:374.577px;top:506.718px;16.7px;serif;transform:scaleX(0.997808);&quot;&gt;ical f&lt;/span&gt;&lt;span style=&quot;left:408.432px;top:506.718px;16.7px;serif;transform:scaleX(0.993996);&quot;&gt;actor&lt;/span&gt;&lt;span style=&quot;left:441.693px;top:506.718px;16.7px;serif;transform:scaleX(0.998963);&quot;&gt;s for basin&lt;/span&gt;&lt;span style=&quot;left:511.312px;top:506.718px;16.7px;serif;transform:scaleX(0.997116);&quot;&gt;s of&lt;/span&gt;&lt;span style=&quot;left:535.919px;top:506.718px;16.7px;serif;transform:scaleX(0.998682);&quot;&gt; Algeria b&lt;/span&gt;&lt;span style=&quot;left:602.722px;top:506.718px;16.7px;serif;transform:scaleX(0.996118);&quot;&gt;etw&lt;/span&gt;&lt;span style=&quot;left:626.825px;top:506.718px;16.7px;serif;transform:scaleX(0.994653);&quot;&gt;een&lt;/span&gt;&lt;span style=&quot;left:649.975px;top:506.718px;16.7px;serif;transform:scaleX(0.995733);&quot;&gt; Septe&lt;/span&gt;&lt;span style=&quot;left:691.211px;top:506.718px;16.7px;serif;transform:scaleX(0.998195);&quot;&gt;mber 198&lt;/span&gt;&lt;span style=&quot;left:754.737px;top:506.718px;16.7px;serif;transform:scaleX(0.999817);&quot;&gt;5 an&lt;/span&gt;&lt;span style=&quot;left:783.122px;top:506.718px;16.7px;serif;transform:scaleX(0.998845);&quot;&gt;d Sep&lt;/span&gt;&lt;span style=&quot;left:820.753px;top:506.718px;16.7px;serif;transform:scaleX(0.995867);&quot;&gt;tem&lt;/span&gt;&lt;span style=&quot;left:845.533px;top:506.718px;16.7px;serif;transform:scaleX(1.00151);&quot;&gt;ber 1993. &lt;/span&gt;&lt;span style=&quot;left:84px;top:525.918px;16.7px;serif;transform:scaleX(0.997157);&quot;&gt;Th&lt;/span&gt;&lt;span style=&quot;left:102.576px;top:525.918px;16.7px;serif;transform:scaleX(0.940704);&quot;&gt;e sim&lt;/span&gt;&lt;span style=&quot;left:139.948px;top:525.918px;16.7px;serif;transform:scaleX(0.955537);&quot;&gt;ple and&lt;/span&gt;&lt;span style=&quot;left:190.558px;top:525.918px;16.7px;serif;transform:scaleX(0.892977);&quot;&gt; m&lt;/span&gt;&lt;span style=&quot;left:209.461px;top:525.918px;16.7px;serif;transform:scaleX(0.99886);&quot;&gt;ultip&lt;/span&gt;&lt;span style=&quot;left:240.104px;top:525.918px;16.7px;serif;transform:scaleX(0.934408);&quot;&gt;le co&lt;/span&gt;&lt;span style=&quot;left:273.992px;top:525.918px;16.7px;serif;transform:scaleX(0.995586);&quot;&gt;rrelatio&lt;/span&gt;&lt;span style=&quot;left:322.074px;top:525.918px;16.7px;serif;transform:scaleX(0.965183);&quot;&gt;ns carried&lt;/span&gt;&lt;span style=&quot;left:389.313px;top:525.918px;16.7px;serif;transform:scaleX(0.913833);&quot;&gt; out on&lt;/span&gt;&lt;span style=&quot;left:439.439px;top:525.918px;16.7px;serif;transform:scaleX(0.90735);&quot;&gt; 23&lt;/span&gt;&lt;span style=&quot;left:462.261px;top:525.918px;16.7px;serif;transform:scaleX(0.92981);&quot;&gt; basi&lt;/span&gt;&lt;span style=&quot;left:495px;top:525.918px;16.7px;serif;transform:scaleX(0.938056);&quot;&gt;ns m&lt;/span&gt;&lt;span style=&quot;left:528.801px;top:525.918px;16.7px;serif;transform:scaleX(0.920198);&quot;&gt;ade it p&lt;/span&gt;&lt;span style=&quot;left:581.827px;top:525.918px;16.7px;serif;transform:scaleX(0.995727);&quot;&gt;ossib&lt;/span&gt;&lt;span style=&quot;left:616.097px;top:525.918px;16.7px;serif;transform:scaleX(0.932654);&quot;&gt;le to emp&lt;/span&gt;&lt;span style=&quot;left:681.949px;top:525.918px;16.7px;serif;transform:scaleX(0.960065);&quot;&gt;hasize th&lt;/span&gt;&lt;span style=&quot;left:742.597px;top:525.918px;16.7px;serif;transform:scaleX(0.934303);&quot;&gt;at some p&lt;/span&gt;&lt;span style=&quot;left:810.308px;top:525.918px;16.7px;serif;transform:scaleX(0.997126);&quot;&gt;hysiog&lt;/span&gt;&lt;span style=&quot;left:854.797px;top:525.918px;16.7px;serif;transform:scaleX(0.995249);&quot;&gt;raph&lt;/span&gt;&lt;span style=&quot;left:884.423px;top:525.918px;16.7px;serif;transform:scaleX(0.995071);&quot;&gt;ical&lt;/span&gt;&lt;span style=&quot;left:84px;top:545.018px;16.7px;serif;transform:scaleX(0.998698);&quot;&gt;characte&lt;/span&gt;&lt;span style=&quot;left:139.457px;top:545.018px;16.7px;serif;transform:scaleX(0.99987);&quot;&gt;ristics are e&lt;/span&gt;&lt;span style=&quot;left:215.409px;top:545.018px;16.7px;serif;transform:scaleX(0.999096);&quot;&gt;xpla&lt;/span&gt;&lt;span style=&quot;left:244.03px;top:545.018px;16.7px;serif;transform:scaleX(1.00023);&quot;&gt;natory of the &lt;/span&gt;&lt;span style=&quot;left:333.482px;top:545.018px;16.7px;serif;transform:scaleX(0.998748);&quot;&gt;varia&lt;/span&gt;&lt;span style=&quot;left:366.72px;top:545.018px;16.7px;serif;transform:scaleX(0.996793);&quot;&gt;nce of th&lt;/span&gt;&lt;span style=&quot;left:425.058px;top:545.018px;16.7px;serif;transform:scaleX(0.997425);&quot;&gt;e ru&lt;/span&gt;&lt;span style=&quot;left:450.585px;top:545.018px;16.7px;serif;transform:scaleX(1.00113);&quot;&gt;noff to sign&lt;/span&gt;&lt;span style=&quot;left:527.464px;top:545.018px;16.7px;serif;transform:scaleX(0.996289);&quot;&gt;ifican&lt;/span&gt;&lt;span style=&quot;left:565.416px;top:545.018px;16.7px;serif;transform:scaleX(0.996457);&quot;&gt;t thresh&lt;/span&gt;&lt;span style=&quot;left:614.949px;top:545.018px;16.7px;serif;transform:scaleX(0.999105);&quot;&gt;olds.&lt;/span&gt;</style></abstract><issue><style face="normal" font="default" size="100%">N° 3</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Djenba Samir</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation géologique et géotechnique des glissements de la ville de Bougaa N.W Sétif</style></title><secondary-title><style face="normal" font="default" size="100%"> 33èmes journées scientifiques internationales du GFHN Avignon France les 19-20 Novembre</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2008</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Djenba Samir</style></author><author><style face="normal" font="default" size="100%">khadidja A</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation géologique et géotechnique des glissements de la ville de Bougaa N.W Sétif </style></title><secondary-title><style face="normal" font="default" size="100%">Colloque international Terre-Eau Annaba les 17, 18,19 Novembre</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2008</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">The impact of hydraulic resources on sustainable development of the Timgad basin north-east of Algerie</style></title><secondary-title><style face="normal" font="default" size="100%">3rd Environmental physics conference Aswan 19-23 Février Egypte [Egyptian Nuclear Physics Association (ENPA)]</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2008</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Djaraf G</style></author><author><style face="normal" font="default" size="100%">Djebar S</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à l&amp;rsquo;étude de stabilité d&amp;rsquo;un tronçon de l&amp;rsquo;autoroute Est-ouest, section (4-2), Elmeridj- Didouch. Constantine.</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2008</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Azizi Yacine</style></author><author><style face="normal" font="default" size="100%">Kerboub D</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation du système d&amp;#39;auscultation du barrage réservoir d&amp;#39;Oued Athmania wilaya de Mila (Algérie nord orientale) Univ de Batna</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2008</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Maalem M</style></author><author><style face="normal" font="default" size="100%">Telali Y</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à l&amp;rsquo;étude des matériaux de construction du barrage Bouggous El Taref. Univ de Batna</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2008</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">La salinité des eaux souterraines dans la région d&amp;rsquo;El-Outaya (Biskra) Algérie</style></title><secondary-title><style face="normal" font="default" size="100%">Journée d’étude et de sensibilisation à la gestion de la ressource en eau dans les régions arides et semi arides. CRSTRA, Biskra le 15 Mars</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2008</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Traitement de la fondation du barrage de fontaine des gazelles-(Biskra) par des injections d&amp;rsquo;étanchéité. Méthodologie et résultats</style></title><secondary-title><style face="normal" font="default" size="100%">Journée d’étude sur les applications des Données Géologiques, Géomorphologiques aux plans d’Aménagement. Laboratoire de Géologie et Environnement. Constantine 29 juin</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2008</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Assurer la durabilité du partenariat Université - Environnement Socio-économique à travers une cellule de veille</style></title><secondary-title><style face="normal" font="default" size="100%">Communication orale programmée aux Journées Nationales d’Etudes et d’Information Sur Le Partenariat Université-Environnement Socio-économique: Défis et Perspectives. Batna, 14 - 15 décembre</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2008</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Numerical indexing of risks of conflicts around the transboundary water resources</style></title><secondary-title><style face="normal" font="default" size="100%">Communication orale au IV International Symposium on Transboundary Water Management. Thessaloniki, Greece,15th-18th October</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2008</style></year></dates><pub-location><style face="normal" font="default" size="100%">Thessaloniki, Greece</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Le phénomène de la remontée des eaux de la nappe phréatique de la cuvette de Ouargla (Sahara algérien),24- 26  juin 2008</style></title><secondary-title><style face="normal" font="default" size="100%"> Communication orale, 10ème  Symposium International de l’eau, Cannes</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2008</style></year></dates><pub-location><style face="normal" font="default" size="100%">Cannes</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Approche d&amp;rsquo;une méthode d&amp;rsquo;indexation numérique des risques de conflits autour des ressources en eau transfrontalières,  24- 26  juin 2008</style></title><secondary-title><style face="normal" font="default" size="100%">Communication orale, 10ème  Symposium International de l’eau, Cannes</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2008</style></year></dates><pub-location><style face="normal" font="default" size="100%">Cannes</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à l&amp;rsquo;étude pétro-structurale de la bordure Est et Sud Est du socle de la Petite Kabylie Nord-Est Algérie. Juin (2008)</style></title><secondary-title><style face="normal" font="default" size="100%">Sciences &amp; Technologie </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2008</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://revue.umc.edu.dz/index.php/d/article/viewFile/482/589</style></url></web-urls></urls><pages><style face="normal" font="default" size="100%">pp. 71-76</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;div style=&quot;left:323.3px;top:766.148px;13.3px;serif;transform:scaleX(1.00075);&quot;&gt;
	The area of study belongs to the higher building of the base of Small Kabylie. It consists of several tectono-lithological units affected by a metamorphism épizonale to mésozonale of low pressure and high temperature. This last estimated at P=4-5 Kbar and T=650-700°C is underlined by the presence of the veins of leucozones and the myrmékite thus near to the field of partial fusion.
&lt;/div&gt;

&lt;div style=&quot;left:352.199px;top:796.849px;13.3px;serif;transform:scaleX(1.00277);&quot;&gt;
	The structural draft shows the superposition of schisto-sandy units épizonales on units of higher rank. This area is overcome in its Western and Eastern part by formations of Oligo-Miocène-Kabyle.
&lt;/div&gt;

&lt;div style=&quot;left:397.2px;top:873.55px;13.3px;serif;transform:scaleX(1.05485);&quot;&gt;
	The study of the syn-schistous deformation highlights an extensive component at vergency is and of the linéations of stretching of direction E - W (D1) with a virgation towards the NNE. This deformation induces the shape in arc marked by plans of schistosity and foliation resulting from the deformation (D2) due to the accommodation of the total overlapping of the building of Beni-Ferguène towards the NW. Alpine and eo-alpine post-schistous deformations of lower (Pt), at vergency East and South, are
&lt;/div&gt;

&lt;div style=&quot;left:94.5px;top:888.85px;13.3px;serif;transform:scaleX(1.00107);&quot;&gt;
	highlighted.
&lt;/div&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">N°27</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Drias Tarek</style></author><author><style face="normal" font="default" size="100%">Toubal Ahmed Chérif</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">De la caractérisation hydrochimique d&amp;rsquo;un système aquifère sous climat semi-aride. Cas de la plaine de Tébessa </style></title><secondary-title><style face="normal" font="default" size="100%">2ème colloque international sur l’eau et l’environnement. 30-31 Janvier  ENSH. Alger. Algérie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2007</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Djenba Samir</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation géologique et géotechnique du gonflement du sol de la région de N&amp;rsquo;Gaous NE Algerien</style></title><secondary-title><style face="normal" font="default" size="100%">32èmes journées scientifiques internationales du GFHN Nantes France les 21-22 Novembre</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2007</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Drias Tarek</style></author><author><style face="normal" font="default" size="100%">Toubal Ahmed Chérif</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation hydrodynamique d&amp;rsquo;un aquifère hétérogène sous climat semi-aride, exemple de la plaine de Tébessa</style></title><secondary-title><style face="normal" font="default" size="100%">4ème journées internationales des géosciences de l’environnement. 08-10 Juin Tétouan. 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Algérie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2007</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Benmansour S</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude stratigraphique et sédimentologique de Manchar Ali Guera, versant Nord de Djebel Bou Arif (Aurès, Nord est D&amp;rsquo;Algérie)</style></title><secondary-title><style face="normal" font="default" size="100%"> Communication au 3ème Séminaire National de Stratigraphie. 19-20-21 et 22 Février, ANGCM/DSGN/ Ministère des énergies/Laghouat</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2007</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Shoot H</style></author><author><style face="normal" font="default" size="100%">Hamel Ahmed</style></author><author><style face="normal" font="default" size="100%">Nezli IE</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Aspect géochimique de la qualité des eaux souterraines exploitées dans les aurès (cas de la vallée de l&amp;rsquo;oued abiod) Algérie</style></title><secondary-title><style face="normal" font="default" size="100%">2eme conférence internationale de la géologie de la Téthys 19-23 mars Caire Egypte</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2007</style></year></dates><pub-location><style face="normal" font="default" size="100%">Caire Egypte</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Hamel Ahmed</style></author><author><style face="normal" font="default" size="100%">Nezli IE</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">L&amp;#39;utilisation du facteur de concentration (Fc) pour le suivi des éléments caractérisant les faciès chimiques des eaux des aurès ALGERIE</style></title><secondary-title><style face="normal" font="default" size="100%">4eme Journées internationales des géosciences de l’environnement. Tetouan 8-10 juin </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2007</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Les Conflits Transfrontaliers sur l&amp;rsquo;Eau</style></title><secondary-title><style face="normal" font="default" size="100%">Communication orale 9ème Symposium International de l’eau, Cannes, 26-28 juin</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2007</style></year></dates><pub-location><style face="normal" font="default" size="100%"> Cannes</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Marmi Ramdane</style></author><author><style face="normal" font="default" size="100%">BOUMEZBEUR A</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Observations géologiques des glissements de terrain dans le Constantinois : cas du tronçon d&amp;rsquo;autoroute Massinissa, Didouche Mourad et Anouche Ali. (Algérie nord-orientale)</style></title><secondary-title><style face="normal" font="default" size="100%">Séminaire International sur les Géosciences au Service du Développement Durable (26, 27 et 28 novembre) Centre Universitaire de Tébessa</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2006</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Marmi Ramdane</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractéristiques géologiques, géotechniques et hydrologiques d&amp;rsquo;un site destiné à l&amp;rsquo;aménagement d&amp;rsquo;un ouvrage hydraulique (Aurès, Algérie Nord-Orientale)</style></title><secondary-title><style face="normal" font="default" size="100%">Third International Conference on water Resources in Mediterranean Basin. 1-3 November Watmed 3 Tripoli- Lebanon</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2006</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Marmi Ramdane</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractéristiques géologiques, géotechniques et hydrologiques d&amp;rsquo;un site destiné à l&amp;rsquo;aménagement d&amp;rsquo;un ouvrage hydraulique (Aurès, Algérie Nord-Orientale) </style></title><secondary-title><style face="normal" font="default" size="100%">Séminaire International sur les Géosciences au Service du Développement Durable. 26-27 et 28 Novembre Centre Uni de Tébessa / Institut des Sciences de la Terre</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2006</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Bouchene. N</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Influence des conditions géologiques sur la stabilité du barrage de Hammam Grouz, Oued El Athemania. Constantine.</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2006</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Hoggas D</style></author><author><style face="normal" font="default" size="100%">Nabti H</style></author><author><style face="normal" font="default" size="100%">Yahiaoui K</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Num:13-, , (2006): Contribution à l&amp;#39;étude de la stabilité de la digue du barrage Saf-Saf Ouesra Tebessa.Département des scs de la terre, Univ- Batna.</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2006</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Hamel Ahmed</style></author><author><style face="normal" font="default" size="100%">Nezli IE</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation de la qualité chimique des eaux souterraines de l&amp;#39;oued Abiod</style></title><secondary-title><style face="normal" font="default" size="100%">journées d'étude internationales sur &quot;la désertification et le développement durable&quot;. CRSTRA et université de Biskra</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2006</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author><author><style face="normal" font="default" size="100%">Djabri Larbi</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Aspects Géochimiques de la Salinité des Eaux du Mio-Plio-Quaternaire et Equilibres Entre Minéraux et Solutions dans la Plaine d&amp;#39;El-Outaya . ALGERIE</style></title><secondary-title><style face="normal" font="default" size="100%">Watmed 3. Tripoli. Liban</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2006</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Hamel Ahmed</style></author><author><style face="normal" font="default" size="100%">Nezli IE</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude des types chimiques des eaux exploitées dans les Aurès (cas de la vallée de l&amp;rsquo;oued Abiod)</style></title><secondary-title><style face="normal" font="default" size="100%">Seminaire international sur les géosciences au service du développement durable 26,27 et 28 Nov Tebessa</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2006</style></year></dates><pub-location><style face="normal" font="default" size="100%">Tebessa, Alger</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Using numerical indexes for mapping the groundwater pollution potential</style></title><secondary-title><style face="normal" font="default" size="100%">Communication orale, 8ème  Symposium International de l’eau, Cannes, 26-30  juin</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2006</style></year></dates><pub-location><style face="normal" font="default" size="100%">Cannes</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Djabri Larbi</style></author><author><style face="normal" font="default" size="100%">Kardache Ramdane</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">La salinité des eaux souterraines de la plaine d&amp;rsquo;El-Outaya (Biskra, Algérie). Biskra, année 2006.</style></title><secondary-title><style face="normal" font="default" size="100%">Journal Algérien des Régions Arides</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2006</style></year></dates><pages><style face="normal" font="default" size="100%">pp 261-265</style></pages><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Marmi Ramdane</style></author><author><style face="normal" font="default" size="100%">BOUMEZBEUR A</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Faisabilité géologique de la retenue collinaire de Foum toub </style></title><secondary-title><style face="normal" font="default" size="100%">1erseminaire national sur la mobilisation et l'exploitation des ressources en eau.Dpt d'Hydraulique en collaboration avec le laboratoire de recherche en Hydraulique appliquée. Univ.Batna</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2005</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">BOUMEZBEUR A</style></author><author><style face="normal" font="default" size="100%">Marmi Ramdane</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">L&amp;rsquo;apport géotechnique à l&amp;rsquo;étude du phénomène du mouvement du sol : retrait gonflement</style></title><secondary-title><style face="normal" font="default" size="100%">Communication au 1er Séminaire sur L'apport de la géotechnique face aux risques naturels. 08/09 Novembre Laboratoire National de l'Habitat et de la Construction/ Batna</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2005</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">BOUMEZBEUR A</style></author><author><style face="normal" font="default" size="100%">Marmi Ramdane</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Faisabilité de la retenue collinaire de Foum Toub : Etude géologique et géotechnique (Aurès, Batna)</style></title><secondary-title><style face="normal" font="default" size="100%">Communication au Premier séminaire national sur la mobilisation et l’exploitation des ressources en eau. 12-13 Décembre Lab. LARHYA / Uni. De Batna</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2005</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Cheriet Manel</style></author><author><style face="normal" font="default" size="100%">Benzagouta Mohamed Said</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation lithologique à base de mesures de K: représentation graphique (Cas du site de Beni Haroun)</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2005</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author><author><style face="normal" font="default" size="100%">Djabri Larbi</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Influence des roches evaporitiques sur la dégradation des eaux souterraines de la plaine d&amp;rsquo;el-outaya </style></title><secondary-title><style face="normal" font="default" size="100%">1er séminaire national sur la mobilisation et l'exploitation des ressources en eau. Dpt d'Hydraulique en collaboration avec le laboratoire de recherche en Hydraulique appliquée. Univ.Batna</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2005</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Marmi Ramdane</style></author><author><style face="normal" font="default" size="100%">BOUMEZBEUR A</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Faisabilité géologique de la retenue collinaire de Foum toub </style></title><secondary-title><style face="normal" font="default" size="100%">1erseminaire national sur la mobilisation et l'exploitation des ressources en eau.Dpt d'Hydraulique en collaboration avec le laboratoire de recherche en Hydraulique appliquée. Univ.Batna</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2005</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Nezli IE</style></author><author><style face="normal" font="default" size="100%">Achour S</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Mécanismes d&amp;#39;acquisition de la salinité des eaux de la nappe phréatique de la basse Vallée de l&amp;rsquo;Oued Mya (Ouargla) </style></title><secondary-title><style face="normal" font="default" size="100%">1er seminaire national sur la mobilisation et l'exploitation des ressources en eau.Dpt d'Hydraulique en collaboration avec le laboratoire de recherche en Hydraulique appliquée. Univ.Batna</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2005</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">BOUMEZBEUR A</style></author><author><style face="normal" font="default" size="100%">Marmi Ramdane</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Faisabilité de la retenue collinaire de Foum Toub : Etude géologique et géotechnique (Aurès, Batna)</style></title><secondary-title><style face="normal" font="default" size="100%">Communication au Premier séminaire national sur la mobilisation et l’exploitation des ressources en eau. 12-13 Décembre 2005. Lab. LARHYA / Uni. De Batna</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2005</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Djenba Samir</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Fluctuation piézométrique interannuelle de la nappe superficielle de Beida bordj (W.Sétif) </style></title><secondary-title><style face="normal" font="default" size="100%">premier séminaire national sur la mobilisation et l’exploitation des ressources en eau Batna les 12-13 décembre </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2005</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Marmi Ramdane</style></author><author><style face="normal" font="default" size="100%">Guiraud R</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Tectonique compressive polyphasée dans la chaîne alpine en Algérie : l&amp;rsquo;exemple du Môle Constantinois et de son avant-pays</style></title><secondary-title><style face="normal" font="default" size="100%">2° Séminaire international sur la Géologie du Grand Constantinois et des Confins algéro-tunisiens SGGC-2, Université de Constantine, 9-11 mai</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2005</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Marmi Ramdane</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à l&amp;rsquo;étude pétro-structurale du secteur Bouchtata-Tamalous situé dans la bordure orientale du socle de la Petite Kabylie</style></title><secondary-title><style face="normal" font="default" size="100%">Séminaire International &quot;la Géologie du  Grand Constantinois  et des Confins Algéro-Tunisiens&quot;. 09-10 et -11 Mai Dépt Sc Terre/ Uni de Constantine/Laboratoire de Géologie et Environnement/Sonatrach</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2005</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">BOUMEZBEUR A</style></author><author><style face="normal" font="default" size="100%">Marmi Ramdane</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Risque naturels liée au phénomène retrait-gonflement des sols &amp;laquo; Cas de Djerma-Batna &amp;raquo;</style></title><secondary-title><style face="normal" font="default" size="100%">Séminaire international sur les Risques Naturels liés aux glissements de terrains et d'éboulement rocheux. 15-16 Novembre Université de 08 Mai 45 Guelma / Laboratoire Génie Civil et Habitat</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2005</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Meziani A</style></author><author><style face="normal" font="default" size="100%">Soltani  H</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à l&amp;#39;étude géotechnique d&amp;#39;un barrage en terre &amp;quot;Fontaine des gazelles sur oued El-Hai wilaya de Biskra. Département sciences de la terre, Univ. de Batna.</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2005</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude de la pollution d&amp;rsquo;une nappe Périurbaine, cas de la plaine d&amp;rsquo;El Madher (Nord-Est Algérie)</style></title><secondary-title><style face="normal" font="default" size="100%">Communication orale, 7ème  Symposium International de l’eau, Cannes, 27 juin-02 juillet </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2005</style></year></dates><pub-location><style face="normal" font="default" size="100%">Cannes</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Marmi Ramdane</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude des paléo-courants dans les formations du barrémien et du miocène : Nouvelle hypothèse sur les apports détritiques miocènes dans l&amp;rsquo;Aurès Nord</style></title><secondary-title><style face="normal" font="default" size="100%">Communication au 1er Séminaire National des Sciences de la Terre au Service du Développement durable. Université Cheikh Larbi Tebessi/ Tébessa 26/27 Avril</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2004</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Yahiaoui K</style></author><author><style face="normal" font="default" size="100%">Inal Ahmed</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Paléo-environnement des calcaires à Rudistes d&amp;rsquo;âge Coniacien inférieur (Berriche) des Monts de Belezma (Algérie orientale)</style></title><secondary-title><style face="normal" font="default" size="100%">Communication au 1er Séminaire National des Sciences de la Terre au Service du Développement durable. Université Cheikh Larbi Tebessi/ Tébessa 26/27 Avril</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2004</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Djabri Larbi</style></author><author><style face="normal" font="default" size="100%">Kardache Ramdane</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Salinité des eaux souterraines de la région Est de la plaine d&amp;#39;El-Outaya</style></title><secondary-title><style face="normal" font="default" size="100%"> Colloque international, terre, eau Annaba du 04 au 06 décembre. Dpt des sciences de la terre. Univ de Annaba</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2004</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">BENNEDJAI N</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Approche statistique de l&amp;rsquo;Influence des caractéristiques physiques des bassins versants sur les écoulements aux exutoires</style></title><secondary-title><style face="normal" font="default" size="100%">Communication orale, Journées d’2tudes sur les Risques Naturels : Inondations, Prévision, Protection. Batna, Algérie, 15-16 Décembre</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2004</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Djabri Larbi</style></author><author><style face="normal" font="default" size="100%">Kardache Ramdane</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Salinité des eaux souterraines de la région Est de la plaine d&amp;#39;El-Outaya</style></title><secondary-title><style face="normal" font="default" size="100%">Colloque international, terre, eau Annaba du 04 au 06 décembre. Dpt des sciences de la terre. Univ de Annaba</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2004</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Nezli IE</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Labar S</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Origines de la salinité des eaux de la nappe phréatique de la basse Vallée de l&amp;rsquo;Oued Mya (Ouargla)</style></title><secondary-title><style face="normal" font="default" size="100%">Journées scientifiques algéro-francaises (colloque de Ouargla JSAF2004). Univ de Ouargla</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2004</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">Zouita N</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude de la pollution de la plaine alluviale de la plaine d&amp;rsquo;El Madher par les rejets de la ville de Batna (Nord-Est Algérie)</style></title><secondary-title><style face="normal" font="default" size="100%">Communication orale, Colloque International Terre et Eau, Annaba, Algérie, 04-06 Décembre</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2004</style></year></dates><pub-location><style face="normal" font="default" size="100%">Annaba, Algérie</style></pub-location><pages><style face="normal" font="default" size="100%">pp372-375</style></pages><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">BENNEDJAI N</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Influence des paramètres physiques sur les débits aux exutoires des bassins versants</style></title><secondary-title><style face="normal" font="default" size="100%">Communication orale, Colloque International Terre et Eau, Annaba, Algérie, 04-06 Décembre</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2004</style></year></dates><pub-location><style face="normal" font="default" size="100%">Annaba, Algérie</style></pub-location><pages><style face="normal" font="default" size="100%">pp 485-488</style></pages><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">La recharge artificielle et la vulnérabilité à la pollution des eaux souterraines : Combinaison des approches pour le choix des sites de recharge</style></title><secondary-title><style face="normal" font="default" size="100%">Communication orale, 6ème Symposium International de l’eau, Cannes, 29 juin-02 juillet</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2004</style></year></dates><pub-location><style face="normal" font="default" size="100%">Cannes</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Djabri Larbi</style></author><author><style face="normal" font="default" size="100%">Kardache Ramdane</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">La qualité chimique des eaux souterraines de la nappe du mio-pliocene d&amp;rsquo;El Outaya ( Biskra )</style></title><secondary-title><style face="normal" font="default" size="100%">Colloque international, eau, oasis, population Biskra du 22 au 24 septembre. Laboratoire LARHYSS . Univ de Biskra </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2003</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Prévention des risques de pollution des eaux souterraines par l&amp;rsquo;évaluation et la cartographie de leur vulnérabilité : Traitement de la méthode DRASTIC sous Matlab</style></title><secondary-title><style face="normal" font="default" size="100%">Communication orale, Colloque Hydrotop, Marseille, France, 22-24 Oct</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2003</style></year></dates><pub-location><style face="normal" font="default" size="100%">Marseille, France</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Approche du bilan hydrodynamique de l&amp;rsquo;aquifère alluvial de la plaine d&amp;rsquo;El Madher (Nord-Est algérien) par une modélisation en régime permanent</style></title><secondary-title><style face="normal" font="default" size="100%">Communication orale, Séminaire International en modélisation numérique en structures et géo matériaux, Batna, Algérie, 22-24 Oct</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2001</style></year></dates><pub-location><style face="normal" font="default" size="100%">Batna, Algérie</style></pub-location><pages><style face="normal" font="default" size="100%">pp 340-353</style></pages><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Evaluation et cartographie de la vulnérabilité à la pollution de l&amp;rsquo;aquifère alluvionnaire de la plaine d&amp;rsquo;El Madher, Nord-Est algérien, selon la méthode DRASTIC, John Libbey Eurotext France.</style></title><secondary-title><style face="normal" font="default" size="100%">Sécheresse</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2001</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.jle.com/fr/revues/sec/e-docs/evaluation_et_cartographie_de_la_vulnerabilite_a_la_pollution_de_l_aquifere_alluvionnaire_de_la_plaine_d_el_madher_nord_est_algerien_selon_la_methode_drastic_230026/article.phtml?cle_doc=0003828A&amp;type=text.html</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Vol.12</style></volume><pages><style face="normal" font="default" size="100%"> pp.95-101</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;div class=&quot;texte&quot;&gt;
	&lt;p&gt;
		La cartographie de la vulnérabilité à la pollution des eaux souterraines permet d'identifier les zones à haut risque de contamination, indépendamment du type de polluant. Elle devrait en principe conditionner les plans d'occupation des sols ou, du moins, permettre de cibler les zones où des mesures rigoureuses de protection devraient être adoptées. La méthode Drastic, qui a été développée en 1987 aux États-Unis par la NWWA (Natural Water Well Association), permet cette approche. C'est une méthode standardisée d'évaluation et de cartographie de la vulnérabilité des eaux souterraines indépendamment du type de polluant et qui prend en compte la majeure partie des facteurs hydrogéologiques qui affectent et contrôlent l'écoulement des eaux souterraines : la profondeur de l'eau, la recharge efficace, les matériaux de l'aquifère, le type de sol, la topographie, l'impact de la zone vadose (zone aérée) et la perméabilité de l'aquifère. Ces facteurs sont représentés par des poids et des cotes qui dépendent respectivement de leur importance relative et des conditions hydrogéologiques locales. La combinaison des poids et cotes des divers paramètres aboutit à une valeur numérique qui est l'indice Drastic. La cartographie de l'indice de vulnérabilité repose sur la superposition de 7 cartes indicielles. Si le mode manuel, long et fastidieux, paraît inadapté pour cette opération, la cartographie automatique par des logiciels qui traitent la variation progressive d'un paramètre ne peut également représenter valablement le phénomène, du fait que l'indice de vulnérabilité est attribuée à la zone elle-même et non pas à son contour. L'utilisation de matrices de calcul dont les éléments représentent le domaine discrétisé permet une cartographie rigoureuse de la vulnérabilité à la pollution. Cet article représente une application de cette méthode à l'aquifère alluvionnaire de la plaine d'El Madher qui est située à environ 15 km au nord-est de la ville de Batna. La cartographie de l'indice Drastic par l'utilisation de matrices sous Matlab a permis de délimiter les zones vulnérables à la pollution.
	&lt;/p&gt;
&lt;/div&gt;
&lt;img src=&quot;https://www.jle.com/_/droit/sec/--/resume/free/230026.png&quot; style=&quot;display:block;&quot; width=&quot;1&quot; height=&quot;0&quot; border=&quot;0&quot;&gt;</style></abstract><issue><style face="normal" font="default" size="100%">n°2</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Mahdjoub Y</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude pétro-structurale de la bordure sud est du socle de la Petite Kabylie &amp;ndash;région de Sidi Mezghiche, Algérie</style></title><secondary-title><style face="normal" font="default" size="100%">Communication au 4eme Séminaire de Géologie Pétrolière/CRD/ Ministère des énergies 13,14 et 15 Novembre Boumerdes</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2000</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation du système aquifère alluvionnaire de la plaine d&amp;#39;El Madher (Nord-Est Algérien) en vue de l&amp;rsquo;expression de son bilan hydrodynamique au moyen d&amp;rsquo;un modèle de simulation en régime permanent.</style></title><secondary-title><style face="normal" font="default" size="100%">Bulletin du Service Géologique de l’Algérie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2000</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.asjp.cerist.dz/en/article/5041</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Vol.11</style></volume><pages><style face="normal" font="default" size="100%">pp. 107-117</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">L objectif de cet article est la caractérisation de l aquifère alluvionnaire de la plaine d’El Madher qui est située à environ 15 Kms au Nord-Est de la ville de Batna et à 450 Kms au SudEst d’Alger, en vue d’exprimer par la suite son bilan hydrodynamique au moyen d’un modèle de simulation des écoulements souterrains en régime permanent. La caractérisation détaillée du système aquifère du point de vue géologique, morphologique, structural et hydrodynamique, a permis de déterminer l’ensemble des conditions aux limites et des conditions internes préconisées pour la mise en oeuvre de la simulation.</style></abstract><issue><style face="normal" font="default" size="100%">n°1</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Simulation en régime permanent des écoulements souterrains de l&amp;rsquo;aquifère alluvionnaire de la plaine d&amp;rsquo;El Madher (Nord-Est Algérien), Rock View Ltd 2000, France.</style></title><secondary-title><style face="normal" font="default" size="100%">Africa Geosciences Review</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2000</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://scholar.google.com/citations?user=GKY-YYAAAAAJ&amp;hl=en&amp;oi=sra</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Vol.7</style></volume><pages><style face="normal" font="default" size="100%">pp. 383-392</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><issue><style face="normal" font="default" size="100%">n° 4</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Djabri Larbi</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Groundwater pollution potential in the valley of the Oued Seybouse, NE Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">Intern. Conf. On Geochemistry, Alex. thCommunication orale, 4Univ., Egypt, 15-16 Sept</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">1999</style></year></dates><pub-location><style face="normal" font="default" size="100%"> Egypt</style></pub-location><pages><style face="normal" font="default" size="100%">pp 389-400</style></pages><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author><author><style face="normal" font="default" size="100%">El Dounia A</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Identification des aquifères profonds par la prospection electrique. Application à l&amp;rsquo;Est Algérien</style></title><secondary-title><style face="normal" font="default" size="100%">Communication orale 2ème Colloque International sur l’Eau et l’Environnement, Agadir, Maroc, 25-27 fev</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">1999</style></year></dates><pub-location><style face="normal" font="default" size="100%"> Agadir, Maroc</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">Djabri Larbi</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Using matrices for mapping the groundwater pollution potential. Case of the DRASTIC method applied to the El Madher plain (North East of Algeria)</style></title><secondary-title><style face="normal" font="default" size="100%">Communication orale, 4th Intern. Conf. On Geochemistry, Alex. Univ., Egypt, 15-16 Sept</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">1999</style></year></dates><pub-location><style face="normal" font="default" size="100%"> Alex. Univ., Egypt</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Evaluation et cartographie de la vulnérabilité à la pollution des eaux souterraines selon la méthode DRASTIC. Cas de la plaine d&amp;rsquo;El Madher (Nord-Est Algérien)</style></title><secondary-title><style face="normal" font="default" size="100%">Communication orale 2ème Colloque International sur l’Eau et l’Environnement, Agadir, Maroc, 25-27 fev</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">1999</style></year></dates><pub-location><style face="normal" font="default" size="100%">Agadir, Maroc</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Cartographie de la vulnérabilité à la pollution des eaux souterraines selon la méthode DRASTIC. Cas de la plaine d&amp;rsquo;El Madher (Nord-Est Algérien), Janvier 1999, Alger.</style></title><secondary-title><style face="normal" font="default" size="100%">Bulletin International de l’Eau et de l’Environnement - EDIL Infeau</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">1999</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language><issue><style face="normal" font="default" size="100%"> n° 21</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">La cartographie de la vulnérabilité des eaux souterraines : Outil de gestion et d&amp;rsquo;aménagement des bassins versants</style></title><secondary-title><style face="normal" font="default" size="100%">Communication Séminaire Scientifique et Technique sur les Bassins Versants, Batna 03-04 Décembre</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">1998</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Modélisation en régime permanent des écoulements souterrains de l&amp;#39;aquifère alluvionnaire de la plaine d&amp;#39;El Madher (Nord-Est algérien).</style></title><secondary-title><style face="normal" font="default" size="100%">Bulletin du Service Géologique de l’Algérie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">1998</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.asjp.cerist.dz/en/article/9101</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Vol.9</style></volume><pages><style face="normal" font="default" size="100%">pp. 201-213</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">La plaine d El Madher est un bassin sédimentaire à remplissage alluvionnaire mio-plioquaternaire qui est le siège d un écoulement souterrain. Elle est située à environ 15 Kms au NordEst de la ville de Batna dont elle constitue un des champs de captage. La caractérisation de cet aquifère a permis notamment de déterminer les conditions aux limites du système et les conditions internes (zones de transmissivités et prélèvements) . Après un test de cohérence concluant sur cette base de données , la modélisation des écoulements souterrains en régime permanent par la méthode des différences finies a permis d aboutir au calage de la piézométrie de référence de la nappe et à l ’approche de l’expression de son bilan hydrodynamique moyen annuel.</style></abstract><issue><style face="normal" font="default" size="100%">n° 2</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Diagnostic et Rénovation des forages</style></title><secondary-title><style face="normal" font="default" size="100%">Séminaire National sur l'Hydraulique, Université de Biskra, Décembre </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">1994</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Piézométrie de la nappe phréatique de la plaine de Ain Touta  (Algérie orientale)</style></title><secondary-title><style face="normal" font="default" size="100%">Communication orale, Séminaire national sur l'Hydraulique et l'environnement, Batna</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">1987</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record></records></xml>