@article {6919,
	title = {Hydrodynamic Characteristics of the \&ldquo;Complex Terminal\&rdquo; aquifer in the Region of Oued Righ North (Algerian Sahara)},
	journal = {Algerian Journal of Environmental Science and Technology},
	year = {In Press},
	abstract = {
	Accessibility of fresh water, the nature{\textquoteright}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. The Oued Righ region is located in Algeria{\textquoteright}s South-East, specifically in the NorthEast 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. It is famous for its date palms, the development of the date culture in this region is attributed not only to the population{\textquoteright}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 results obtained from using different approaches of water hydrodynamics in the Complex Terminal aquifer. The aquifer{\textquoteright}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 showed 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 2.36{\texttimes} 102-m 2 /sis 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.

},
	url = {https://www.aljest.net/index.php/aljest/article/view/521},
	author = {Hammadi, A. and Brinis, Nafaa and Djidel, M}
}
@article {6918,
	title = {Risk assessment ofirrigation with water contaminated by trace metals (Cd, Cr, Pb and Zn) on the soil-plant complex in the ElMadher plain (Batna, north-east Algeria)},
	journal = {Journal of Water and Land Development},
	year = {In Press},
	author = {Benfarhi, F and Menani, Mohamed-Redha}
}
@article {6916,
	title = {Calculation of water needs of the main crops and water resources available in a semi-arid climate, case of Zana-Gada{\"\i}ne plain, Northeastern Algeria},
	journal = {Algerian Journal of Environmental Science and Technology ALJEST},
	volume = {8},
	number = {2},
	year = {2022},
	abstract = {
	The relative scarcity of water resources in Algeria and their unequal distribution induce a rational use of available resources. The Zana-Gada{\"\i}ne 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-Gada{\"\i}ne 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.

},
	url = {https://www.aljest.net/index.php/aljest/article/view/570},
	author = {H. Belalite, and M.R. Menani, and A. Athamena}
}
@article {6924,
	title = {Using vadose-zone water stable isotope profiles for assessing groundwater recharge under different climatic conditions},
	journal = {Hydrological Sciences Journal },
	volume = {66},
	number = {10},
	year = {2021},
	abstract = {
	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 (δ2H and δ18O) that were used along with the piston displacement method to estimate recharge. Annual recharge rates of 0.2\% ({\textpm} 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.

},
	url = {https://www.tandfonline.com/doi/full/10.1080/02626667.2021.1957479},
	author = {Boumaiza, Lamine and Chesnaux, Romain and Drias, Tarek and Walter, Julien and Stumpp, Christine}
}
@article {6923,
	title = {paleoenvironmental study of oum ali region(t{\'e}bessa, algeria) during quaternary, through the study of fluvial terrace of khenigue wadi},
	journal = {ACTA GEOBALCANICA  },
	volume = {7},
	number = {4},
	year = {2021},
	pages = {151-157},
	abstract = {
	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

},
	url = {https://www.geobalcanica.org/wp-content/uploads/AGB/2021/AGB-2021-7-21.pdf},
	author = {DEFAFLIA , Nabil and Fouad Djaiz and Fehdi, Chamseddine}
}
@article {6922,
	title = {Characterization of Cenomanian-Turonian oxic facies in Tunisia: sequence stratigraphy and correlation of recorded bioevents},
	journal = {Arabian Journal of Geosciences},
	volume = {14},
	year = {2021},
	abstract = {
	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\&nbsp;Whiteinella archaeocretacea\&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\&nbsp;Rotalipora\&nbsp;(or\&nbsp;Thomasinella), the\&nbsp;Heterohelix\&nbsp;shift, the\&nbsp;Whiteinella\&nbsp;proliferation, the filament event, and the appearance of\&nbsp;Helvetotruncana helvetica. Among these bioevents, the\&nbsp;Heterohelix\&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.

},
	author = {Hanini, Amine and Houla, Yassine and DJAIZ, Foued and Chairat, Imen and Mabrouk Boughdiri and Maamri, Ridha and Zagrarni,Mohamed-Faouzi}
}
@article {6921,
	title = {THE VERTICAL DISTRIBUTION OF THE ALLUVIAL CHEMO-FACIES OF BOUMERZOUG WADI, CONSTANTINE, NORTHEASTERN ALGERIA: PALEOENVEROMENTAL SIGNIFICANCE AND CLIMATE EVOLUTION},
	journal = {Analele Universit{\u a}{\c t}ii din Oradea, Seria Geografie},
	volume = {31},
	number = {1},
	year = {2021},
	pages = {68-79},
	abstract = {
	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.

},
	url = {https://d1wqtxts1xzle7.cloudfront.net/84550251/auog.311108-865-libre.pdf?1650469151=\&response-content-disposition=inline\%3B+filename\%3DThe_Vertical_Distribution_of_the_Alluvia.pdf\&Expires=1663166053\&Signature=GgE6IslXDLa0uV9lBn--z69CxZVgU3Cu8BAoi2RqaTXm9w},
	author = {RABAHI, Noureddine and DJAIZ, Foued and DEFAFLIA , Nabil and GUASTALDI, Enrico and AMROUNE, Abdelouahab}
}
@article {6917,
	title = {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)},
	journal = {Italian Journal of Groundwater ACQUE SOTTERRANEE},
	volume = {10},
	number = {3},
	year = {2021},
	abstract = {
	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.

},
	url = {https://www.acquesotterranee.net/index.php/acque/article/view/511},
	author = {Harizi, Khaled and Mohamed Redha Menani and Chabour, Nabil and Labar, Sofiane}
}
@article {6926,
	title = {Groundwater modelling of the Tebessa-Morsott alluvial aquifer (northeastern Algeria): A geostatistical approach},
	journal = {Groundwater for Sustainable Development },
	volume = {11},
	year = {2020},
	abstract = {This paper studies aquifer{\textquoteright}s hydrodynamic behavior by combining a flow-simulation model with\&nbsp;transmissivity\&nbsp;optimization (cokriging) in order to provide an optimal management scheme for the groundwater aquifer. The use of a cokriging approach improves the\&nbsp;transmissivity\&nbsp;data which are insufficient for the database of the\&nbsp;groundwater flow\&nbsp;simulation model. The obtained results are then used to model the\&nbsp;groundwater flow\&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\&nbsp;leakage\&nbsp;rate are similar compared to those calculated by the analytical approach, (84,354\&nbsp;m3/day for the recharge and 36,986\&nbsp;m3/day for pumped water flow rate). The results of the transient regime show the alluvial aquifer affected by large drawdowns reaching 40\&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.},
	url = {https://www.sciencedirect.com/science/article/abs/pii/S2352801X1930311X},
	author = {Drias, Tarek and Abdelhamid Khedidja and Moufida Belloula and Badraddine, Saadali and Saibi, Khedoudj}
}
@article {6925,
	title = {Identifying groundwater degradation sources in a Mediterranean coastal area experiencing significant multi-origin stresses},
	journal = {Science of The Total Environment },
	volume = {746},
	year = {2020},
	abstract = {
	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\&nbsp;stable isotopes\&nbsp;δ2H-H2O and δ18O-H2O, and stable isotopes of nitrate δ15N-NO3\&nbsp;and δ18O-NO3, and then integrated into the history of land use over the study area. Groundwater nitrate concentrations ranging from 1.6 to 235\&nbsp;mg/L with a median value of 69\&nbsp;mg/L are evidence of the degradation of groundwater quality induced by\&nbsp;anthropogenic sources. The combined of δ15N-NO3\&nbsp;and δ18O-NO3\&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\&nbsp;saltwater intrusion\&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 δ2H-H2O and δ18O-H2O 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\&nbsp;cumulative effect\&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.

},
	url = {https://www.sciencedirect.com/science/article/abs/pii/S004896972034732X},
	author = {Boumaiza, Lamine and Chesnaux, Romain and Drias, Tarek and Walter, Julien and Huneau, Fr{\'e}d{\'e}ric and Garel, Emilie and Knoeller, Kay and Stumpp, Christine}
}
@article {6920,
	title = {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)},
	journal = {Journal of Fundamental and Applied Sciences},
	year = {2019},
	abstract = {
	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.

},
	url = {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},
	author = {Boudjema,  Abderrezak and Guettaia, Sabrine and Brinis, Nafaa}
}
@mastersthesis {5706,
	title = {Contribution {\`a} l\&$\#$39;{\'e}tude g{\'e}otechnique du viaduc de la penetrante Bir chouhada-Batnap{\'e}n{\'e}trante Bir-Echouhada - Batna},
	year = {2019},
	author = {Kehiha Haifa and Khetta Makhloufa}
}
@mastersthesis {5704,
	title = {Contribution {\`a} l\&$\#$39;{\'e}tude g{\'e}otechnique de la p{\'e}n{\'e}trante  autoriti{\`e}re. Tran{\c c}on Eleulma Djemila},
	year = {2019},
	author = {Zekiri Ahmed}
}
@mastersthesis {5701,
	title = {Cartographie de vuln{\'e}rabilit{\'e} de l\&$\#$39;aquif{\`e}re superficiel de Biska},
	year = {2019},
	author = {Basli Aleddine and Aksa Nasreddine}
}
@mastersthesis {5700,
	title = {Suivi pi{\'e}zom{\'e}trique et hydrochique de l\&$\#$39;aquif{\`e}re alluvionnaire de Ain Djasser},
	year = {2019},
	author = {Mekhloufi Nadjet and Bastal Dhaouia}
}
@mastersthesis {5699,
	title = {Le Turonien de Dj Boukezzez (ChaabetOuledChelih) : Caract{\'e}risation lithobiostratigraphique et interpr{\'e}tation pal{\'e}oenvironnementale.},
	year = {2019},
	author = {Aichaoui Billal and Abid Belgacem}
}
@mastersthesis {5695,
	title = {Coupe de Dj BouArif : Etude lithostratigraphique, s{\'e}dimentologique et r{\'e}flexions pal{\'e}oenvironnementales {\`a} partir de l\&rsquo;{\'e}tude de la faune et de la microfaune (Aur{\`e}s, Batna).},
	year = {2019},
	author = {Bessariani tahar and Guettaoui Imed}
}
@mastersthesis {5693,
	title = {Mise en Evidence de l\&$\#$39;{\'e}v{\`e}nement anoxique oc{\'e}anique 2 (EAO-2) dans la r{\'e}gion de Batna (NE, Alg{\'e}rie)},
	year = {2019},
	abstract = {
	R{\'e}sum{\'e}R{\'e}sum{\'e}:La pr{\'e}sente {\'e}tude s{\textquoteright}int{\'e}resse aux d{\'e}p{\^o}ts c{\'e}nomano-turoniens, observables dans la r{\'e}gion de Batna,afin de d{\'e}finir la mise en {\'e}vidence de l{\textquoteright}{\'e}v{\`e}nement anoxique oc{\'e}anique 2 (EAO-2). Cette r{\'e}gion couvre deux domaines pal{\'e}og{\'e}ographiques et structuraux : le pr{\'e}atlasique(Monts de Bellezma-Batna) au NOet l{\textquoteright}atlasique (Monts de l{\textquoteright}Aur{\`e}s) au SE. Pour le faire,une analyse s{\'e}dimentologique, biostratigraphique et g{\'e}ochimique est r{\'e}alis{\'e}e sur deux coupes Th{\'e}ni{\`e}t El Manchar et Firmet Riche {\guillemotleft}Dj Bou Arif{\guillemotright}. Bas{\'e}es sur les ammonites et les foraminif{\`e}res planctoniques, deux formations ont {\'e}t{\'e} d{\'e}finies: (1) la Formation des Marnes de Smail, subdivis{\'e}e en quatre unit{\'e}s litho-stratigraphiques (IA, IB, IC, ID), dat{\'e}e du C{\'e}nomanien et (2) la base de la Formation des Dolomies de l{\textquoteright}Oued Skhoun (unit{\'e}, IIA) dat{\'e}e du Turonien inf{\'e}rieur. L{\textquoteright}analyse qualitative et quantitative des foraminif{\`e}res (planctoniques et/ou benthiques), des ostracodes, l{\textquoteright}{\'e}tude du microfaci{\`e}s et des marqueurs g{\'e}ochimiques, permet de reconstituer l{\textquoteright}{\'e}volution du pal{\'e}o-environnement et les variations pal{\'e}o-bathym{\'e}triques au cours de l{\textquoteright}intervalle stratigraphique concern{\'e}. Ainsi, les unit{\'e}s IA-IB-IC et la partie inf{\'e}rieure de l{\textquoteright}unit{\'e} ID (C{\'e}nomanien) sont domin{\'e}es par des associations de fora-minif{\`e}res benthiques agglutin{\'e}s et des carapaces enti{\`e}res d{\textquoteright}ostracodes, t{\'e}moignant d{\textquoteright}un milieu de plate-forme et d{\textquoteright}un faible hydrodynamisme. Les calcaires sup{\'e}rieurs de l{\textquoteright}unit{\'e} IC et inf{\'e}rieurs de l{\textquoteright}unit{\'e} ID sont marqu{\'e}s par la pr{\'e}sence de rudistes traduisant une reductiondu milieu de s{\'e}dimentation et une augmentation de l{\textquoteright}hydrodynamisme. Dans ces d{\'e}p{\^o}ts, les associations montrent une diversit{\'e} sp{\'e}cifique faible {\`a} moyenne et une abondance plus ou moins {\'e}lev{\'e}e de foraminif{\`e}res benthiques, t{\'e}moignant de conditions trophiques et d{\textquoteright}oxyg{\'e}nation consid{\'e}r{\'e}es comme normales. Les termes sommitaux de l{\textquoteright}unit{\'e} ID (sommet du C{\'e}nomanien)et l{\textquoteright}unit{\'e} IIA (base du Turonien) marquent, quant {\`a} eux, une {\'e}volution vers des conditions plus profondes, comme le montre la succession standard des {\'e}v{\'e}nements d{\'e}j{\`a} reconnus en Afrique du nord, {\`a} savoir : l{\textquoteright}abondance de foraminif{\`e}res planctoniques, la pr{\'e}sence de {\textquoteleft}filaments{\textquoteright} et une r{\'e}duction drastique de la faune d{\textquoteright}ostracodes. D{\textquoteright}une mani{\`e}re g{\'e}n{\'e}rale, la s{\'e}dimentation des deux formations dans les deux domaines repr{\'e}sente une s{\'e}quence qui {\'e}volue d{\textquoteright}un environnement de plate-forme externe distale {\`a} celui d{\textquoteright}une plate-forme moyenne, avec une phase r{\'e}gressive. Cette s{\'e}quence s{\textquoteright}ach{\`e}ve avec le retour aux conditions profondes concomitantes d{\textquoteright}une hausse eustatique et d{\'e}p{\^o}t de s{\'e}diments p{\'e}lagiques caract{\'e}risant un intervalle transgressif (IT) et s{\textquoteright}inscrit dans le cycle eustatique majeur t{\'e}thysien de troisi{\`e}me ordre. L{\textquoteright}{\'e}volution s{\'e}quentielle et pal{\'e}og{\'e}ographique des d{\'e}p{\^o}ts c{\'e}nomaniens et turoniens inf{\'e}rieurs de la r{\'e}gion de Batna d{\'e}pendent intimement du contexte structural de la r{\'e}gion.En outre, les courbes isotopiques du, carbone (Δ13C) et de l{\textquoteright}oxyg{\`e}ne (Δ18O) des carbonates mettent en {\'e}vidence des anomalies isotopiques relatives aux modifications pal{\'e}o-environnementales. Les donn{\'e}es du Δ13C et celles du COT indiquent une productivit{\'e} primaire faible. Les donn{\'e}es duΔ18O, quant {\`a} elles, indiquent une augmentation des pal{\'e}o-temp{\'e}ratures, cause principale du d{\'e}clenchement de l{\textquoteright}EAO 2. Ces interpr{\'e}tations pal{\'e}o-environnementales s{\textquoteright}accordent avec les donn{\'e}es connues du contexte pal{\'e}og{\'e}ographique r{\'e}gional et mettent en exergue les sp{\'e}cificit{\'e}s t{\'e}thysiennes. 

},
	url = {https://biblio.univ-annaba.dz/wp-content/uploads/2019/11/These-Slami-Rafika.pdf},
	author = {Slami Rafika}
}
@mastersthesis {5684,
	title = {Evaluation du transport solide au niveau du bassin versant d\&$\#$39;Oued Bounamoussa et ses incidences sur l\&$\#$39;envasement du barrage de Chefia},
	year = {2019},
	author = {Bouhadeb Chamsseddine}
}
@proceedings {4898,
	title = {Caracterisation hydrochimiques des eaux du continental intercalaire et complexe terminal et les probl{\`e}mes d\&rsquo;irrigation{\`a} la vall{\'e}e d\&rsquo;oued Righ  },
	journal = {Second International Symposium Water Resources and Environmental Impact Assessment  in North Africa (WREIANA 2019) March 25 -27 , 2019-Sousse, Tunisia},
	year = {2019},
	author = {Djenba Samir}
}
@proceedings {4897,
	title = {Impact de la pollution agricole sur la qualit{\'e} des eaux de l\&$\#$39;aquif{\`e}re de Teleghma},
	journal = {Second International Symposium Water Resources and Environmental Impact Assessment  in North Africa (WREIANA 2019) March 25 -27 , 2019-Sousse, Tunisia},
	year = {2019},
	author = {Dekakra Mouna and MENANI Mohamed redha and Abdelhamid Khedidja}
}
@proceedings {4896,
	title = {Physicochemical and organic quality assessment of Mexa and Bougous waters and its suitability for agricultural use},
	journal = {Second International Symposium Water Resources and Environmental Impact Assessment  in North Africa (WREIANA 2019) March 25 -27 , 2019-Sousse, Tunisia},
	year = {2019},
	author = {B. Saadali and H. Zerouk and Drias Tarek}
}
@proceedings {4895,
	title = {Assessment of the capacitive function of Shallow aquifer using probabilistic and deterministic approaches (geostatistics - 3D model)},
	journal = {Second International Symposium Water Resources and Environmental Impact Assessment  in North Africa (WREIANA 2019) March 25 -27 , 2019-Sousse, Tunisia},
	year = {2019},
	url = {https://www.wreiana2019.com},
	author = {Drias Tarek and Abdelhamid Khedidja and Belloula Moufida}
}
@proceedings {4894,
	title = {Reviewing the potential anthropogenic sources of groundwater contamination - Case study of the expanding urban area of Taleza in Algeria.},
	journal = {the 72nd Canadian Geotechnical Conference, St-John{\textquoteright}s, (September 29 to October 02, 2019)Newfoundland, Canada},
	year = {2019},
	url = {https://www.iaeg.info {\guilsinglright} Congresses},
	author = {Boumaiza Lamine and Chabour Nabil and Drias Tarek}
}
@proceedings {4893,
	title = {there still a chance to save the groundwater in Taleza aquifer ?},
	journal = {AGC-AMC-AIH - GAC-MAC-IAH Conference | Quebec City},
	year = {2019},
	url = {https://gacmac-quebec2019.ca},
	author = {Boumaiza Lamine and Chabour Nabil and Drias Tarek}
}
@article {4889,
	title = {Quality assessment of shallow groundwater for irrigation purposes in Tadjenanet \&ndash; Chelghoum Laid area (Eastern Algeria) ISSN / e-ISSN 1571-5124 / 1814-2060},
	journal = {International Journal of River Basin Management},
	year = {2019},
	abstract = {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), Ca{\texttwosuperior}$^{+}$, Mg{\texttwosuperior}$^{+}$, Na$^{+}$, K$^{+}$, HCO3$^{-}$, SO4{\texttwosuperior}$^{-}$, Cl$^{-}$ 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{\textquoteright}s ratio (KR). These parameters combined allowed to conclude that the quality of groundwater was roughly suitable for irrigation.},
	url = {https://www.researchgate.net/publication/333708795_Quality_Assessment_of_Shallow_Groundwater_for_irrigation_purposes_in_Tadjenanet_-_Chelghoum_Laid_area_Eastern_Algeria},
	author = {Abdelhamid Khedidja and Boudoukha Abderrahmane}
}
@proceedings {4887,
	title = {Les carbonates marins campano-maastrichtiens dans les gorges d\&$\#$39;El Kantara, Aur{\`e}s occidental, Alg{\'e}rie : control sur la biodiversit{\'e}, les types de microfaci{\`e}s et l\&$\#$39;architecture des d{\'e}p{\^o}ts},
	journal = {Premier Colloque sur la g{\'e}ologie des Bassins S{\'e}dimentaires Maghr{\'e}bins FSTGAT-USTHB 01 au 03-10-2019},
	year = {2019},
	author = {Benmansour Sana}
}
@proceedings {4886,
	title = {Contribution {\`a} l\&$\#$39;{\'e}tude du Cr{\'e}tac{\'e} sup{\'e}rieur- Tertiaire : cas de Dj. Arhane, bassin decGhassira (Aur{\`e}s central, NE Alg{\'e}rien)},
	journal = {Premier Colloque sur la g{\'e}ologie des Bassins S{\'e}dimentaires Maghr{\'e}bins FSTGAT-USTHB 01 au 03-10-2019},
	year = {2019},
	author = {Benmansour Sana}
}
@proceedings {4885,
	title = {Etude lithostratigraphique et analyse s{\'e}quentielle de la r{\'e}gion de Maafa- synclinal de B{\'e}ni Fedhala (Aur{\`e}s, Atlas Saharien Oriental)},
	journal = {Premier Colloque sur la g{\'e}ologie des Bassins S{\'e}dimentaires Maghr{\'e}bins FSTGAT-USTHB 01 au 03-10-2019},
	year = {2019},
	author = {Benmansour Sana}
}
@proceedings {4884,
	title = {Caract{\'e}risation g{\'e}ologique et apport de la g{\'e}ophysique pour la mobilisation des ressources hydriques dans le  bassin de Gadaine (Ain Yagout, Alg{\'e}rie NE)},
	journal = {1st  National Seminar on GeoSciences and Environment SGSE 19 October 23-24, Tamanrasset, },
	year = {2019},
	author = {DJAIZ Fouad and ATHAMENA Ali and Lamouri Bachir and A. Bousahaba and Belalite Halima and Touansa Rachid and Khanfer Soumia and Marred Manal and Chairat Imen}
}
@proceedings {4883,
	title = {Essai de caracterisation lithostratigraphiques et pal{\'e}oenvironnementdes formations Eoc{\`e}ne du bassin de Ghassira : Coupe  du Kef El-Arous (Aur{\`e}s Central, NE Alg{\'e}rien)},
	journal = {1st  National Seminar on GeoSciences and Environment SGSE 19 October 23-24, Tamanrasset},
	year = {2019},
	author = {Marred Manal and DJAIZ Fouad and Boushaba Abdellah and Lamouri Bachir and Kherchouche Adila}
}
@proceedings {4882,
	title = {Contribution {\`a} l\&rsquo;{\'e}tude du basin N{\'e}og{\`e}ne Batna-ain Touta, limite aur{\`e}s-Monts de Belezma},
	journal = {1st  National Seminar on GeoSciences and Environment SGSE 19 October 23-24, Tamanrasset},
	year = {2019},
	author = {Khanfer Soumia and DJAIZ Fouad}
}
@proceedings {4881,
	title = {Reconsideration of the Cenomanian-Turonian stratigraphics units in the Tebessa region (Algero-TunisienConfines): Petroleum implications},
	journal = {1st  National Seminar on GeoSciences and Environment SGSE 19 October 23-24, Tamanrasset},
	year = {2019},
	author = {Chairat Imen and DJAIZ Fouad and Boughdiri Mabrouk}
}
@proceedings {4880,
	title = {Hydrochemical Characteristics under current condition exploitation usingstatistics methods : case of the Zana- Roknia plain, North east of Algeria},
	journal = {1st  National Seminar on GeoSciences and Environment SGSE 19 October 23-24, Tamanrasset},
	year = {2019},
	author = {ATHAMENA Ali and MENNANI Mohamed Redha and DJAIZ Fouad}
}
@proceedings {4879,
	title = {Les terrasses fluviatiles quaternaires de Oued El Gourzi et oued El Hay (Batna, NE Alg{\'e}rie) : S{\'e}dimentologie Caract{\'e}ristiques de l\&rsquo;Environnement},
	journal = {1st  National Seminar on GeoSciences and Environment SGSE 19 October 23-24, Tamanrasset},
	year = {2019},
	author = {DJAIZ Fouad and Lamouri Bachir and Boughdiri Mabrouk and Touansa Rachid and Boushaba Abdellah and Mrred Manel and Khaner Soumia and Chairat Imen}
}
@proceedings {4878,
	title = {Les d{\'e}pots Mioc{\`e}ne de la r{\'e}gion de T{\'e}bessa (Nord-est Alg{\'e}rien) : Analyses s{\'e}dimentologiques, Micropal{\'e}ontologiques et Pal{\'e}oenvironnement },
	journal = {Premier Colloque sur la g{\'e}ologie des Bassins S{\'e}dimentaires Maghr{\'e}bins FSTGAT-USTHB 01 au 03-10-2019},
	year = {2019},
	author = {Defaflia Nabil and A. Benkhedda and DJAIZ Fouad and A. Cerif and M. Djerab-Ruault and L. Gouadia}
}
@proceedings {4877,
	title = {Caract{\'e}risation g{\'e}ologique et apport de la g{\'e}ophysique pour la mobilisation des ressources hydriques dans le bassin d\&rsquo;El Mather.},
	journal = {Premier Colloque sur la g{\'e}ologie des Bassins S{\'e}dimentaires Maghr{\'e}bins FSTGAT-USTHB 01 au 03-10-2019},
	year = {2019},
	author = {Nadji Hocine and DJAIZ Fouad and M. Hmmimed}
}
@proceedings {4876,
	title = {La lithostratigraphie de l\&rsquo;Ammonitico Rosso de Djebel Kasserou (Monts de Batna)},
	journal = {Premier Colloque sur la g{\'e}ologie des Bassins S{\'e}dimentaires Maghr{\'e}bins FSTGAT-USTHB 01 au 03-10-2019},
	year = {2019},
	author = {R. Touansa and DJAIZ Fouad and Boughdiri Mabrouk and I. Cherif}
}
@proceedings {4875,
	title = {Contribution {\`a} l\&rsquo;{\'e}tude du cr{\'e}tac{\'e} sup{\'e}rieur-Tertiaire: Cas de Djebel Arhane, bassin de Ghassira (Aur{\`e}s Central, NE Alg{\'e}rien.},
	journal = {Premier Colloque sur la g{\'e}ologie des Bassins S{\'e}dimentaires Maghr{\'e}bins FSTGAT-USTHB 01 au 03-10-2019},
	year = {2019},
	author = {M. Marred and A. Kherchouche and Benmansour Sana and DJAIZ Fouad}
}
@proceedings {4874,
	title = {Evolution tectono-s{\'e}dimentaire du bassin n{\'e}og{\`e}ne de Batna-Ain Touta, limite Aur{\`e}s-Monts de Belezma},
	journal = {Premier Colloque sur la g{\'e}ologie des Bassins S{\'e}dimentaires Maghr{\'e}bins FSTGAT-USTHB 01 au 03-10-2019},
	year = {2019},
	author = {S. Khanfer and DJAIZ Fouad and Lamouri Bachir}
}
@proceedings {4865,
	title = {The Campanian-Maastrichtian series of Dj. Ga{\^a}ga (Tebessa, NE of Algeria) : quantitative and qualitative analysis and palaeoenvironmental interpretation},
	journal = {7. INTERNANATIONAL EARTH SCIENCE COLLOQUIUM ON THE AEGEAN REGION. Izmir/ Turkiye. 7-11 october 2019},
	year = {2019},
	author = {Benmansour Sana}
}
@proceedings {4864,
	title = {Lithostratigraphical and sedimentological characterization of the Aptian formation on the Northern flank of Dj Bou Arif (NE of Algeria)},
	journal = {7. INTERNANATIONAL EARTH SCIENCE COLLOQUIUM ON THE AEGEAN REGION. Izmir/ Turkiye. 7-11 october 2019},
	year = {2019},
	author = {Benmansour Sana}
}
@article {4863,
	title = {Geological Characterization and contibution of Geophysics to the mobilization of water resources in the Ain Djasser basin (South-S{\'e}tifien, Algeria NE), ISSN 2052-3408},
	journal = {The Euro-arab Organization for Environment and Water  and Desert Researches, International Journal of Environment and Water },
	volume = {Vol. 8},
	number = {Issue3},
	year = {2019},
	pages = {pp. 66-77},
	abstract = {Le bassin d{\textquoteright}Ain Djasser fait partie de l{\textquoteright}ensemble Sud-S{\'e}tifien. Ce dernier est repr{\'e}sent{\'e} par une plaine inter-montagneuse appartenant au bassin des hauts plateaux constantinois. Il est caract{\'e}ris{\'e} par un climat de type m{\'e}diterran{\'e}en. L{\textquoteright}hydrologie tributaire du relief est la cons{\'e}quence directe des eaux de surface et de la fonte des neiges. La synth{\`e}se g{\'e}ologique montre un domaine allochtone r{\'e}sultant d{\textquoteright}une histoire polyphas{\'e}e associant les tectoniques atlasique et alpine. Ce dernier est caract{\'e}ris{\'e} par des s{\'e}ries s{\'e}dimentaires carbonat{\'e}es colmat{\'e} par d{\textquoteright}abondantes formations terrig{\`e}nes. L{\textquoteright}alimentation de l{\textquoteright}eau souterraine des diff{\'e}rentes nappes profondes {\`a} semi-profondes provient essentiellement de l{\textquoteright}infiltration des eaux de pluies. Ce cort{\`e}ge de roche forme une nappe libre et captive, par endroit recoup{\'e}e par des forages {\`a} des profondeurs de 178 {\`a} 330 m, fournissant un d{\'e}bit moyen de 15 l/s. L{\textquoteright}interpr{\'e}tation des coupes g{\'e}o{\'e}lectriques du bassin montrent, (i) des formations alluvionnaires du mio-plio-quaternaire de quelques dizaines de m{\`e}tres qui forment un bon aquif{\`e}re superficiel, (ii) des calcaires fissur{\'e}s du jurassico-cr{\'e}tac{\'e} dont le toit est atteint {\`a} des profondeurs variables est un aquif{\`e}re captif. L{\textquoteright}influence d{\textquoteright}accidents entre les diff{\'e}rents blocs rend possible une {\'e}ventuelle alimentation des aquif{\`e}res entres eux. L{\textquoteright}analyse litho-stratigraphique montre que le substratum et la couverture s{\'e}dimentaire ne pr{\'e}sentent pas de grandes variations lat{\'e}rales. Par contre, nous observons au niveau des sondages une variation dans l{\textquoteright}{\'e}paisseur et la lithologie des couches, essentiellement au niveau de la formation du remplissage mio-plio-quaternaire. L{\textquoteright}objectif de cette {\'e}tude r{\'e}side pour l{\textquoteright}essentiel, dans la mobilisation des ressources en eaux superficielles et souterraine pour leurs exploitations dans les domaines agricoles et l{\textquoteright}{\'e}levage, en vue d{\textquoteright}une utilisation rationnelle et planifi{\'e}e de cet {\'e}l{\'e}ment vital qu{\textquoteright}est l{\textquoteright}eau},
	url = {https://www.researchgate.net/publication/330104660_Caracterisation_geologique_et_apport_de_la_geophysique_pour_la_mobilisation_des_ressources_hydriques_dans_le_bassin_d{\textquoteright}Ain_Djasser_Sud-Setifien_Algerie_NE_Geological_Characterization_and_contribution_o},
	author = {Fouad Djaiz and Defaflia Nabil and ATHAMENA Ali and Bachir Lamouri and Mabrouk Boughdiri and Halima Belalite and Boushaba Abdellah}
}
@proceedings {4859,
	title = {Analyse statistique des param{\`e}tres hydrochimiques du continental intercalaire de la r{\'e}gion de biskra - sud-est alg{\'e}rien},
	journal = {1st national seminar on geosciences and environment SGSE{\textquoteright}19, Tamanrasset, Alg{\'e}rie},
	year = {2019},
	author = {Brinis Nafaa}
}
@proceedings {4858,
	title = {Caract{\'e}risation hydrochimique et aptitude {\`a} l\&$\#$39;irrigation des eaux du (CI) dans la r{\'e}gion de Touggourt -ouargla- Oued Righ au sud alg{\'e}rien},
	journal = {1st national seminar on geosciences and environment SGSE{\textquoteright}19, Tamanrasset, Alg{\'e}rie},
	year = {2019},
	author = {Chafou Nasereddine}
}
@proceedings {4857,
	title = {Analyse statistique des param{\`e}tres hydrochimiques du continental intercalaire de la r{\'e}gion de biskra - sud-est alg{\'e}rien},
	journal = {1st national seminar on geosciences and environment SGSE{\textquoteright}19, Tamanrasset, Alg{\'e}rie},
	year = {2019},
	author = {Chafou Nasereddine}
}
@proceedings {4856,
	title = {Caract{\'e}risation hydrochimique et aptitude {\`a} l\&$\#$39;irrigation des eaux du (CI) dans la r{\'e}gion de Touggourt -ouargla- Oued Righ au sud alg{\'e}rien},
	journal = {1st national seminar on geosciences and environment SGSE{\textquoteright}19, Tamanrasset, Alg{\'e}rie},
	year = {2019},
	author = {Brinis Nafaa}
}
@proceedings {4854,
	title = {Identification des param{\`e}tres responsables de la min{\'e}ralisation des sources d\&$\#$39;eau utilis{\'e}es pour l\&$\#$39;irrigation dans le synclinal de BOUZINA, Nord est alg{\'e}rien},
	journal = {Seminaire international sur l{\textquoteright}hydrog{\'e}ologie et l{\textquoteright}environnement , Ouargla Algerie},
	year = {2019},
	author = {Mekoussi Adel}
}
@proceedings {4853,
	title = {Identification des param{\`e}tres responsables de la min{\'e}ralisation des sources d\&$\#$39;eau utilis{\'e}es pour l\&$\#$39;irrigation dans le synclinal de BOUZINA, Nord est alg{\'e}rien},
	journal = {Seminaire international sur l{\textquoteright}hydrog{\'e}ologie et l{\textquoteright}environnement , Ouargla Algerie},
	year = {2019},
	author = {Brinis Nafaa}
}
@proceedings {4852,
	title = {Identification des aquif{\`e}res par les m{\'e}thodes g{\'e}ophysiques. Cas du syst{\`e}me aquif{\`e}re de hammam bradaa nord-est de guelma. Alg{\'e}rie},
	journal = {Colloque sur le g{\'e}ologie des bassins s{\'e}dimentaires Maghrebins Alger, Alg{\'e}rie},
	year = {2019},
	author = {Brinis Nafaa}
}
@proceedings {4848,
	title = {Caract{\'e}risation de potentialit{\'e} aquif{\`e}re du socle cristallin par les apports de la t{\'e}l{\'e}d{\'e}tection et de SIG (r{\'e}gion de Tamanrasset)},
	journal = {1er S{\'e}minaire National sur les g{\'e}osciences et l{\textquoteright}environnement SGSE{\textquoteright}2019},
	year = {2019},
	author = {Azizi Yacine and MENANI Mohamed redha and Boucenna Fatih and Ag Maatallah Lamine and Bouaam Med Lamine}
}
@proceedings {4847,
	title = {Collapse susceptibility mapping for Karst sinkholes in Cheria area, NE Algeria},
	journal = {1er S{\'e}minaire National sur les g{\'e}osciences et l{\textquoteright}environnement SGSE{\textquoteright}2019},
	year = {2019},
	author = {Azizi Yacine and MENANI Mohamed redha and Boumazbeur Abderrahmane}
}
@proceedings {4832,
	title = {Hydrogeology of montain basin, cas of O. Labiod, North Eastern of Algreia},
	journal = {15 th ICWRE - Antalya, Turkey, 25-28 Oct },
	year = {2019},
	author = {Rihani Abla}
}
@article {3627,
	title = {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 },
	journal = {Journal of Fundamental and Applied Sciences},
	volume = {volume 11},
	number = {issue 2},
	year = {2019},
	pages = {pp.786-803},
	author = {Boudjema A and Guettaia Sabrine and Brinis Nafaa}
}
@article {3612,
	title = {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 },
	journal = {Journal of groundwater science and engineering. },
	volume = {vol 7},
	number = {n{\textdegree}2},
	year = {2019},
	pages = {pp.115-132},
	abstract = {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{\texttimes}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.},
	url = {http://gwse.iheg.org.cn/EN/abstract/abstract367.shtml},
	author = {Belouanas Hamza and MENANI Mohamed redha}
}
@mastersthesis {5698,
	title = {La limite Cr{\'e}tac{\'e}/ Tertiaire dans la r{\'e}gion de Menaa : caract{\'e}risation pal{\'e}ontologique et s{\'e}dimentologique},
	year = {2018},
	author = {Baaguigui  Samra and Rahmoun Aicha}
}
@mastersthesis {5694,
	title = {Le C{\'e}nomanien de Chaabet Ouled Chelih : S{\'e}dimentologie et pal{\'e}oenvironnements (L\&rsquo;ensemble Aur{\`e}s-Bellezma).},
	year = {2018},
	author = {Khouaked Khadidja and Rahmoune Amar}
}
@mastersthesis {5688,
	title = {Contribution {\`a} l\&rsquo;{\'e}tude hydrog{\'e}ologique de la vall{\'e}e de Manaa. W Batna},
	year = {2018},
	author = {Benabbes.L and Beda.S}
}
@mastersthesis {5687,
	title = {Contribution {\`a} l\&rsquo;{\'e}tude hydrog{\'e}ologique de la r{\'e}gion de Djamaa (W) El-Oued},
	year = {2018},
	author = {Labed.E and Harrouz.A}
}
@mastersthesis {5685,
	title = {Contribution {\`a} l\&rsquo;{\'e}tude du dimensionnement des p{\'e}rim{\`e}tres de protection du lac du barrage de fontaine des gazelles (Wilaya de Biskra).},
	year = {2018},
	author = {Reghais.A and Maachi.F}
}
@mastersthesis {5683,
	title = {Etude des sources thermomin{\'e}rales de la r{\'e}gion de S{\'e}tif dans leur contexte structural},
	year = {2018},
	abstract = {Dans ce contexte, la pr{\'e}sente {\'e}tude vient se greffer {\`a} d{\textquoteright}autres travaux de recherche (m{\'e}moires de Magister et th{\`e}ses de Doctorat), et ce pour compl{\'e}ter les travaux entrepris d{\'e}j{\`a} dans ce domaine {\`a} travers les sources thermomin{\'e}rales de la Wilaya de S{\'e}tif. Les premi{\`e}res recherches scientifiques men{\'e}es sur les eaux thermales restent toujours d{\textquoteright}actualit{\'e} et pr{\'e}sentent un int{\'e}r{\^e}t ind{\'e}niable {\`a} plus d{\textquoteright}un titre. En effet ces {\'e}tudes bas{\'e}es sur des apports scientifiques sp{\'e}cialis{\'e}s, ont permis de comprendre le ph{\'e}nom{\`e}ne du thermalisme (qui a {\'e}t{\'e} jusqu{\textquoteright}a un pass{\'e} r{\'e}cent consid{\'e}r{\'e} par la population comme ph{\'e}nom{\`e}ne surnaturel) et de d{\'e}finir l{\textquoteright}origine des eaux dites thermales ainsi que leurs zones d{\textquoteright}alimentation et leurs processus d{\textquoteright}acquisition de la temp{\'e}rature et de la min{\'e}ralit{\'e}. A signaler que la r{\'e}gion d{\textquoteright}{\'e}tude a fait l{\textquoteright}objet d{\textquoteright}{\'e}tudes g{\'e}ologiques par J.M Vila (1980) dans sa th{\`e}se de doctorat d{\textquoteright}{\'e}tat {\textquotedblleft}La chaine alpine d{\textquoteright}Alg{\'e}rie orientale et les confins alg{\'e}ro-tunisiens{\textquotedblright}, o{\`u} il a attribu{\'e} le caract{\`e}re d{\textquoteright}allochtonie. Nous avons pens{\'e} alors qu{\textquoteright}une {\'e}tude des sources thermales de la r{\'e}gion de S{\'e}tif pourra {\'e}tayer les r{\'e}sultats de la g{\'e}ophysique et infirmer ou confirmer le caract{\`e}re d{\textquoteright}allochtonie attribu{\'e} {\`a} cet ensemble. A partir de cela, nous allons essayer de mieux comprendre l{\textquoteright}origine des eaux dites thermomin{\'e}rales (Froides et chaudes) ainsi que leurs zones d{\textquoteright}alimentation et leurs processus d{\textquoteright}acquisition de la temp{\'e}rature et de la min{\'e}ralit{\'e} et d{\textquoteright}optimiser l{\textquoteright}interpr{\'e}tation des analyses physico-chimiques en utilisant des moyens d{\textquoteright}investigation appropri{\'e}s. Le programme d{\textquoteright}action pour la r{\'e}alisation de ce travail doit r{\'e}pondre aux pr{\'e}occupations suivantes : -Quel est l{\textquoteright}{\'e}tat actuel de la qualit{\'e} chimique des eaux souterraines de la r{\'e}gion {\'e}tudi{\'e}e -Quels sont les m{\'e}canismes physico-chimiques r{\'e}gissant l{\textquoteright}{\'e}volution des {\'e}l{\'e}ments chimiques dans le temps et dans l{\textquoteright}espace (processus d{\textquoteright}acquisition de la temp{\'e}rature et de la min{\'e}ralit{\'e})? -Quels sont les processus d{\textquoteright}acquisition des temp{\'e}ratures en profondeur des diff{\'e}rents points d{\textquoteright}eau chaude en utilisant des g{\'e}othermom{\`e}tres chimiques, comme indicateurs de la thermalit{\'e} des gisements d{\textquoteright}eaux. Afin de r{\'e}pondre {\`a} ces pr{\'e}occupations, nous allons adopter la m{\'e}thodologie suivante : -Etude du cadre naturel et hydrodynamique en relation avec le chimisme du milieu -Etude des param{\`e}tres physiques et chimiques de l{\textquoteright}eau. -Etude des d{\'e}pendances et relations entre les divers param{\`e}tres physico-chimiques de l{\textquoteright}eau. -Etude des m{\'e}canismes d{\textquoteright}acquisition de la temp{\'e}rature et de la min{\'e}ralisation des eaux thermales et leurs origines. Pour concr{\'e}tiser ce programme de travail, un suivi saisonnier des mesures physicochimiques sera effectu{\'e} sur le terrain ainsi que des pr{\'e}l{\`e}vements d{\textquoteright}{\'e}chantillons d{\textquoteright}eaux destin{\'e}s aux analyses chimiques en {\'e}l{\'e}ments majeurs, mineurs. L{\textquoteright}analyse des r{\'e}sultats ainsi obtenus sera d{\'e}velopp{\'e}e {\`a} travers les deux parties constituant cette th{\`e}se. Premi{\`e}re partie CHAPITRE I : Synth{\`e}se g{\'e}ologique de l{\textquoteright}aire d{\textquoteright}{\'e}tude Elle reste d{\textquoteright}une grande importance, dans le domaine du thermalisme nous d{\'e}crirons les limites g{\'e}ographiques de la r{\'e}gion de S{\'e}tif et nous examinerons ensuite la g{\'e}ologie et l{\textquoteright}hydrog{\'e}ologie qui portera sur l{\textquoteright}{\'e}tude des principales phases tectoniques, et plus particuli{\`e}rement le syst{\`e}me de la fracturation permettant l{\textquoteright}{\'e}mergence des eaux chaudes ; ainsi que la d{\'e}finition des diff{\'e}rents aquif{\`e}res dans le contexte lithostratigraphique, structural, g{\'e}ophysique et hydrog{\'e}ologique. CHAPITRE II : hydroclimatologie Elle a pour objet d{\textquoteright}{\'e}tudier les facteurs importants comme la temp{\'e}rature de l{\textquoteright}air pour d{\'e}finir les limites de la thermalit{\'e} de la r{\'e}gion et les pr{\'e}cipitations qui conditionnent le bilan hydrologique et la recharge des aquif{\`e}res. Elle permettra {\'e}galement la classification de la zone concern{\'e}e sur la base d{\textquoteright}indices climatiques et d{\textquoteright}{\'e}tablir les principaux {\'e}l{\'e}ments du bilan hydrique qui est d{\textquoteright}une importance capitale Deuxi{\`e}me partie CHAPITRE I : hydrochimie Cette partie essentielle dans notre travail de recherches, reposera sur le traitement des donn{\'e}es des diff{\'e}rentes analyses chimiques aussi bien les {\'e}l{\'e}ments majeurs que mineurs (fer, mangan{\`e}se fluor, iode etc...) et la relation existante entre eux. En particulier la teneur en fer dans les eaux de Hammam Guergour. L{\textquoteright}interpr{\'e}tation et l{\textquoteright}exploitation de ces analyses permettront d{\textquoteright}aboutir aux origines g{\'e}ologiques des eaux thermomin{\'e}rales (froides et chaudes), mais aussi d{\textquoteright}avoir une id{\'e}e sur la nature des formations lithologiques travers{\'e}es par ces eaux et leur dynamique. CHAPITRE II : G{\'e}othermom{\'e}trie Dans ce chapitre nous tenterons d{\textquoteright}estimer les temp{\'e}ratures des eaux en profondeur des diff{\'e}rentes sources thermales en utilisant divers g{\'e}othermom{\`e}tres chimiques, comme indicateurs des temp{\'e}ratures minimales et maximales au droit de l{\textquoteright}aquif{\`e}re. Sachant que la plupart des m{\'e}thodes utilis{\'e}es reposent sur les teneurs des eaux de certains {\'e}l{\'e}ments caract{\'e}ristiques tels que : silice, calcium, sodium, potassium et carbonates},
	url = {https://www.pnst.cerist.dz/detail.php?id=49416/},
	author = {Djemmal Samir}
}
@mastersthesis {5682,
	title = {Flux azot{\'e} : origine et devenir dans les eaux souterraines, cas de la r{\'e}gion de Zana-est Alg{\'e}rien},
	year = {2018},
	abstract = {Nous avons essay{\'e}, par ce travail, d{\textquoteright}apporter une contribution {\`a} l{\textquoteright}{\'e}tudier les aquif{\`e}res de la plaine de Zana, et d{\textquoteright}{\'e}valuer les risques de la pollution li{\'e}e au flux azot{\'e}.La plaine de Zana fait partie du bassin versant des hauts plateaux constantinois et plus pr{\'e}cis{\'e}ment du sous bassin versant Merdja Zana, qui s{\textquoteright}{\'e}tend sur une superficie de 369 Km{\texttwosuperior} environ.L{\textquoteright}{\'e}tude de la g{\'e}ologie en association avec les donn{\'e}es de la g{\'e}ophysique met en {\'e}vidence l{\textquoteright}existence de deux formations. La premi{\`e}re formation, de surface d{\textquoteright}{\^a}ge Mio-Plio-Quaternaire form{\'e}e par desniveaux de sable, de gravier, de calcaire lacustre et des intercalations argileuses. La deuxi{\`e}me formation, elle est carbonat{\'e}e et form{\'e}e essentiellement par des calcaires du Cr{\'e}tac{\'e} inf{\'e}rieur et du Jurassique sup{\'e}rieur de l{\textquoteright}ensemble sud s{\'e}tifien et du parautochtone aur{\'e}sien. Le recouvrement de surface atteint dans certainsendroits les 150m d{\textquoteright}{\'e}paisseur notamment au milieu de la plaine et une faible {\'e}paisseur au voisinage des massifs. Quant aux formations carbonat{\'e}es elles ont 350m d{\textquoteright}{\'e}paisseur.La g{\'e}omorphologie, montre que notre bassin est allong{\'e}, il a une altitude moyenne de 935m et il est caract{\'e}ris{\'e} par un relief mod{\'e}r{\'e} et de pente douce.Le r{\'e}seau hydrographique est pet d{\'e}velopper et de type endor{\'e}ique avec un {\'e}coulement temporaire.L{\textquoteright}{\'e}tude climatologique a montr{\'e} que la r{\'e}gion d{\textquoteright}{\'e}tude a un climat semi aride avec un bilan hydrologique d{\'e}ficitaire.L{\textquoteright}aper{\c c}u hydrog{\'e}ologique de la plaine montre que les formations du Cr{\'e}tac{\'e} inf{\'e}rieur et du Jurassique sup{\'e}rieur peuvent offrir des possibilit{\'e}s aquif{\`e}res tr{\`e}s int{\'e}ressantes de m{\^e}me que la formation superficielle, elle pr{\'e}sente des potentialit{\'e}s aquif{\`e}res non n{\'e}gligeables. La pi{\'e}zom{\'e}trie montre une convergence vers les d{\'e}pressions de Merdja de Zana et le Chott Saboun, qui repr{\'e}sentent des exutoires naturels dela nappe.L{\textquoteright}{\'e}tude hydrochimique a permis d{\textquoteright}attribuer l{\textquoteright}origine {\'e}vaporitique aux {\'e}l{\'e}ments Na+, Mg++, K+, Cl-,SO4--, quant {\`a} l{\textquoteright}{\'e}l{\'e}ment HCO3-, il est issu des formations carbonat{\'e}es. Les deux compagnes d{\textquoteright}analyses effectu{\'e}es montrent que les eaux issues del{\textquoteright}aquif{\`e}re superficiel et de l{\textquoteright}aquif{\`e}re karstique ont le m{\^e}me faci{\`e}s hydrochimique qui est de type chlorur{\'e} et sulfat{\'e} magn{\'e}sien, ce qui t{\'e}moigne de l{\textquoteright}existence d{\textquoteright}une interaction probable entre les deux aquif{\`e}res},
	url = {http://docplayer.fr/66130950-Flux-azote-dans-les-eaux-souterraines-origine-et-devenir-cas-de-la-plaine-de-zana-est-algerien.html},
	author = {ATHAMENA Ali}
}
@proceedings {4899,
	title = {Proposal for a new method for assessing the vulnerability of aquifers to contamination, ISSN 1737-3638},
	journal = {3rd International Conference on Integrated Environmental Management for Sustainable Development "ICIEM 2018" , May 02 to 05, 2018.  Sousse, Tunisia},
	year = {2018},
	url = { www.iciem-conference.com},
	author = {Drias Tarek and Abdelhamid Khedidja and Belloula Moufida}
}
@conference {4868,
	title = {TERRASSES FLUVIATILES QUATERNAIRES DE L\&$\#$39;OUED EL HAY (BATNA, NE ALG{\'E}RIE): S{\'E}DIMENTOLOGIE ET CARACT{\'E}RISTIQUES DE L\&$\#$39;ENVIRONNEMENT S{\'E}DIMENTAIRE.},
	booktitle = {4{\`e}me Colloque International les G{\'e}osciences au service du D{\'e}veloppement durable (2018)  T{\'e}bessa, Alg{\'e}rie},
	year = {2018},
	abstract = {Une {\'e}tude stratigraphique et s{\'e}dimentologique a {\'e}t{\'e} r{\'e}alis{\'e}e sur une terrasse alluviale de la r{\'e}gion d{\textquoteright}Oued El Hay, au sud de Batna (NE Alg{\'e}rie). Les structures s{\'e}dimentaires observ{\'e}es sont principalement des zones d{\textquoteright}{\'e}rosion, des zones inondables, des figures en biseau et des variations d{\textquoteright}{\'e}paisseur associ{\'e}es {\`a} des joints de stratification. Du point de vue s{\'e}dimentologique, les s{\'e}diments sont domin{\'e}s par des fractions argilo-limono-sableuses, suivies par des fractions de gravier et de cailloux. Les teneurs mod{\'e}r{\'e}es en CaCO3 r{\'e}sultent de la dissolution des reliefs calcaires {\`a} proximit{\'e} (calcaire cr{\'e}tac{\'e}) associ{\'e}e {\`a} l{\textquoteright}augmentation de la temp{\'e}rature et l{\textquoteright}humidit{\'e} du milieu. L{\textquoteright}observation morphoscopique de grains de quartz avec une loupe binoculaire permet d{\textquoteright}offrir une {\'e}volution plus ou moins importante, car ils sont souvent {\'e}mouss{\'e}s ou sous-arrondis. L{\textquoteright}{\'e}tude s{\'e}dimentologique a {\'e}t{\'e} r{\'e}alis{\'e}e sur 16 {\'e}chantillons pr{\'e}lev{\'e}s syst{\'e}matiquement du haut vers le bas de la coupe stratigraphique. L{\textquoteright}examen de la taille brute de la fraction inf{\'e}rieure {\`a} 2 mm a permis d{\textquoteright}individualiser 03 niveaux dans des couches s{\'e}dimentaires, certaines fractions grossi{\`e}res riches (gravier, cailloux et blocs) alternant avec des couches riches en sable et en limon. Le pourcentage de fraction d{\textquoteright}argile est dominant et reste pratiquement constant presque tout au long de la section stratigraphique.},
	url = {https://www.researchgate.net/publication/330038660_TERRASSES_FLUVIATILES_QUATERNAIRES_DE_L{\textquoteright}OUED_EL_HAY_BATNA_NE_ALGERIE_SEDIMENTOLOGIE_ET_CARACTERISTIQUES_DE_L{\textquoteright}ENVIRONNEMENT_SEDIMENTAIRE},
	author = {Fouad Djaiz and Defaflia Nabil and Bachir Lamouri and ATHAMENA Ali and Boushaba Abdellah}
}
@proceedings {4867,
	title = {Quaternary fluviatile terraces of the Oued El Gourzi (Batna, NE Algeria): sedimentology and characteristics of the depositional environment},
	journal = {1ST CONFERENCES OF THE ARABIAN JOURNAL OF GEOSCIENCES (CAJC) (2018) Hammamet, Tunisie},
	year = {2018},
	author = {DJAIZ Fouad and Defaflia Nabil and Lamouri Bachir and Boushaba Abdellah and Chairat. I}
}
@article {4866,
	title = {Geological Characterization and contibution of Geophysics to the mobilization of water resources in the ain djasser basin (South-S{\'e}tifien, Algeria NE)},
	journal = {The Euro-arab Organization for Environment,Water  and Desert Researches, (2018)   Antalya, Turquie},
	year = {2018},
	author = {DJAIZ Fouad and Defaflia Nabil and ATHAMENA Ali and Lamouri Bachir and Boughdiri Mabrouk and Belalite Halima and Boushaba Abdellah}
}
@article {4862,
	title = {The impact of the mobilization of water resources in semi-arid areas on sustainable development the case of Timgad Basin northeastern of Algeria},
	journal = { Advances in Sustainable and Environmental Hydrology, Hydrogeology, Hydrochemistry and Water Resources },
	year = {2018},
	pages = {pp.355-357 },
	abstract = {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.},
	url = {https://link.springer.com/chapter/10.1007/978-3-030-01572-5_83},
	author = {ATHAMENA Ali and Mohamed Redha Menani and Fouad Djaiz and Halima Belalite}
}
@article {4861,
	title = {Quaternary fluviatile terraces of the Oued El Gourzi (Batna, NE Algeria): sedimentology and characteristics of the depositional},
	journal = {Advances in Science, Technology \& Innovation },
	year = {2018},
	pages = {pp 331-334 },
	abstract = {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 CaO3 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.},
	url = {https://link.springer.com/chapter/10.1007/978-3-030-01452-0_79},
	author = {Fouad Djaiz and Defaflia Nabil and Bachir Lamouri and Boushaba Abdellah}
}
@proceedings {4860,
	title = {Biostratigraphie, G{\'e}ochimie et r{\'e}ponse des composantes microfauniques aux variations nvironnementales au passage C{\'e}nomanien-Turonien {\`a} Thniet El Manchar (Monts de Belezma, Batna, NE Alg{\'e}rie)},
	journal = {Estudios Geol{\'o}gicos intitul{\'e} },
	volume = {74},
	number = {1},
	year = {2018},
	abstract = {[fr] La pr{\'e}sente {\'e}tude livre une analyse biostratigraphique et g{\'e}ochimique des d{\'e}p{\^o}ts c{\'e}nomano-turoniens de la r{\'e}gion Th{\'e}ni{\`e}t El Manchar, situ{\'e}e dans les Monts de Bellezma-Batna, et leur {\'e}volution verticale. Une coupe (TM), {\'e}paisse de 180 m, est d{\'e}crite dans ce secteur. Elle correspond {\`a} la Formation des Marnes de Smail, subdivis{\'e}e en quatre unit{\'e}s litho-stratigraphiques (IA, IB, IC, ID), dat{\'e}e du C{\'e}nomanien gr{\^a}ce {\`a} la pr{\'e}sence d{\textquoteright}ammonites et de corail, et {\`a} la base de la Formation des Dolomies de l{\textquoteright}Oued Skhoun (unit{\'e}, IIA), dat{\'e}e de la base du Turonien au moyen de foraminif{\`e}res planctoniques. L{\textquoteright}analyse qualitative et quantitative des foraminif{\`e}res (planctoniques et/ou benthiques), des ostracodes et des marqueurs g{\'e}ochimiques, permet de reconstituer l{\textquoteright}{\'e}volution du pal{\'e}o-environnement et les variations pal{\'e}o-bathym{\'e}triques au cours de l{\textquoteright}intervalle stratigraphique concern{\'e}. Ainsi, les unit{\'e}s IA-IB-IC et la partie inf{\'e}rieure de l{\textquoteright}unit{\'e} ID (C{\'e}nomanien) sont domin{\'e}es par des associations de foraminif{\`e}res benthiques agglutin{\'e}s et des carapaces enti{\`e}res d{\textquoteright}ostracodes, t{\'e}moignant d{\textquoteright}un milieu de plate-forme et d{\textquoteright}un faible hydrodynamisme. Dans ces d{\'e}p{\^o}ts, les associations montrent une diversit{\'e} sp{\'e}cifique faible {\`a} moyenne et une abondance plus ou moins {\'e}lev{\'e}e, t{\'e}moignant de conditions trophiques et d{\textquoteright}oxyg{\'e}nation consid{\'e}r{\'e}es comme normales. Les derniers termes de l{\textquoteright}unit{\'e} ID (sommet du C{\'e}nomanien) et l{\textquoteright}unit{\'e} IIA (base du Turonien) marquent, quant {\`a} eux, une {\'e}volution vers des conditions plus profondes, comme le montre la succession standard des {\'e}v{\'e}nements d{\'e}j{\`a} reconnus en Afrique du nord, {\`a} savoir: l{\textquoteright}abondance de foraminif{\`e}res planctoniques, la pr{\'e}sence de {\textquoteleft}filaments{\textquoteright} et une r{\'e}duction drastique de la faune d{\textquoteright}ostracodes. En outre, les courbes isotopiques du carbone (δ13C) et de l{\textquoteright}oxyg{\`e}ne (δ18O) des carbonates mettent en {\'e}vidence des anomalies isotopiques relatives aux modifications pal{\'e}o-environnementales. Les donn{\'e}es du δ13C et celles du COT indiquent une productivit{\'e} primaire faible. Les donn{\'e}es du δ18O, quant {\`a} elles, indiquent une augmentation des pal{\'e}o-temp{\'e}ratures, cause principale du d{\'e}clenchement de l{\textquoteright}EAO 2. Ces interpr{\'e}tations pal{\'e}o-environnementales s{\textquoteright}accordent avec les donn{\'e}es connues du contexte pal{\'e}og{\'e}ographique r{\'e}gional et mettent en exergue les sp{\'e}cificit{\'e}s t{\'e}thysiennes.},
	url = {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},
	author = {Slami Rafika and Salmi Laouar Sihem and Bruno Ferr{\'e} and Riadh Aouissi and Fatiha Kechid-Benkherouf}
}
@proceedings {4849,
	title = {Approche hydrog{\'e}ologique des plaines de Gadaine et Zana-chott saboun (Wilaya de Batna, Nord est alg{\'e}rien)},
	journal = {4eme colloque international : les g{\'e}osciences au service du d{\'e}veloppement durable Tebessa, Algerie},
	year = {2018},
	author = {ATHAMENA Ali}
}
@proceedings {4845,
	title = {Le colmatage des membranes d\&$\#$39;osmose inverse en dessalment d\&$\#$39;eau : {\'e}tude de l\&$\#$39;ihibition de la pr{\'e}cipitation de CaCO3 par Zn++},
	journal = {Colloque International de Chimie CIC 5, Batna, Alg{\'e}rie, 04-06 d{\'e}cembre 2018},
	year = {2018},
	author = {Ait Mohand Said Meriem and Bouhidel Kamel}
}
@proceedings {4844,
	title = {Coexistence effect of some ions on the nanofiltration quality},
	journal = {5{\`e}me s{\'e}minaire international sur l{\textquoteright}eau et l{\textquoteright}environnement, Chlef, 20-22 novembre 2018},
	year = {2018},
	author = {Ait Mohand Said Meriem and Bouhidel Kamel}
}
@proceedings {4843,
	title = {Synthetisis of  ZnO Bentonite as photocatalysis to degrade cationic yellow dye},
	journal = {2nd International symposium on catalysis , Tlemcen, 1-3 Octobre 2018},
	year = {2018},
	author = {Belgaid Nassima and MENANI Mohamed redha and Bouhidel Kamel}
}
@proceedings {4842,
	title = {Valorisation de mat{\'e}riaux g{\'e}ologiques dans l\&$\#$39;industrie de l\&$\#$39;eau},
	journal = {1er s{\'e}minaire maghr{\'e}bin sur  l{\textquoteright}eau et l{\textquoteright}environnement dans les zones arides, Ouargla, 23-25 avril 2018},
	year = {2018},
	author = {Belgaid Nassima and MENANI Mohamed redha and Bouhidel Kamel}
}
@proceedings {4841,
	title = {Synthetisis of Inorganic/organic modified Bentonite and its application for textile dye removal from water},
	journal = {Colloque International de Chimie CIC 5, Batna, Alg{\'e}rie, 04-06 d{\'e}cembre 2018},
	year = {2018},
	author = {Belgaid Nassima and MENANI Mohamed redha and Bouhidel Kamel}
}
@proceedings {4840,
	title = {Elaboration of Al-Bent, Fe-Bent, CTAB Bent,, AL-CTAB-Bent and Fe-CTAB-Bent from algerian Bentonite clay to adsorb cationic textiles dyes},
	journal = {International Water Forum Conference, Hammamet, Tunisie, 19-21 Mars },
	year = {2018},
	author = {Belgaid Nassima}
}
@proceedings {4839,
	title = {Approche hydrog{\'e}ologie et isotopique pour la connaissance de l\&$\#$39;origine de la salinisation des eaux souterraines d\&$\#$39;Oued Labiod, NE alg{\'e}rien },
	journal = {4{\`e}me colloque international sur les g{\'e}osciences et le d{\'e}veloppement durable, T{\'e}bessa,  Nov },
	year = {2018},
	author = {Rihani Abla and MENANI Mohamed redha}
}
@proceedings {4837,
	title = {Approche hydrog{\'e}ologique des plaines de Gdaine et Zana-chott saboun, NE alg{\'e}rien.},
	journal = {4{\`e}me colloque international sur les g{\'e}osciences, T{\'e}bessa},
	year = {2018},
	author = {Belalit Halima and MENANI Mohamed redha}
}
@proceedings {4835,
	title = {The SASS transboundary water resources, joint management and risk of conflicts},
	journal = {International Journal of arts and sciences UNLV, 12-16, 2018, USA},
	year = {2018},
	url = {https://unlv2018.sched.com/},
	author = {MENANI Mohamed redha}
}
@proceedings {4834,
	title = {Hydrogeological and hydrochemical study of Teleghma aquifer (NE Algeria)},
	journal = {3rd International conference on Integrated environmental management for sustainable development, 2-5 mai 2018, Sousse, Tunisie},
	year = {2018},
	author = {Dekakra Mouna and MENANI Mohamed redha and Abdelhamid Khedidja}
}
@proceedings {4833,
	title = {Adaptation de l\&$\#$39;agriculture saharienne {\`a} la s{\'e}cheresse - cas de la r{\'e}gion d\&$\#$39;Oued Souf (Alg{\'e}rie)},
	journal = {16 {\`e}me Conf{\'e}rence Internationale EURO-RIOB, 17-20 Oct 2018, S{\'e}ville, Espagne},
	year = {2018},
	author = {MENANI Mohamed redha}
}
@article {3622,
	title = {Approche hydrog{\'e}ologique du bassin mioc{\`e}ne de Timgad(Wilaya de Batna -- nord-est alg{\'e}rien), ISSN: 1370 - 6071},
	journal = {Geo-Eco-Trop~},
	volume = {volume 42},
	number = { issue 1 },
	year = {2018},
	pages = {pp.33-42},
	abstract = {Timgad Basin is a part of the North-East Algerian Saharan Atlas. It is located at the northern of the Aur{\`e}s 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.},
	url = {http://www.geoecotrop.be/uploads/publications/pub_421_03.pdf},
	author = {Lebchek Soumia and MENANI Mohamed redha}
}
@article {3616,
	title = {The influence of the aquifer geometry on the groundwater flows (Timgad Basin, North-East Algeria), ISSN / e-ISSN: 2220-6663 /2222-3045},
	journal = {journal of Biodiversity and Environmental Sciences (JBES)},
	volume = {Vol. 12},
	number = {No. 5},
	year = {2018},
	pages = {pp. 354-360},
	abstract = {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\&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.},
	url = {https://innspub.net/jbes/influence-aquifer-geometry-groundwater-flows-timgad-basin-north-east-algeria/},
	author = {Lebchek Soumia and MENANI Mohamed redha}
}
@article {3610,
	title = {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},
	journal = {Arabian Journal of Geosciences},
	volume = {Vol 11},
	number = {Issue 13},
	year = {2018},
	abstract = {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.},
	url = {https://doi.org/10.1007/s12517-018-3681-5},
	author = {Athamenani Ali and MENANI Mohamed redha}
}
@mastersthesis {2916,
	title = {{\'E}tude g{\'e}ologique de la plaine Sud S{\'e}tifienne par une approche g{\'e}ophysique},
	year = {2018},
	author = {Kechha}
}
@mastersthesis {2915,
	title = {{\'E}tude g{\'e}ologique de la plaine de Gadaine par une approche g{\'e}ophysique},
	year = {2018},
	author = {Douaflia Abdelkader and Benour yahia}
}
@proceedings {2416,
	title = {Hydrochemical Analysis and Evaluation of Groundwater Quality of an Alluvial Aquifer. Algeria.},
	year = {2018},
	author = {Drias Tarek and Fehdi Chemseddine and Belloula Moufida}
}
@proceedings {2190,
	title = {Evolution tectono-sedimentaires dans la serie aptienne de Telidjene-Tebessa (Algerie oreiental)},
	journal = {4eme Colloque International, les G{\'e}osciences au service du D{\'e}veloppement durable, universit{\'e} Larbi Tebessi,Tebessa, Alger 22 novembre.},
	year = {2018},
	address = {Tebessa, Alger},
	author = {Bentahar Fahima and Inal Ahmed and Yahaoui Abedel Ouahab}
}
@proceedings {2189,
	title = {Lithostratigraphie de la serie Aptienne du DJ Bouroumane-Tebessa (Algerie oriental)},
	journal = {4eme Colloque International, les G{\'e}osciences au service du D{\'e}veloppement durable, universit{\'e} Larbi Tebessi,Tebessa, Alger 22 novembre.},
	year = {2018},
	address = {Tebessa, Alger},
	author = {Bentahar Fahima and Yahaoui Abedel Ouahab and Inal Ahmed}
}
@proceedings {2170,
	title = {Les ressources en eau du Nord Est Algerien region de Tolga, qualit{\'e} des eaux  de la nappe des calcaires},
	journal = {4eme Colloque International, les G{\'e}osciences au service du D{\'e}veloppement durable, universit{\'e} Larbi Tebessi,Tebessa, Alger 22 novembre},
	year = {2018},
	address = {Tebessa, Alger},
	author = {Zouaoui Siham and MENANI Mohamed redha and Bouabid Abd Ennasser}
}
@proceedings {2169,
	title = {Etude de la qualit{\'e} des eaux de la nappe superficielle dans la region de Tolga},
	journal = {4eme Colloque International, les G{\'e}osciences au service du D{\'e}veloppement durable, universit{\'e} Larbi Tebessi,Tebessa, Alger 22 novembre.},
	year = {2018},
	address = {Tebessa, Alger},
	author = {Zouaoui Siham and MENANI Mohamed redha and Bouabid Abd Ennasser and Boukhenissa F and Ahmadi L}
}
@article {2138,
	title = {Use of mechanical drill data and vertical electrical soundings for the identification of aquifer geometry of lower Maestrichtian limestone M\&$\#$39;Daourouch Drea plain Wilaya of Souk Ahras NE Algerian, ISSN / e-ISSN 2220-6663 / 2222-3045},
	journal = {Journal of Biodiversity and Environmental Sciences (JBES)},
	volume = {Volume 12},
	number = {1},
	year = {2018},
	pages = {pp 90-95},
	abstract = {This paper was made in the region of M{\textquoteright}daourouch-Dr{\'e}a 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.},
	url = {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/},
	author = {Brahmia Ali and Brinis Nafaa}
}
@proceedings {2135,
	title = {Contribution of statistical technique in the Characterization hydro-chimical of groundwater, case of the region Zana-Roknia, Eastern Algeria},
	journal = {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},
	year = {2018},
	address = {Antalya, Turkey },
	author = {ATHAMENA Ali}
}
@article {2130,
	title = {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},
	journal = {Arabian Journal of Geosciences},
	volume = { Vol 11},
	number = {Issue 13},
	year = {2018},
	abstract = {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.},
	url = {https://doi.org/10.1007/s12517-018-3681-5},
	author = {ATHAMENA Ali and MENANI Mohamed redha}
}
@proceedings {2128,
	title = {Qualit{\'e} des eaux de surface d\&$\#$39;Oued Saf-Saf (Nord Est Algerien)},
	journal = {4eme Colloque International, les G{\'e}osciences au service du D{\'e}veloppement durable, universit{\'e} Larbi Tebessi,Tebessa, Alger 22 novembre},
	year = {2018},
	address = {Tebessa, Alger},
	author = {Kemoukh Sami and DJAIZ Fouad and ATHAMENA Ali}
}
@proceedings {2127,
	title = {The Evaluation of the Belezmamounts thermal potential: at the South-Eastern confinement of the South Setifian Set, Eastern Algeria},
	journal = {4eme Colloque International, les G{\'e}osciences au service du D{\'e}veloppement durable, universit{\'e} Larbi Tebessi,Tebessa, Alger 22 novembre},
	year = {2018},
	address = {Tebessa, Alger},
	author = {ATHAMENA Malika and MENANI Mohamed redha and ATHAMENA Ali}
}
@proceedings {2126,
	title = {Approche hydrog{\'e}ologique des plaines de Gadaine et Zana-Chott Saboun (wilaya de Batna, Nord-Est Algerienne)},
	journal = {4eme Colloque International, les G{\'e}osciences au service du D{\'e}veloppement durable, universit{\'e} Larbi Tebessi,Tebessa, Alger 22 novembre},
	year = {2018},
	author = {Bilalite Halima and MENANI Mohamed redha and ATHAMENA Ali}
}
@proceedings {2125,
	title = {Barrages et Envirennement, une relation d{\'e}velopp{\'e}, Cas du Barrage de Beni-Haroun, Mila, Est Algerie},
	journal = {4eme Colloque International les G{\'e}osciences au service du D{\'e}veloppement durable, universit{\'e} Larbi Tebessi,Tebessa, Alger 22 novembre},
	year = {2018},
	address = {Tebessa, Alger},
	author = {ATHAMENA Ali and MENANI Mohamed redha and Bilalite Halima and Ghenima Z and Teffaha S and Kihel K}
}
@proceedings {2124,
	title = {Approche statistique dans la caract{\'e}risation physico-chimique des eaux souterraines, cas de Chott-Saboun, Est Alg{\'e}rie},
	journal = {4eme Colloque International les G{\'e}osciences au service du D{\'e}veloppement durable, universit{\'e} Larbi Tebessi,Tebessa, Alger 22 novembre},
	year = {2018},
	address = {Tebessa, Alger},
	author = {ATHAMENA Ali}
}
@proceedings {2009,
	title = {10{\`e}me International Symposium on Cephalopods \&laquo; Present and Past \&raquo; organised by Sidi Mohamed Ben Abdellah University Fes and the Westfalische Wilhelms University, Muenster, 26th March-3rd April 2018.MAROC},
	journal = {10th INTERNATIONAL SYMPOSIUM {\textquotedblleft}CEPHALOPODS {\textendash} PRESENT AND PAST},
	year = {2018},
	address = {MAROC},
	author = {DJAIZ Fouad}
}
@article {1887,
	title = {Hydrogeochemical Assessment of an Alluvial Aquifer Under Semi-Arid Climat. Eastern Algeria, ISSN 2321 \&ndash;9009},
	journal = {International Journal of Advances in Science, Engineering and Technology (IJASEAT)},
	volume = {Volume-6},
	number = {Issue-1},
	year = {2018},
	abstract = {The study of the water quality in the alluvial aquifer of Tebessa-Morsott basinwas carried out to perform a preliminary assessmentof the hydrochemical quality of same groundwater samples and their suitability for irrigation uses. The high salinity coupledwith 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.},
	url = {http://www.iraj.in/journal/journal_file/journal_pdf/6-331-148853256927-32.pdf},
	author = {Drias Tarek and Belloula Moufida}
}
@inbook {1885,
	title = {Hydrochemical Analysis and Evaluation of Groundwater Quality of an Alluvial Aquifer. Algeria},
	booktitle = {Recent Advances in Environmental Science from the Euro-Mediterranean and Surrounding Regions},
	year = {2018},
	pages = { 637-639},
	publisher = {Springer },
	organization = {Springer },
	address = {Cham},
	abstract = {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.},
	url = {https://doi.org/10.1007/978-3-319-70548-4_191},
	author = {Drias Tarek and Chemseddine Fehdi and Moufida Belloula}
}
@article {1884,
	title = {Statistical and hydro-geochemical characteristics of the M\&rsquo;daourouch-Drea plain\&rsquo;s groundwater; North-east of Algeria, ISSN / e-ISSN 1429-7426 / 2083-4535},
	journal = {Journal of Water and Land Development},
	number = {N{\textdegree}38},
	year = {2018},
	pages = { pp 19{\textendash}26. (VII-IX) 2018 (promesse de publication).},
	abstract = {This work was conducted on 23 samples distributed between springs, wells and boreholes tapping the shal-low and deep aquifer in the M{\textquoteright}Daourouch-Drea area located in extreme northeast of Algeria. Ca2+, Mg2+, Na+, K+, Cl{\textendash}, SO42{\textendash}, HCO3{\textendash} and NO3{\textendash} were analysed. The interpretation of the geological-geophysical data allowed us to highlight two aquifers. The first consists of conglomerates, sandstones, gravels, sands, marls, limestones, la-custrine and alluvial deposits varying in thickness from a few tens to a few hundred meters, representing Neo-gene-Quaternary filling of the studied basin. The second is more important localized in the cracked and karstified limestones of upper Cretaceous age; these limestones are outcropped on the flanks of the syncline and the bor-ders of the basin. The first aquifer sometimes rests directly on the second which allows hydraulic communication between them. The hydogeochemical and statistical study, with the combination of numerous tools, indicates that the chemistry of groundwater in the M{\textquoteright}Daourouch-Drea Plain is controlled both by the dissolution of the miner-als of the evaporite formations and those of the carbonate formations.},
	url = {https://www.degruyter.com/downloadpdf/j/jwld.2018.38.issue-1/jwld-2018-0038/jwld-2018-0038.pdf},
	author = {Brahmia Ali and Brinis Nafaa and Nouar Tahar}
}
@article {1883,
	title = {Use of mechanical drill data and vertical electrical soundings for the identification of aquifer geometry of lower Maestrichtian limestone M\&$\#$39;Daourouch Drea plain Wilaya of Souk Ahras NE Algerian},
	journal = {Journal of Biodiversity and Environmental Sciences (JBES)},
	volume = {12},
	number = {01},
	year = {2018},
	pages = {pp 90-95},
	abstract = {This paper was made in the region of M{\textquoteright}daourouch-Dr{\'e}a 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.},
	url = {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/},
	author = {Brahmia Ali and Brinis Nafaa}
}
@inbook {1882,
	title = {La pollution des rejets liquides de la ville de Batna (Alg{\'e}rie). Impacts sur l\&rsquo;agriculture et sur les eaux destin{\'e}es {\`a} l\&rsquo;usage domestique},
	booktitle = {Eau et climat en Afrique du Nord et au Moyen-Orient},
	year = {2018},
	pages = {113-124},
	author = {MENANI Mohamed redha}
}
@inbook {1881,
	title = {{\'E}valuation du risque de conflit autour des eaux transfrontali{\`e}res du syst{\`e}me aquif{\`e}re du Sahara septentrional (SASS)},
	booktitle = {Eau et climat en Afrique du Nord et au Moyen-Orient},
	year = {2018},
	pages = {45-69},
	abstract = {
	
		Le SASS couvre une superficie d{\textquoteright}environ 1\&nbsp;000\&nbsp;000 km{\texttwosuperior}, il est partag{\'e} par l{\textquoteright}Alg{\'e}rie, la Libye et la Tunisie. Il est situ{\'e} dans une zone hyper aride avec une recharge actuelle minime mais un grand volume stock{\'e}, {\'e}valu{\'e} entre 20\&nbsp;000 et 31\&nbsp;000 km3.
	

	
		Depuis 1970 {\`a} nos jours, l{\textquoteright}exploitation du SASS est pass{\'e}e de 0,6 {\`a} plus de 2,5 milliards m3/an., d{\textquoteright}o{\`u} des risques majeurs \&nbsp;de salinisation des eaux, de r{\'e}duction de l{\textquoteright}art{\'e}sianisme, de tarissement des exutoires naturels, de baisse de la pi{\'e}zom{\'e}trie, d{\textquoteright}augmentation des rabattements ou d{\textquoteright}interf{\'e}rences des p{\'e}rim{\`e}tres de captage entre pays{\textellipsis}Ce qui menace {\`a} terme la durabilit{\'e} du d{\'e}veloppement socio-{\'e}conomique engag{\'e} dans l{\textquoteright}ensemble de la zone.
	

	
		Pour parer au mieux {\`a} ces risques et surtout pour mieux s{\textquoteright}en pr{\'e}munir, un processus de coop{\'e}ration a {\'e}t{\'e} initi{\'e} depuis 1998 sous l{\textquoteright}{\'e}gide de l{\textquoteright}observatoire du Sahara septentrional (OSS) en partenariat avec les institutions en charge des ressources en eau dans les 3 pays.
	

	
		L{\textquoteright}importance de cet immense r{\'e}servoir pour le d{\'e}veloppement de la zone SASS et la n{\'e}cessit{\'e} de sa gestion durable et concert{\'e}e a amen{\'e} {\`a} une entente pour son {\'e}tude en plusieurs phases\&nbsp;: la caract{\'e}risation hydrog{\'e}ologique du syst{\`e}me aquif{\`e}re et sa mod{\'e}lisation, l{\textquoteright}identification des risques environnementaux et l{\textquoteright}inclusion de l{\textquoteright}aspect socio-{\'e}conomique dans des sc{\'e}narios de d{\'e}veloppement.
	

	
		Les ressources en eau du SASS sont tr{\`e}s faiblement renouvelables, environ 1 milliard de m3/an, vis-{\`a}-vis des pr{\'e}l{\`e}vements actuels estim{\'e}s {\`a} 2,5 milliards de m3/an. La prise en compte de cette donn{\'e}e a {\'e}t{\'e} d{\'e}terminante pour pousser les scientifiques {\`a} {\'e}tablir la meilleure mod{\'e}lisation conceptuelle possible du syst{\`e}me qui soit {\`a} m{\^e}me de permettre d{\textquoteright}envisager diff{\'e}rents sc{\'e}narios d{\textquoteright}exploitation de la ressource tout en tenant compte des perspectives de d{\'e}veloppement socio-{\'e}conomique de chacun des 3 pays.
	

	
		Les donn{\'e}es actuelles, quoique rassurantes, ne signifient pas l{\textquoteright}inexistence, {\`a} court ou moyen terme, d{\textquoteright}un risque de conflit autour de ces eaux transfrontali{\`e}res. En effet, le probl{\`e}me m{\'e}rite d{\textquoteright}{\^e}tre analys{\'e} {\`a} travers plusieurs indicateurs qui ont un impact sur ce risque.
	

	
		L{\textquoteright}objectif de cette note est d{\textquoteright}{\'e}valuer le risque de conflit autour des eaux du SASS {\`a} travers un indice global exprim{\'e} num{\'e}riquement 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.
	

	
		L{\textquoteright}indice global de risque de conflit obtenu pour le cas du SASS semble refl{\'e}ter correctement la situation qui y pr{\'e}vaut actuellement. La comparaison de ce r{\'e}sultat avec ceux obtenus pour les eaux transfrontali{\`e}res du bassin du Jourdain (risque {\'e}lev{\'e}) et ceux du syst{\`e}me aquif{\`e}re du Guarani (risque faible), conforte l{\textquoteright}{\'e}chelle des valeurs adopt{\'e}e dans cette m{\'e}thode d{\textquoteright}indexation num{\'e}rique.
	

},
	author = {MENANI Mohamed redha}
}
@mastersthesis {5702,
	title = {Contribution au Suivi pi{\'e}zom{\'e}trique et hydrochimie  dans la plaine de Belezma (W, de Batna)},
	year = {2017},
	author = {Righi Asma}
}
@mastersthesis {5697,
	title = {{\'E}tude stratigraphique et s{\'e}dimentologique du Campanien sup{\'e}rieur du massif d\&$\#$39;El Kantara},
	year = {2017},
	author = {Touahria Kamel and Khabar Ali}
}
@mastersthesis {5689,
	title = {Contribution {\`a} l\&rsquo;{\'e}tude hydrog{\'e}ologique de la nappe Mio-Plioc{\`e}ne de la r{\'e}gion de Tolga},
	year = {2017},
	author = {Toumi.A}
}
@mastersthesis {5686,
	title = {Impact des plans d\&rsquo;eau artificiels sur les r{\'e}gimes hydrologiques - Cas du barrage de beni haroune - mila - Est alg{\'e}rien},
	year = {2017},
	author = {Ghemima. Z}
}
@mastersthesis {5681,
	title = {Les effondrements dans les terrains karstiques du plateau de Cheria (NE de l\&$\#$39;Alg{\'e}rie), impacts gotechnique et environnementaux et cartographie des zones vuln{\'e}rables au ph{\'e}nom{\`e}ne.},
	year = {2017},
	abstract = {Les effondrements des cavit{\'e}s souterraines dans les calcaires karstifi{\'e}s constituent un al{\'e}a g{\'e}ologique s{\'e}rieux qui continue {\`a} recevoir une intention particuli{\`e}re {\`a} l{\textquoteright}{\'e}chelle de la plan{\`e}te. Il s{\textquoteright}agit d{\textquoteright}un ph{\'e}nom{\`e}ne tr{\`e}s connus, li{\'e} {\`a} la pr{\'e}sence de vides souterrains dans les terrains calcaires, dolomitiques et gypsif{\`e}res. Le plateau de Ch{\'e}ria correspond {\`a} une structure synclinale, grossi{\`e}rement triangulaire d{\textquoteright}orientation NE {\textendash} SW affect{\'e} par une fracturation orthogonale {\`a} l{\textquoteleft}axe du pli. Il est essentiellement form{\'e} de calcaires Eoc{\`e}ne largement karstifi{\'e} et recouvert de mat{\'e}riaux meubles, essentiellement des alluvions, des argiles et des encroutements calcaires. Ce bassin en question abrite trois aquif{\`e}res superpos{\'e}s, l{\textquoteright}aquif{\`e}re du Maastrichtien, l{\textquoteright}Eoc{\`e}ne et la nappe alluviale du Moi-Plio-Quaternaire. Celle qui fait l{\textquoteright}objet de cette {\'e}tude est la nappe de l{\textquoteright}Eoc{\`e}ne. Le sens d{\textquoteright}{\'e}coulement g{\'e}n{\'e}rale dans les nappes souterraines notamment les alluvions et l{\textquoteright}Eoc{\`e}ne est sensiblement Nord-Sud. La surexploitation actuelle des eaux souterraines a rendu la nappe des alluvions sans int{\'e}r{\^e}t hydrog{\'e}ologique, et a caus{\'e} un grand rabattement dans les calcaires de l{\textquoteright}Eoc{\`e}ne. Les m{\'e}thodes directes et indirectes d{\textquoteright}explorations du sous-sol de la r{\'e}gion ont r{\'e}v{\'e}l{\'e}s la pr{\'e}sence de plusieurs cavit{\'e}s souterraines de dimensions importantes. La m{\'e}thode de tomographie {\'e}lectrique, G{\'e}oradar et les sondages m{\'e}caniques ont montr{\'e} l{\textquoteright}existence {\`a} faible profondeur des cavit{\'e}s dans la r{\'e}gion d{\textquoteright}{\'e}tude. La stabilit{\'e} de ces cavit{\'e}s d{\'e}pend d{\textquoteright}un c{\^o}t{\'e} des propri{\'e}t{\'e}s m{\'e}caniques de la masse rocheuse formant le toit de la galerie, et les dimensions de cette derni{\`e}re. Cette {\'e}tude nous a permis d{\textquoteright}{\'e}tablir des relations entre l{\textquoteright}{\'e}paisseur du toit, largeur de cavit{\'e}, et la charge pour un RMR (Rock masse rating) variable. La cartographie men{\'e}e {\`a} l{\textquoteright}{\'e}chelle de la r{\'e}gion a pu d{\'e}limiter les zones susceptibles de pr{\'e}senter des cavit{\'e}s naturelles instables et cela va permet en cons{\'e}quence de trouver des solutions au probl{\`e}me de l{\textquoteright}effondrement {\`a} l{\textquoteright}{\'e}chelle de la r{\'e}gion},
	url = {http://www.secheresse.info/spip.php?article79566},
	author = {Azizi Yacine}
}
@mastersthesis {5679,
	title = {APPROCHES HYDROGEOCHIMIQUES ET GEOTHERMOMETRIQUES POUR L\&rsquo;ETUDE DES EAUX THERMALES  CAS DU SYSTEME GEOTHERMAL EXPLOITE DANS LA REGION DE BISKRA AU SUD ALGERIEN},
	year = {2017},
	author = {Chafou Nasereddine}
}
@proceedings {4888,
	title = {{\'E}tude tectono-s{\'e}dimentaire de la s{\'e}rie campanienne de Dj. Lekhal (plaine d\&$\#$39;ain Touta)},
	journal = {La 4eme {\'e}dition du Congr{\`e}s des Doctorants 2017 de la FSTGAT se tiendra le 24 et 25 Avril 2017, \&aacut la maison de la science, USTHB, Alger},
	year = {2017},
	author = {Benmansour Sana}
}
@proceedings {4871,
	title = {Sedimentology, Geochemistry and Various Microfaunal Component Responses to Environmental Fluctuations of the Cenomanian-Turonian Boundary at Th{\'e}ni{\`e}t El Manchar (Batna, NE Algeria)},
	journal = {19th International Conference on Geological and Earth Sciences, Word Academy of Science Energinee Ring and Technology, Rome, Italy },
	year = {2017},
	author = {Slami Rafika}
}
@proceedings {4870,
	title = {Les impactes des plans d\&rsquo;eaux artificielles sur les r{\'e}gimes climatiques et hydrologiques {\`a} l\&rsquo;{\'e}chelle. Cas d\&rsquo;un bassin versant du barrage de Beni Haroune, (Mila Est Alg{\'e}rien)},
	journal = {Colloque International Eau-Soci{\'e}t{\'e}-Climat 2017(ESC- 2017) Hammamet 2-3-4 Octobre 2017.},
	year = {2017},
	author = {ATHAMENA Ali and DJAIZ Fouad and Belalit Halima and Guemima. Z and Toufaha. S and Kihel. K}
}
@proceedings {4869,
	title = {G{\'e}om{\'e}trie de l\&rsquo;aquif{\`e}re N{\'e}og{\`e}ne dans le bassin d\&rsquo;El Outaya, Atlas saharien au sud alg{\'e}rien},
	journal = {Colloque International Eau-Soci{\'e}t{\'e}-Climat 2017(ESC- 2017) Hammamet 2-3-4 Octobre 2017},
	year = {2017},
	author = {Brinis Nafaa and Boudoukha Abderahmane and DJAIZ Fouad}
}
@proceedings {4850,
	title = {caracterisation hydrogeologique et hydro-chimique du bassin neogene de timgad (nord-est algerien)},
	journal = {The 1st International Symposium (WREIANA 2017) Water Resources and Environmental Impact Assessment in North Africa, Gafsa, Tunisie},
	year = {2017},
	author = {Brinis Nafaa}
}
@proceedings {4836,
	title = {Caract{\'e}risation hydrog{\'e}ologique et hydrochimique du bassin n{\'e}og{\`e}n,e de Timgad, NE alg{\'e}rien},
	journal = {1er International symposium - WREIANA, 24-26, Gafsa, Tunisie},
	year = {2017},
	author = {Lebchek Soumia and MENANI Mohamed redha and Brinis Nafaa}
}
@article {3629,
	title = {Le campanien -Maastrichtien du bassin des Aur{\`e}s, Alg{\'e}rie: Biostratigraphie, Pal{\'e}oenvironnements et leurs implications.},
	journal = {Annal de pal{\'e}ontologie , Science Direct-Elsevier masson France},
	year = {2017},
	url = {http://doi.org/10.1016/j.annpal. 2017.11.001},
	author = {Benmansour Sana and Yahiaoui Abdelouahab}
}
@article {3625,
	title = {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 },
	journal = {International Journal of GEOMATE},
	volume = {Vol. 12},
	number = {Issue 30},
	year = {2017},
	pages = {pp. 1 - 7},
	abstract = {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{\textquoteright} 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.},
	url = {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},
	author = {Mansouri Zineb and MENANI Mohamed redha}
}
@mastersthesis {2921,
	title = {Etudes s{\'e}dimentologiques de la s{\'e}rie coniacienne du Dj Metlili (Algerie nord oriental)},
	year = {2017},
	author = {Bentahar Fahima}
}
@mastersthesis {2918,
	title = {Etude Pal{\'e}o-Environnemental de la R{\'e}gion de Ain Touta Au Quaternaire : Terrasses Fluviatiles d\&rsquo;Oued El Hai.},
	year = {2017},
	author = {Brikat and Sehtal Sami}
}
@mastersthesis {2917,
	title = {Etude Pal{\'e}o-Environnemental de la R{\'e}gion d\&rsquo;El Mather Au Quaternaire : Terrasses Fluviatiles d\&rsquo;Oued El Gourzi},
	year = {2017},
	author = {Bekkari Sif eddine and Adel Abdelhak}
}
@mastersthesis {2449,
	title = {Contribution {\`a} l\&rsquo;{\'e}tude hydrog{\'e}ologique de la r{\'e}gion du Droh (w) Biskra},
	year = {2017},
	author = {Saada Brahim~Oussama}
}
@mastersthesis {2448,
	title = {Contribution {\`a} l\&rsquo;{\'e}tude hydrog{\'e}ologique du champ captant de l\&rsquo;oued Biskra},
	year = {2017},
	author = {Saber A}
}
@proceedings {2417,
	title = {hydrochemical analysis and evaluation of groundwater quality of an alluvial aquifer. algeria},
	journal = {1st Euro-Mediterranean Conference for Environmental Integration (EMCEI) Springer, Sousse. Tunisia},
	year = {2017},
	address = {Sousse. Tunisia},
	url = {https://www.emcei.net},
	author = {Drias Tarek and Fehdi Chemseddine and Belloula Moufida}
}
@proceedings {2326,
	title = {Qualit{\'e} chimique des eaux de l\&rsquo;aquif{\`e}re Moi-plioc{\`e}ne utilis{\'e} pour l\&rsquo;irrigation de la plaine d\&rsquo;El Outaya au sud Alg{\'e}rien},
	journal = {Colloque International Eau-Soci{\'e}t{\'e}-Climat 2017(ESC- 2017) Hammamet 2-3-4 Octobre },
	year = {2017},
	author = {Brinis Nafaa and Boudoukha Abderahmane and DJAIZ Fouad}
}
@proceedings {2297,
	title = {Qualit{\'e} des eaux du Complexe Terminale du Nord-Est Alg{\'e}rien. R{\'e}gion de Tolga},
	journal = {The 1St Atlas Georessources International Congress, (AGIC). 20-22 March, Hammet, Tunisia.},
	year = {2017},
	address = { Hammet, Tunisia.},
	author = {Zouaoui Siham and MENANI Mohamed redha and Bouabid Abd Ennasser}
}
@article {2195,
	title = {Rock Typing: Reservoir Determination from rock \&ndash; fluid interaction and dynamic behavior : Case Study from an Algerian Oil Field Reservoir},
	journal = {DGMK/{\"O}GEW-Fr{\"u}hjahrstagung, Fachbereich Aufsuchung und Gewinnung Celle, 5./6. April},
	year = {2017},
	abstract = {
	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.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\&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.



	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.



	Application of these listed method for TAGI (TriasArgilo-GreseuxInferieur: Lower Shaly {\textendash} 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).

},
	author = {Benzagouta Mohammed Said and Belhouchet Houssam and Achi. N and Amro.M}
}
@proceedings {2173,
	title = {Caract{\'e}risation g{\'e}ologique et apport de la g{\'e}ophysique pour la mobilisation des ressources hydrique dans le bassin d\&$\#$39;Ain Djasser (Sud-setifien, Alg{\'e}rien NE)},
	journal = {Colloque international Eau{\textendash}Soci{\'e}t{\'e}{\textendash}Climat{\textquoteright}2017 (ESC-2017), Hammamet, Tunis le 2, 3 et 4 Octobre .},
	year = {2017},
	address = {Hammamet, Tunis},
	author = {DJAIZ Fouad and Defaflia Nabil and Boushaba Abdellah and Marmi Ramdane and Dardakhe Mohamed and ATHAMENA Ali and ATHAMENA Malika}
}
@proceedings {2171,
	title = {Impacts des plans d\&$\#$39;Eau sur les r{\'e}gimes hydro-climatiques a l\&$\#$39;{\'e}chelle d\&$\#$39;un bassin verssant, cas du barrage de Beni Haroun, Milan Est Algerien},
	journal = {Colloque international Eau{\textendash}Soci{\'e}t{\'e}{\textendash}Climat{\textquoteright}2017 (ESC-2017), Hammamet, Tunis le 2, 3 et 4 Octobre},
	year = {2017},
	address = {Hammamet, Tunis},
	author = {ATHAMENA Ali and DJAIZ Fouad and Bilalite Halima and Ghenima Z and Teffaha S and Kihel K}
}
@proceedings {2148,
	title = {G{\'e}om{\'e}trie de l\&rsquo;aquif{\`e}re N{\'e}og{\`e}ne dans le bassin d\&rsquo;El-Outaya, Atlas saharien au sud alg{\'e}rien },
	journal = {Colloque international Eau{\textendash}Soci{\'e}t{\'e}{\textendash}Climat{\textquoteright}2017 (ESC-2017), Hammamet, Tunis le 2, 3 et 4 Octobre },
	year = {2017},
	address = {Hammamet, Tunis },
	author = {Brinis Nafaa and Boudoukha Abderahmane and DJAIZ Fouad}
}
@proceedings {2145,
	title = {Qualit{\'e} chimique des eaux de l\&rsquo;aquif{\`e}re Mio-plioc{\`e}ne utilis{\'e}es pour l\&rsquo;irrigation de la plaine d\&rsquo;El-Outaya au sud alg{\'e}rien},
	journal = {Colloque international Eau{\textendash}Soci{\'e}t{\'e}{\textendash}Climat{\textquoteright}2017 (ESC-2017),Hammamet, Tunis le 2, 3 et 4 Octobre },
	year = {2017},
	address = {Hammamet, Tunis },
	author = {Brinis Nafaa and Boudoukha Abderahmane and DJAIZ Fouad}
}
@proceedings {2137,
	title = {Caract{\'e}risation des {\'e}coulements souterrains dans le socle precambrien fissure  de la region de tamanrasset},
	journal = {The 1st international symposium WREIANA, Gafsa 24-26 mars },
	year = {2017},
	address = { Gafsa },
	author = {Boulahbal Souad and MENANI Mohamed redha}
}
@proceedings {2136,
	title = {Etude des ecoulements souterrains dans les gneiss schisteux fissur{\'e}s du pr{\'e}cambrien de la region de tamanrasset},
	journal = {The 1st Atlas Georesources International Congress, Hammamet, tunisia 20-22 mars},
	year = {2017},
	address = {Hammamet, tunisia},
	author = {Boulahbal Souad and MENANI Mohamed redha}
}
@proceedings {2061,
	title = {Assessment of water requirements of olive and apricots trees in Tinibaouine region (north-eastern of Algeria). Impacts of Global Change on Western Mediterranean Aquifers,},
	journal = {Proceedings Congress on Groundwater and Global Change in the Western Mediterranean, Granada },
	year = {2017},
	pages = {pp 277-282},
	address = {Granada },
	url = {http://www.aih-ge.org/index.php/gwm-change-2017/},
	author = {Mansouri Zineb and MENANI Mohamed redha}
}
@proceedings {2011,
	title = {Influence des variations climatiques sur les r{\'e}serves d\&rsquo;eau souterraine des plaines de Zana Chott Saboun et Gadaine (Nord-Est Alg{\'e}rien)},
	journal = {Proceedings Congress on Groundwater and Global Change in the Western Mediterranean Granada. Impacts of Global Change on Western Mediterranean Aquifers},
	year = {2017},
	pages = {pp 171-176},
	address = {Granada},
	url = {http://www.aih-ge.org/index.php/gwm-change-2017/},
	author = {Bilalite Halima and MENANI Mohamed redha}
}
@article {1892,
	title = {Assessing soil loss using GIS based RUSLE methodology. Case of the Bou Namoussa watershed \&ndash; North-East of Algeria, 2018, PL ISSN 1429\&ndash;7426., Polish Academy of Sciences (PAN), Committee on Agronomic Sciences, Degruyte, DOI: 10.2478/jwld-2018},
	journal = {Journal of Water and Land Development },
	number = {No. 36 (I{\textendash}III)},
	year = {2017},
	pages = {pp 27{\textendash}35},
	abstract = {This study aims to estimating annual soil erosion rate and its spatial distribution in the Bou Namoussa water-shed located in the North-East of Algeria by applying the revised universal soil loss equation (RUSLE) within a Geographical Information System environment (GIS). The application of the RUSLE model in different natural environments and on every scale takes into account five key factors namely: the rainfall erosivity, the soil erodi-bility, the steepness and length of slopes, the vegetation cover and the conservation support practices. Each of these factors was generated in GIS as a raster layer, their combination, resulted in the development of a soil loss map indicating an average erosion rate of 7.8 tꞏha{\textendash}1ꞏy{\textendash}1. The obtained soil loss map was classified into four ero-sion severity classes; low, moderate, high and very high severity representing respectively 40, 30.48, 22.59 and 6.89\% of the total surface. The areas, showing moderate, high and very high erosion rates which represent more than half of the basin area were found generally located in regions having high erodibility soils, steep slopes and low vegetation cover. These areas should be considered as priorities in future erosion control programs in order to decrease the siltation rate in the Cheffia reservoir. },
	url = {http://www.itp.edu.pl/wydawnictwo/journal/36_2018_I_III/Bouhadeb.pdf},
	author = {BOUHADEB and MENANI Mohamed redha and BOUGUERRA H and DERDOUS O}
}
@article {1891,
	title = {The contribution of fracturations in the emergence of the thermal springs in Setif city, Eastern Algeria, Carbonates Evaporites},
	journal = {Springer},
	year = {2017},
	abstract = {Setif city covers an area of 6550\&nbsp;km2; it is located about 300\&nbsp;km southeast of Algiers and 100\&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{\textendash}SSE, NW{\textendash}SE, and NE{\textendash}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\&nbsp;m deep.},
	url = {https://www.researchgate.net/publication/318603314_The_contribution_of_fracturations_in_the_emergence_of_the_thermal_springs_in_Setif_city_Eastern_Algeria},
	author = {DJEMMAL S and MENANI Mohamed redha and CHAMEKH K and BAALI F}
}
@article {1890,
	title = {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; Environment, ISSN: 2186-2990, Japan. Feb,2017},
	journal = {International Journal of GEOMATE},
	volume = { Vol. 12},
	number = {Issue 30},
	year = {2017},
	pages = {pp. 46 - 52. },
	abstract = {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 {\textdegree} 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{\textquoteright} 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 3.71mm / 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},
	url = {https://www.geomatejournal.com/sites/default/files/articles/46-52-160424-Zineb-Feb-2017.pdf},
	author = {Mensouri Z and MENANI Mohamed redha}
}
@mastersthesis {5705,
	title = {les caracteristiques physicovhimiques des eaux de continentale intercalaire et de complexe ternimale daans la r{\'e}gion d\&$\#$39;oued Righ},
	year = {2016},
	author = {Belaloui souad and Seba sakina}
}
@mastersthesis {5703,
	title = {Contribution hydrog{\'e}ologique de la plaine de Ain Djasser},
	year = {2016},
	author = {Nezzar Badreddine and Bezai Abderahim}
}
@mastersthesis {5696,
	title = {Etude T{\'e}ctono- s{\'e}dimentaire de la s{\'e}rie Campanienne de Dj. Lekhal (Plaine d\&rsquo;Ain-Touta)},
	year = {2016},
	author = {Guetafi Anfal and Touati Zina}
}
@mastersthesis {5692,
	title = {La s{\'e}rie compano-maestrichtienne de l\&rsquo;anticlinal de Djebel El Azreg : Lithostratigraphie, Pal{\'e}odiversit{\'e} et S{\'e}dimentologie (Aur{\`e}s, Alg{\'e}rie oriental},
	year = {2016},
	author = {Benmansour Sana}
}
@mastersthesis {5691,
	title = {Etude de la qualit{\'e} des eaux souterraines de la nappe profonde destin{\'e}es a l\&rsquo;irrigation cas de la r{\'e}gion de Tolga (W de Biskra)},
	year = {2016},
	author = {Khelil.M and Fedel.W}
}
@mastersthesis {5690,
	title = {Etude de la qualit{\'e} des eaux souterraines de la nappe du quaternaire de la r{\'e}gion de Tolga (W de Biskra)},
	year = {2016},
	author = {Boukhnissa.F and Ahmadi. L}
}
@mastersthesis {5680,
	title = {Etude hydrog{\'e}ologique et gestion int{\'e}gr{\'e}e des eaux de la source de Tinibaouine (Wilaya de Batna -NE Alg{\'e}rien)},
	year = {2016},
	abstract = {La r{\'e}gion de Tinibaouine est situ{\'e}e au Nord-est de l{\textquoteright}Alg{\'e}rie, en bordure Septentrionale des Monts de Batna-Belezma, Elle est caract{\'e}ris{\'e}e par un climat de type semi-aride {\`a} aride avec une pr{\'e}cipitation moyenne annuelle qui n{\textquoteright}exc{\`e}de pas 465mm, et une temp{\'e}rature moyenne annuelle de l{\textquoteright}ordre de 22{\textdegree}C. Cette r{\'e}gion est caract{\'e}ris{\'e}e par la culture de l{\textquoteright}abricot comme culture essentielle suivie des olives, dont les parcelles sont toutes irrigu{\'e}es {\`a} partir de la source. Il s{\textquoteright}agit en effet de 450 Ha d{\textquoteright}arbres destin{\'e}s {\`a} l{\textquoteright}abricotier et de 108 Ha aux olives. L{\textquoteright}{\'e}mergence naturelle des eaux qui ont pour le r{\'e}servoir Dj. Refaa situ{\'e} en contrefort Sud de la plaine de Tinibaouine o{\`u} {\'e}merge la source. Son d{\'e}bit actuel est de l{\textquoteright}ordre de 100 {\`a} 110 l/s (mesur{\'e} en Mars 2015) alors qu{\textquoteright}il pouvait atteindre 200 l/s par le pass{\'e} en 1971. L{\textquoteright}objectif de ce travail est de cerner les contraintes naturelles et anthropiques ayant une incidence directe sur l{\textquoteright}usage de la source et de chercher le mode de gestion appropri{\'e}, qui tienne compte non seulement des solutions techniques qui s{\textquoteright}inspire {\'e}galement des r{\`e}gles sociales qui r{\'e}gissent l{\textquoteright}usage et les conflits qui leurs sont li{\'e}s.},
	url = {http://www.secheresse.info/spip.php?article67759},
	author = {Mansouri Zineb}
}
@mastersthesis {5678,
	title = {ORIGINES ET M{\'E}CANISMES D\&$\#$39;ACQUISITION DE LA MINERALISATION DES EAUX SOUTERRAINES EXPLOITEES DANS LES AURES.  Cas de la vall{\'e}e de l\&rsquo;Oued Abdi (w) de Batna (Nord-Est Alg{\'e}rien)},
	year = {2016},
	author = {Mekaoussi Adel}
}
@proceedings {4873,
	title = {Stratigraphie, g{\'e}ochimie et r{\'e}ponses microfaunistiques aux changement environnementals autour de la limite C{\'e}nomanien-Turonien dans les monts Bellezma-Batna, NE Alg{\'e}rie},
	journal = {Le 1er Colloque International sur la g{\'e}ologie de la cha{\^\i}ne des Maghr{\'e}bides et des r{\'e}gions voisines (CIGCM 2016), Universit{\'e} Ferhat Abbas -S{\'e}tif 1},
	year = {2016},
	author = {Slami Rafika}
}
@proceedings {4872,
	title = {Etude micropal{\'e}ontologique (foraminif{\`e}res, ostracodes) et pal{\'e}oenvironnementale de la limite C{\'e}nomano-Turonienne dans les monts de Batna (Exemple : coupe de Th{\'e}ni{\`e}t El Manchar, Nord-Est Alg{\'e}rie)},
	journal = {1st Arabian Geosciences Union International Conference AIC1, USTHB Alger },
	year = {2016},
	author = {Slami Rafika}
}
@proceedings {4855,
	title = {Int{\'e}r{\^e}t de l\&rsquo;{\'e}tude g{\'e}ologique et hydrog{\'e}ologique pour la mobilisation des ressources hydriques dans le bassin de Timgad (Aur{\`e}s, alg{\'e}rie NE)},
	journal = {Le 1er s{\'e}minaire national sur l{\textquoteright}eau et l{\textquoteright}environnement (SNEE, 2016). Mila, Alg{\'e}rie},
	year = {2016},
	author = {Brinis Nafaa}
}
@proceedings {4846,
	title = {Les variations climatiques sur les eaux souterraines de la plaine de Gadaine (nord-est alg{\'e}rien)},
	journal = {1er S{\'e}minaire National sur l{\textquoteright}eau},
	year = {2016},
	author = {Belalit Halima and MENANI Mohamed redha}
}
@proceedings {4838,
	title = {Approche hydrog{\'e}ologique du bassin n{\'e}og{\`e}ne de Timgad, NE alg{\'e}rien},
	journal = {2nd Ionternational conference on water resources, ICWR, Ouragla, 21-22 Nov },
	year = {2016},
	author = {Lebchek Soumia and MENANI Mohamed redha}
}
@proceedings {4831,
	title = {Caract{\'e}risation hydrochimique et isotopique des eaux souterraines du sous bassin de Oued Labiod, massif des aur{\`e}s, NE Alg{\'e}rien },
	journal = {5{\`e}me conf{\'e}rence internationale du r{\'e}seau eaux et climats, Fes, 12-13 Oct },
	year = {2016},
	author = {Rihani Abla and MENANI Mohamed redha}
}
@proceedings {4830,
	title = {IWRM in north Eastern Batna plains},
	journal = {43rd IAH congress, Montpellier 25-29 sept},
	year = {2016},
	url = {www.iah.org},
	author = {MENANI Mohamed redha}
}
@article {3628,
	title = {The Campaniane Maastrichtian of the Aures basin, Algeria  Paleobiogeographical distrubution of Ostracods},
	journal = {Elsevier Cretaceous Research },
	volume = {Vol. 58},
	year = {2016},
	pages = {pp.86-107},
	abstract = {A detailed biostratigraphic study of four sections (El Kantara, Menaa, Tighanimine and El Ga{\^a}ga) in the Campanian{\textendash}Maastrichtian of the Aures Basin in Algeria allows the identification of 109\&nbsp;ostracod\&nbsp;species belonging to 50 genera. From a biochronostratigraphic point of view, none of the identified ostracod assemblages are typically restricted to the\&nbsp;Campanian\&nbsp;or to the\&nbsp;Maastrichtian, but rather characterize a range covering the Campanian{\textendash}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\&nbsp;Late Cretaceous. The\&nbsp;dispersal\&nbsp;of the ostracods reflects marine communication between these provinces and India, the southern USA and Jamaica, Brazil and Europe.},
	url = {https://doi.org/10.1016/j.cretres.2015.09.015},
	author = {Benmansour Sana and Yahiaoui Abdelouahab}
}
@mastersthesis {2920,
	title = {{\'E}tude g{\'e}ologique de la plaine d\&rsquo;El Mather par une approche g{\'e}ophysique.},
	year = {2016},
	author = {Naji Hossein and Meddour Taib}
}
@mastersthesis {2919,
	title = {{\'E}tude g{\'e}ologique de la plaine d\&rsquo;Ain Djasser par une approche g{\'e}ophysique.},
	year = {2016},
	author = {Derdakhe Mohamed and Baci Maamer}
}
@mastersthesis {2451,
	title = {Traitement des eaux sal{\'e}es -par osmose inverse- pour la production d\&$\#$39;eau potable dans le sud alg{\'e}rien / Unit{\'e} de d{\'e}min{\'e}ralisation de Touggourt},
	year = {2016},
	author = {Beldjani I and Henni Y}
}
@mastersthesis {2450,
	title = {Contribution {\`a} une {\'e}tude Comparative entre    la qualit{\'e} des eaux du Complexe Terminal et du Continental Intercalaire dans la r{\'e}gion D\&rsquo;EL-OUED.},
	year = {2016},
	author = {Dif H}
}
@proceedings {2423,
	title = {water resources in a semi-arid country case a{\"\i}n djasser northeast Algeria},
	journal = {Desalination for Environment : Clean Water and Energy May22{\textendash}26, Rome-Italy},
	year = {2016},
	address = { Rome-Italy},
	author = {Djenba Samir}
}
@proceedings {2422,
	title = {les probl{\`e}mes de mouvement de sols nord de wilaya de S{\'e}tif},
	journal = {1er colloque international sur la g{\'e}ologie de la chaine maghr{\'e}bides et des r{\'e}gions limitrophes S{\'e}tif },
	year = {2016},
	author = {Djenba Samir}
}
@proceedings {2421,
	title = {hydrodynamic caracreization of ground of the region of Tadjnenet- Chelghoum aid (eastern algeria)},
	journal = {International conference on Applied Geology and Environment May19{\textendash}21, Mahdia-  Tunisia},
	year = {2016},
	address = {Mahdia-  Tunisia},
	author = {khadidja A and Djenba Samir and Boudoukha Abderahmane}
}
@proceedings {2420,
	title = {Study of the instability of the land : typology and mapping cases of the wilaya of setif (eastern algeria)},
	journal = {International conference on Applied Geology and Environment May19{\textendash}21 Mahdia-  Tunisia},
	year = {2016},
	address = {Mahdia-  Tunisia},
	author = {Djenba Samir and khadidja A and Boudoukha Abderahmane}
}
@proceedings {2419,
	title = {Assessment of groundwater quality in the plain of ichemoul using the geomatics approach},
	journal = {ISER-78th International Conference on Chemical and Environmental Science (ICCES) Zurich, Switzerland November 22nd -23rd},
	year = {2016},
	address = {Zurich, Switzerland },
	author = {Belloula Moufida and Drias Tarek}
}
@proceedings {2418,
	title = {Hydrogeochemical assessment of an alluvial aquifer under semi-arid climat. Eastern Algeria},
	journal = {ISER-78th International Conference on Chemical and Environmental Science (ICCES) Zurich, Switzerland November 22nd -23rd },
	year = {2016},
	address = {Zurich, Switzerland },
	author = {Drias Tarek and Belloula Moufida}
}
@proceedings {2193,
	title = {Les probl{\`e}mes de mouvements de sols au nord de la wilaya de Setif},
	journal = {1er colloque international sur la g{\'e}ologie de la chaine des maghr{\'e}bides et des r{\'e}gions voisines (CIGCM 2016), universit{\'e} Ferhat Abbas Setif1 Setif, Alger},
	year = {2016},
	address = {Setif, Alger},
	author = {Djenba Samir}
}
@article {2192,
	title = {CONTROLE DES CARACTERISTIQUES PETROPHYSIQUES DES RESERVOIR CARBONATES: CAS DU CONIACIEN \&ndash;SANTONIEN(SUD EST CONSTANTINOIS)},
	journal = {Sciences \& Technologie},
	number = {N{\textdegree}43},
	year = {2016},
	pages = {pp 27-40},
	abstract = {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.},
	url = {http://revue.umc.edu.dz/index.php/d/article/view/2148/2291},
	author = {Cheriet Manel and Benzagouta Mohamed Said}
}
@article {2191,
	title = {Expansive And Aggressive Soil Characteristics And Their Impact On Building Construction: Case Of El Kouif City (tebessa, Algeria)},
	journal = {Bulletin du Service G{\'e}ologique de l{\textquoteright}Alg{\'e}rie },
	volume = {Volume 27},
	number = {Num{\'e}ro 1},
	year = {2016},
	pages = {pp 105-121 },
	abstract = {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.},
	url = {https://asga.dz/wp-content/uploads/2019/01/Bulletin-vol-27-2016.pdf},
	author = {Aoun Mounira and Benzagouta Mohamed Said}
}
@proceedings {2188,
	title = {Aptitude a l\&$\#$39;irrigation par les eaux uses epurees cas de la STEP de Sidi Merouane, willaya de Mila, Est Algerien},
	journal = {10th international conference for water ressources and water security in the middle East and North Africa, held in Istanbul, Turkey on th 14th-16th November},
	year = {2016},
	address = {Istanbul, Turkey },
	author = {ATHAMENA Ali}
}
@proceedings {2187,
	title = {les impacts climatiques sur les eaux souterraines, cas de la plaine de Zana-Chott saboun, Est Algerien},
	journal = {10th international conference for water ressources and water security in the middle East and North Africa, held in Istanbul, Turkey on th 14th-16th November},
	year = {2016},
	address = {Istanbul, Turkey},
	author = {ATHAMENA Ali}
}
@proceedings {2186,
	title = {L\&$\#$39;int{\'e}ret de l\&$\#$39;etude g{\'e}ologique et hydrog{\'e}ologique pour la mobilisation des ressources hydriques dans le bassin de Timgad (Aures, Algerie Nord oriental)},
	journal = {1er S{\'e}minaire National sur l{\textquoteright}eau et l{\textquoteright}environnement (SNEE 2016), Centre universitaire Abdelhafid Boussouf, Milla, Alger 28-29 novembre},
	year = {2016},
	address = {Milla, Alger},
	author = {DJAIZ Fouad and Defaflia Nabil and Brinis Nafaa and ATHAMENA Ali and Marmi Ramdane}
}
@proceedings {2185,
	title = {Aptitude {\`a} l\&$\#$39;irrigation par les eaux us{\'e}es {\'e}pur{\'e}es, cas de la STEPde Sidi Merouane, willaya de Mila, Est Algerien},
	journal = {1er S{\'e}minaire National sur l{\textquoteright}eau et l{\textquoteright}environnement (SNEE 2016), Centre universitaire Abdelhafid Boussouf, Milla, Alger 28-29 novembre},
	year = {2016},
	address = {Milla, Alger},
	author = {ATHAMENA Ali and Lehchili Nouh and Benchaoui Amine and Benabdelaziz Noureddine}
}
@proceedings {2176,
	title = {Fluctuation du niveau pi{\'e}zom{\'e}trique des eaux souterraines cas de la plaine de Zana-Chott Saboun, Batna Est Algerien},
	journal = {1er S{\'e}minaire National sur l{\textquoteright}eau et l{\textquoteright}environnement (SNEE 2016), Centre universitaire Abdelhafid Boussouf, Milla, Alger 28-29 novembre},
	year = {2016},
	address = {Milla, Alger},
	author = {ATHAMENA Ali and Bilalite Halima and Bechar Salah-Eddine and Guesmi Hayat}
}
@proceedings {2013,
	title = {Anthropogenic pressures on groundwater resources. Case of the Northern plains of Batna region (North-East Algeria)},
	journal = {43rd IAH  Congress, 25-29 September, Montpellier, France, },
	number = {Abstract n{\textdegree} 2701. },
	year = {2016},
	author = {MENANI Mohamed redha}
}
@article {1983,
	title = {Geological, Hydrological and Hydrogeological Characterization of the Timgad\&rsquo;s Basin (Aures, Algeriane) for the Mobilization of Water Resources},
	journal = {International Journal of Environment and Water ISSN 2052-3408},
	volume = {Vol 5},
	number = {Issue 3},
	year = {2016},
	pages = {pp 143},
	abstract = {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 Ch{\'e}lia. 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. Caract{\'e}risation g{\'e}ologique, hydrologique et hydrog{\'e}ologique du bassin de Timgad (Aur{\`e}s, Alg{\'e}rie NE), pour la mobilisation des ressources hydriques R{\'e}sum{\'e} : Le bassin de Timgad est situ{\'e}e dans les Aur{\`e}s. Il est caract{\'e}ris{\'e} par une moyenne annuelle des pr{\'e}cipitations de l{\textquoteright}ordre de 800 mm. L{\textquoteright}hydrologie tributaire du relief est la cons{\'e}quence directe des eaux de surface et de la fonte des neiges provenant des hauteurs du massif de Ch{\'e}lia. L{\textquoteright}alimentation de l{\textquoteright}eau souterraine des diff{\'e}rentes nappes phr{\'e}atiques profondes {\`a} semi-profonde provient essentiellement de l{\textquoteright}infiltration des eaux de pluies dans les couches g{\'e}ologiques. Ce cort{\`e}ge de roche forme une nappe libre qui est recoup{\'e}e par des forages sur une profondeur de 137-400 m fournissant un d{\'e}bit de 6 l/s. et des gr{\'e}s blancs grossiers fractur{\'e}s formant une nappe captive {\`a} 190 m avec un d{\'e}bit de 28 l/s. L{\textquoteright}examen des coupes g{\'e}o{\'e}lectriques du bassin montrent que les formations du mioc{\`e}ne et du cr{\'e}tac{\'e} sont dont l{\textquoteright}ensemble, {\'e}pais, h{\'e}t{\'e}rog{\`e}ne et susceptible de contenir de grandes potentialit{\'e}s d{\textquoteright}aquif{\`e}res {\`a} des niveaux diff{\'e}rents. L{\textquoteright}influence de failles normales verticales rend possible une {\'e}ventuelle alimentation des aquif{\`e}res entres eux. L{\textquoteright}importance de l{\textquoteright}implantation d{\textquoteright}ouvrage de retenue dans le bassin est de minimiser le ph{\'e}nom{\`e}ne d{\textquoteright}envasement, de r{\'e}guler le d{\'e}bit d{\textquoteright}{\'e}coulement et de contribuer {\`a} l{\textquoteright}irrigation de la plaine ainsi que l{\textquoteright}alimentation des briqueteries. L{\textquoteright}objectif de cette approche, est la mobilisation des ressources en eaux superficielles d{\'e}cid{\'e}e par l{\textquoteright}{\'e}tat en vue d{\textquoteright}une utilisation rationnelle et planifi{\'e}e de ce facteur vital qui et l{\textquoteright}eau.},
	url = {https://www.researchgate.net/publication/330038879_Geological_Hydrological_and_Hydrogeological_Characterization_of_the_Timgad{\textquoteright}s_Basin_Aures_Algeria_ne_for_the_Mobilization_of_Water_Resources},
	author = {DJAIZ Fouad and Defaflia N and Brinis Nafaa and ATHAMENA Ali and Marmi R}
}
@article {1894,
	title = {L\&rsquo;{\'e}tude des caract{\'e}ristiques hydrodynamiques et la vuln{\'e}rabilit{\'e} de la plaine alluvionnaire de Ksar Belezma (Batna - nord-est Alg{\'e}rien), ISSN 1112-3680,Juin 2016},
	journal = {Larhyss Journal},
	number = {n{\textdegree}26},
	year = {2016},
	pages = {pp. 237-247},
	abstract = {The cartography of the vulnerability in the pollution of subterranean waters allows identifying zones with high risk of contamination who takes into account the major part of the hydrogeological factors which allocate and control the  Mansouri Z.\&amp; al. / Larhyss Journal, 26(2016), 237-247238flow of subterranean waters: the depth of the water, the refill.These factors are represented by weights and quotations which depend respectively on their relative importance and on local hydrogeological conditions.The overall of the weights and the quotations of the diverse parameters and in a numerical value which is the indication Drastic. The cartography of the indication of vulnerability bases on the overlapping of 7 indexed cards. },
	url = {https://www.asjp.cerist.dz/en/article/55339},
	author = {Mensouri Z and MENANI Mohamed redha}
}
@proceedings {4900,
	title = {Les instabilit{\'e}s de terrain le long de la route nationale N\&deg;9 S{\'e}tif-Bejaia N.E Alg{\'e}rien},
	journal = {2 {\`e}me s{\'e}minaire national sur les g{\'e}orisques Jijel, 17 et 18 Novembre 2015},
	year = {2015},
	author = {Djenba Samir}
}
@article {4891,
	title = {Cartographie de la vuln{\'e}rabilit{\'e} de l\&rsquo;aquif{\`e}re alluvionnaire de T{\'e}bessa-Morsott. Est Alg{\'e}rien, ISSN 1112-3680},
	journal = {LARHYSS Journal},
	number = {N{\textdegree}22},
	year = {2015},
	pages = {pp.35-48},
	abstract = {Comme dans toutes les r{\'e}gions de l{\textquoteright}Afrique du Nord, notamment du Maghreb,la r{\'e}gion du grand bassin M{\'e}ll{\`e}gue a connu au cours des vingt derni{\`e}res ann{\'e}esune s{\'e}cheresse tr{\`e}s intense et persistante. Cette s{\'e}cheressea {\'e}t{\'e} caract{\'e}ris{\'e}e parun d{\'e}ficit pluviom{\'e}trique consid{\'e}rable et a eu un impact tr{\`e}s n{\'e}gatif sur lesr{\'e}gimes d{\textquoteright}{\'e}coulement des oueds et des sources et sur l{\textquoteright}alimentation des nappesaquif{\`e}res. Ce d{\'e}ficit hydro pluviom{\'e}trique s{\textquoteright}est r{\'e}percut{\'e} sur l{\textquoteright}ensemble desactivit{\'e}s socio-{\'e}conomiques de cette r{\'e}gion surtout sur son d{\'e}veloppementagricole. Par ailleurs ce ph{\'e}nom{\`e}ne a eu ainsi un impact {\'e}cologique end{\'e}gradant, en g{\'e}n{\'e}rale, l{\textquoteright}environnementet en favorisant notamment, lapollution des eaux et le d{\'e}p{\'e}rissement du milieu naturel. Pour cela, il estimportant de mettre en place une politique qui permettraitd{\textquoteright}une partd{\textquoteright}accro{\^\i}trenos ressources en eauet de les prot{\'e}ger d{\textquoteright}autre part.Dans le but de localiser les zones vuln{\'e}rables {\`a} la pollution et leurs origines, descampagnes d{\textquoteright}{\'e}chantillonnage d{\textquoteright}eaux et desmesures pi{\'e}zom{\'e}triques ont {\'e}t{\'e}r{\'e}alis{\'e}es pendant les p{\'e}riodes des Hautes et Basses Eaux des ann{\'e}es 2005,2006. L{\textquoteright}indice de contamination calcul{\'e} nous a permis de dresser des cartes devuln{\'e}rabilit{\'e} sur lesquelles on a distingu{\'e} trois zones {\`a} degr{\'e} de contaminationcroissant.},
	url = {http://archives.univ-biskra.dz/bitstream/123456789/2888/1/4.Seghir_Karima.pdf},
	author = {Drias Tarek and Toubal Ahmed Ch{\'e}rif}
}
@article {4890,
	title = {Approche Hydrochimique De L\&rsquo;aquifere Superficiel De Ain Djacer. Est Algerien  SSN 1112-3680},
	journal = {LARHYSS Journal },
	volume = {Volume 12},
	number = {N{\textdegree}24},
	year = {2015},
	pages = {pp. 281-299},
	abstract = {La r{\'e}gion de Ain Djacer est le si{\`e}ge d{\textquoteright}un aquif{\`e}re superficiel qui se trouve dans les alluvions du Mio-Plio-Quaternaire. Cette nappe qui a pour substratum les argiles et les marnes gypseuses du Mioc{\`e}ne, est entour{\'e}e par les calcaires du Cr{\'e}tac{\'e} qui constituent une limite {\`a} potentiel impos{\'e}. Il s{\textquoteright}agit d{\textquoteright}un synclinal combl{\'e} par les s{\'e}diments du Mio-Plio-Quaternaire o{\`u} tous les {\'e}coulements convergent vers le centre de la plaine. L{\textquoteright}exploitation intensive des ressources en eaux souterraines de la r{\'e}gion a largement influenc{\'e} le fonctionnement hydrodynamique et hydrochimique de cette nappe. Ceci a induit une baisse du niveau statique et une min{\'e}ralisation des eaux souterraines. Afin de mettre en {\'e}vidence l{\textquoteright}effet de cette situation sur la qualit{\'e} des eaux souterraines, une {\'e}tude hydrog{\'e}ochimique a {\'e}t{\'e} men{\'e}e. Cette {\'e}tude a montr{\'e} que le faci{\`e}s est bicarbonat{\'e} calcique pr{\`e}s des calcaires et chlorur{\'e} sodique au centre de la plaine en liaison avec la lithologie. L{\textquoteright}analyse thermodynamiques a montr{\'e} que les principaux ph{\'e}nom{\`e}nes g{\'e}ochimiques intervenant dans l{\textquoteright}acquisition de la charge saline sont li{\'e}s {\`a} l{\textquoteright}interaction eau-roche (dissolution des min{\'e}raux carbonat{\'e}s et {\'e}vaporitiques), {\`a} l{\textquoteright}{\'e}change cationique et {\`a} la concentration le long de l{\textquoteright}{\'e}coulement},
	url = {http://www.univ-tebessa.dz/fichiers/univ-batna/344-1161-1-PB.pdf},
	author = {Djenba Samir and Boudoukha Abderrahmane and BENCER}
}
@mastersthesis {2521,
	title = {Etude hydrog{\'e}ologique de la plaine de Balezma. BAtna},
	year = {2015},
	author = {Boudour Nassima}
}
@mastersthesis {2453,
	title = {Contribution {\`a} l\&$\#$39;{\'e}tude hydrochimique des eaux de la nappe phr{\'e}atique d\&$\#$39;oued souf et d{\'e}tection d\&$\#$39;{\'e}ventuelles traces de pollution},
	year = {2015},
	author = {Ghori S and Henka A~}
}
@mastersthesis {2452,
	title = {Contribution a l\&rsquo;{\'e}tude hydrogeologique de la nappe du complexe terminal  de la vall{\'e}e nord  d\&rsquo;oued Righ.},
	year = {2015},
	author = {Hamidi. N and Hamidi}
}
@proceedings {2429,
	title = {Les instabilit{\'e}s de terrain le long de la route nationale N\&deg;9 S{\'e}tif-Bejaia N.E Alg{\'e}rien},
	journal = {2 {\`e}me s{\'e}minaire national sur les g{\'e}orisques Jijel, 17 et 18 Novembre},
	year = {2015},
	author = {Djenba Samir and Boudoukha Abderahmane and Belkhiri Chettah Badani}
}
@proceedings {2428,
	title = {Hydrochemical characterization of alluvial aquifer of Tebessa- Morsott - Eastern Algeria},
	journal = {2nd International Scientific Conference on Applied Sciences and Engineering. 16-17 February, Dubai, United Arab Emirates. },
	year = {2015},
	author = {Drias Tarek}
}
@proceedings {2427,
	title = {Effect of the salinity on water for irrigation in the upper valley of Oued Rhumel - Eastern Algeria},
	journal = {International conference of Desalination for clean water and energy - Salinity gradient power session. 10 -14 May, Palermo, Italy. },
	year = {2015},
	author = {khadidja A and Boudoukha Abderahmane and Drias Tarek}
}
@proceedings {2424,
	title = {Effect of the salinity on water quality of the alluvial aquifer of Tebessa-Morsott - Eastern Algeria},
	journal = { International conference of Desalination for clean water and energy - Salinity gradient power session. 10 -14 May, Palermo, Italy },
	year = {2015},
	address = {Palermo, Italy },
	author = {Drias Tarek and khadidja A}
}
@article {2330,
	title = {Impact de la mobilisation des ressources hydriques dans les zones semi arides sur le d{\'e}veloppement durable, Cas du bassin de Timgad, Alg{\'e}rie, ISSN 2052-3408},
	journal = {International Journal of Environment \& Water },
	volume = {Volume 4},
	number = {Num{\'e}ro 2},
	year = {2015},
	pages = {pp 118-123},
	abstract = {La retenue collinaire est un ouvrage destin{\'e} g{\'e}n{\'e}ralement {\`a} am{\'e}liorer une agricultureexistante par l{\textquoteright}irrigation de petits p{\'e}rim{\`e}tres et par cons{\'e}quent am{\'e}liorer les terres irrigu{\'e}es,elle peut avoir d{\textquoteright}autres objectifs.L{\textquoteright}{\'e}tude de faisabilit{\'e} de tout terrain (r{\'e}gion) restefondamentale avant d{\textquoteright}entreprendre tout projet de recherche appliqu{\'e}e. Notre travailpropos{\'e} rev{\^e}t une importance socio-{\'e}conomique pour la r{\'e}gion de Timgad. Les r{\'e}sultats de ce travail constituent un apport scientifique utilisable aussi bien par les op{\'e}rateurs socio-{\'e}conomiques que les d{\'e}cideurs pour tout plan d{\textquoteright}am{\'e}nagement. Dans la r{\'e}gion {\'e}tudi{\'e}e, Les ressources hydriques sont en {\'e}troite relation avec les formations g{\'e}ologiques de la r{\'e}gion, donc l{\textquoteright}analyse de ces derniers est primordial. L{\textquoteright}objectif principal de l{\textquoteright}implantation de la retenue de Foum Toub est de contribuer {\`a} l{\textquoteright}irrigation de la plaine de Foum Toub, de r{\'e}gulariser le d{\'e}bit de l{\textquoteright}Oued Foum Toub et de minimiser le ph{\'e}nom{\`e}ne d{\textquoteright}envasement du barrage de Koudiet Lemdaour. Pour cela, les sites retenus pour la construction de cet ouvrage sont repr{\'e}sent{\'e}s par un substratum imperm{\'e}able. Les mat{\'e}riaux meubles, favorable pour servir de zones d{\textquoteright}emprunt sont localis{\'e}s dans les d{\'e}pressions avoisinantes ainsi que les gr{\`e}s qui peuvent {\^e}tre utilis{\'e}s comme mat{\'e}riaux de construction de la digue.},
	url = {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},
	author = {ATHAMENA Ali and MENANI Mohamed redha and ATHAMENA Malika and DJAIZ Fouad}
}
@article {2329,
	title = {Establishment theoretical of recommendation fertilization guide of vegetable crops in Algeria: concept and validation, ISSN 2349-0837 },
	journal = {JOURNAL OF ADVANCES IN AGRICULTURE },
	volume = { Volume 5},
	number = {Num{\'e}ro  1},
	year = {2015},
	pages = {pp  606-620},
	abstract = {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/kg{\^a}{\texteuro}{\textbrokenbar}).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.},
	url = {https://www.researchgate.net/publication/284030914_Establishment_theoretical_of_recommendation_fertilization_guide_of_vegetable_crops_in_Algeria_concept_and_validation},
	author = {Sbih Mahtali and Bensid Zoubeir and Bounouara Zohra and DJAIZ Fouad and Ferrag Youcef}
}
@proceedings {2328,
	title = {Le bassin n{\'e}og{\`e}ne de Timgad : Pal{\'e}ocourants et s{\'e}dimentation (Alg{\'e}rie Nord-Orientale)},
	journal = {3{\'e}m{\'e} colloque international sur la G{\'e}ologie du Sahara  du 09 au 10 D{\'e}cembre 2015, Universit{\'e} Kasdi Merbah OUARGLA},
	year = {2015},
	author = {DJAIZ Fouad and Marmi Ramdane}
}
@proceedings {2327,
	title = {La mobilisation des ressources hydriques dans le bassin de Timgad (Aur{\`e}s, Alg{\'e}rie NE)},
	journal = {3{\'e}m{\'e} colloque international sur la G{\'e}ologie du Sahara  du 09 au 10 D{\'e}cembre 2015, Universit{\'e} Kasdi Merbah OUARGLA},
	year = {2015},
	author = {DJAIZ Fouad and Marmi Ramdane and Ayhamena Ali and Brinis Nafaa}
}
@proceedings {2149,
	title = {Etude des caract{\'e}ristiques hydrochimiques des eaux des sources de la partie nord du synclinal de Ghassira dans le massif des Aur{\`e}s dans l\&rsquo;atlas saharien. Alg{\'e}rie.},
	journal = {3eme colloque international sur la g{\'e}ologie du Sahara Alg{\'e}rien: Ressources min{\'e}rales, en hydrocarbures et en eaux, Ouargla, Alger},
	year = {2015},
	address = {Ouargla, Alger},
	author = {Brinis Nafaa and Brahmia Ali}
}
@proceedings {2062,
	title = {Approche hydrog{\'e}ologique du bassin n{\'e}og{\`e}ne de Timgad (nord-est alg{\'e}rien), 9-10 d{\'e}cembre 2015},
	journal = {3{\`e}me Colloque International sur la G{\'e}ologie du Sahara, Th{\`e}me III Eau \& Environnement, Ouargla},
	year = {2015},
	address = {Ouargla},
	author = {Lebchek. S and MENANI Mohamed redha}
}
@proceedings {2017,
	title = {Aspects quantitatifs et qualitatifs de la source de Chapuis (Tahabort) : impact sur l\&rsquo;aspect touristique de la r{\'e}gion de Tamanrasset, Ouargla, 9-10 d{\'e}cembre 2015.},
	journal = {3{\`e}me Colloque International sur la G{\'e}ologie du Sahara, Th{\`e}me III Eau \& Environnement},
	volume = {Volume 03},
	year = {2015},
	author = {Azizi Yacine and MENANI Mohamed redha and Boucenna Fatih and Cheref Nouar}
}
@article {2002,
	title = {Approche hydrochimique de l\&rsquo;aquif{\`e}re superficiel de ain djacer. Est alg{\'e}rien, D{\'e}cembre},
	journal = {Larhyss Journal },
	number = {n{\textdegree}24},
	year = {2015},
	pages = { pp 281-299},
	abstract = {
	
		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.\&nbsp;
	

},
	url = {http://larhyss.net/ojs/index.php/larhyss/article/view/344},
	author = {Djenba S and Boudoukha Abderahmane}
}
@article {2001,
	title = {Cartographie de la vuln{\'e}rabilit{\'e} de l\&rsquo;aquif{\`e}re alluvionnaire de T{\'e}bessa-Morsott. Est Alg{\'e}rien. ISSN 1112- 3680, June 2015},
	journal = {Larhyss journal },
	number = {n{\textdegree}22},
	year = {2015},
	pages = {pp 35-48},
	abstract = {
	
		
			Une nouvelle m{\'e}thodologie est propos{\'e}e pour la caract{\'e}risation de la vuln{\'e}rabilit{\'e} {\`a} la pollution des nappes d{\textquoteright}eau souterraine libres. Cette m{\'e}thodologie constitue une am{\'e}lioration de la m{\'e}thode DRASTIC, universellement utilis{\'e}e. La vuln{\'e}rabilit{\'e} {\`a} la pollution est bas{\'e}e uniquement sur les param{\`e}tres relatifs {\`a} la recharge, au sol (pente et nature) et {\`a} la zone non satur{\'e}e (faci{\`e}s et {\'e}paisseur) de l{\textquoteright}aquif{\`e}re, tandis que la m{\'e}thodologie propos{\'e} est\&nbsp; bas{\'e}e uniquement sur les param{\`e}tres propres {\`a} la zone satur{\'e}e.
		

		
			Cette m{\'e}thodologie a {\'e}t{\'e} appliqu{\'e}e au bassin de l{\textquoteright}oued Ksob situ{\'e} {\`a} l{\textquoteright}extr{\^e}me Est Alg{\'e}rien renfermant une nappe fortement sollicit{\'e}, qui s{\textquoteright}{\'e}tend sur environ 320 km{\texttwosuperior} d{\textquoteright}extension.
		

		
			Les r{\'e}sultats ont montr{\'e} que cette nappe est caract{\'e}ris{\'e}e par une vuln{\'e}rabilit{\'e} globalement moyenne {\`a} faible. Les champs captant d{\textquoteright}eau potable (produisant environ 400 l/s) sont par contre situ{\'e}s dans des secteurs de moyenne {\`a} forte vuln{\'e}rabilit{\'e} {\`a} la pollution, leur protection par des p{\'e}rim{\`e}tres de protection rapproch{\'e}e et {\'e}loign{\'e}e est recommand{\'e}e dans les plus brefs d{\'e}lais.
		
	

},
	url = {http://larhyss.net/ojs/index.php/larhyss/article/view/275},
	author = {Drias Tarek and Toubal Ahmed Ch{\'e}rif}
}
@article {1994,
	title = {Analyse statistique et g{\'e}ochimique de la Dynamique des param{\`e}tres physico-chimiques des Eaux souterraines du synclinal de ghassira Alg{\'e}rie orientale. ISSN 1112-3680, June 2015},
	journal = {Larhyss Journal},
	number = {n{\textdegree}22},
	year = {2015},
	pages = {pp 123-137},
	abstract = {This paper is about groundwater{\textquoteright}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\&nbsp;\&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{\textquoteright}s quality.\&nbsp; 80\% of analyzed samples are influenced by evaporate rocks (gypsum, halite{\textellipsis}) and 20\% by limestone. Many processes have generated these two classes and are relating, especially, with the rocks of aquifers.},
	url = {http://larhyss.net/ojs/index.php/larhyss/article/view/282},
	author = {Brinis Nafaa and Boudoukha Abderahmane and Hamel Ahmed}
}
@article {1986,
	title = {Impact de la mobilisation des ressources hydriques dans les zones semi arides sur le d{\'e}veloppement durable, Cas du bassin de Timgad, Alg{\'e}rie. ISSN 2052-3408},
	journal = {International Journal of Environment \& Water},
	volume = {Vol 4},
	number = {Issue 2},
	year = {2015},
	abstract = {La retenue collinaire est un ouvrage destin{\'e} g{\'e}n{\'e}ralement {\`a} am{\'e}liorer une agriculture existante par l{\textquoteright}irrigation de petits p{\'e}rim{\`e}tres et par cons{\'e}quent am{\'e}liorer les terres irrigu{\'e}es, elle peut avoir d{\textquoteright}autres objectifs. L{\textquoteright}{\'e}tude de faisabilit{\'e} de tout terrain (r{\'e}gion) reste fondamentale avant d{\textquoteright}entreprendre tout projet de recherche appliqu{\'e}e. Notre travail propos{\'e} rev{\^e}t une importance socio-{\'e}conomique pour la r{\'e}gion de Timgad. Les r{\'e}sultats de ce travail constituent un apport scientifique utilisable aussi bien par les op{\'e}rateurs socio-{\'e}conomiques que les d{\'e}cideurs pour tout plan d{\textquoteright}am{\'e}nagement. Dans la r{\'e}gion {\'e}tudi{\'e}e, Les ressources hydriques sont en {\'e}troite relation avec les formations g{\'e}ologiques de la r{\'e}gion, donc l{\textquoteright}analyse de ces derniers est primordial. L{\textquoteright}objectif principal de l{\textquoteright}implantation de la retenue de Foum Toub est de contribuer {\`a} l{\textquoteright}irrigation de la plaine de Foum Toub, de r{\'e}gulariser le d{\'e}bit de l{\textquoteright}Oued Foum Toub et de minimiser le ph{\'e}nom{\`e}ne d{\textquoteright}envasement du barrage de Koudiet Lemdaour. Pour cela, les sites retenus pour la construction de cet ouvrage sont repr{\'e}sent{\'e}s par un substratum imperm{\'e}able. Les mat{\'e}riaux meubles, favorable pour servir de zones d{\textquoteright}emprunt sont localis{\'e}s dans les d{\'e}pressions avoisinantes ainsi que les gr{\`e}s qui peuvent {\^e}tre utilis{\'e}s comme mat{\'e}riaux de construction de la digue. },
	url = {https://www.google.com/url?sa=t\&rct=j\&q=\&esrc=s\&source=web\&cd=4\&cad=rja\&uact=8\&ved=2ahUKEwjimLHa0cLgAhWGDewKHRXdAZQQFjADegQIBxAC\&url=http\%3A\%2F\%2Farmspark.msem.univ-montp2.fr\%2Fmedfriend\%2FHammamet2015\%2F8-ManEnvironment\%2FATHAMENA_article.doc\&usg=AOvVaw1},
	author = {ATHAMENA Ali and MENANI Mohamed redha and ATHAMENA Malika and DJAIZ Fouad}
}
@article {1905,
	title = {Evaluation du risque de conflit autour des eaux transfrontali{\`e}res du syst{\`e}me aquif{\`e}re du Sahara Septentrional (SASS)., ISSN 1112-3680, June 2015,},
	journal = { Larhyss Journal},
	number = {n{\textdegree}22},
	year = {2015},
	pages = {pp. 59-69},
	abstract = {Le SASS couvre une superficie d{\textquoteright}environ 1000000 km{\texttwosuperior}, ilest partag{\'e} parl{\textquoteright}Alg{\'e}rie, la Libye et la Tunisie. Il est situ{\'e} dans une zone hyper aride avec unerecharge actuelle minime mais un grand volume stock{\'e}, {\'e}valu{\'e} entre 20000 et31000 km3.Depuis 1970 {\`a} nos jours, l{\textquoteright}exploitation du SASS est pass{\'e}e de 0,6 {\`a}plus de2,5milliards m3/an., d{\textquoteright}o{\`u}desrisques majeursdesalinisation des eaux,der{\'e}duction de l{\textquoteright}art{\'e}sianisme,detarissement des exutoires naturels,debaisse dela pi{\'e}zom{\'e}trie,d{\textquoteright}augmentation des rabattements oud{\textquoteright}interf{\'e}rencesdesp{\'e}rim{\`e}tres de captageentre pays...Ce qui menace {\`a} terme la durabilit{\'e} dud{\'e}veloppement socio-{\'e}conomique engag{\'e} dans l{\textquoteright}ensemble de la zone.Pour parer aumieux {\`a} ces risques et surtout pour mieux s{\textquoteright}enpr{\'e}munir, unprocessus de coop{\'e}ration a {\'e}t{\'e} initi{\'e}depuis 1998sous l{\textquoteright}{\'e}gide de l{\textquoteright}observatoiredu Sahara septentrional(OSS)en partenariat avec les institutions en charge desressources en eau dans les 3 pays.L{\textquoteright}importance de cet immense r{\'e}servoir pour le d{\'e}veloppement de la zone SASSet la n{\'e}cessit{\'e} de sa gestion durable et concert{\'e}e a amen{\'e} {\`a} une entente pour son{\'e}tude enplusieurs phases: la caract{\'e}risation hydrog{\'e}ologique du syst{\`e}meaquif{\`e}re et sa mod{\'e}lisation, l{\textquoteright}identification des risques environnementaux etl{\textquoteright}inclusion de l{\textquoteright}aspect socio-{\'e}conomique dans des sc{\'e}narios de d{\'e}veloppement.Les ressources en eau du SASS sont tr{\`e}s faiblement renouvelables,environ1milliard dem3/an, vis-{\`a}-vis des pr{\'e}l{\`e}vements actuels estim{\'e}s {\`a} 2,5 milliards dem3/an. La prise en compte de cette donn{\'e}ea {\'e}t{\'e} d{\'e}terminante pour pousser lesscientifiques {\`a} {\'e}tablir la meilleure mod{\'e}lisation conceptuelle possible dusyst{\`e}me qui soit {\`a} m{\^e}me de permettre d{\textquoteright}envisager diff{\'e}rents sc{\'e}nariosd{\textquoteright}exploitation de la ressource tout en tenant compte des perspectives de d{\'e}veloppement socio-{\'e}conomique de chacun des 3 pays.Les donn{\'e}es actuelles, quoique rassurantes, ne signifient pas l{\textquoteright}inexistence, {\`a}court ou moyen terme, d{\textquoteright}un risque de conflit autour de ces eauxtransfrontali{\`e}res. En effet, le probl{\`e}me m{\'e}rite d{\textquoteright}{\^e}tre analys{\'e} {\`a} travers plusieursindicateurs qui ont un impact sur ce risque.L{\textquoteright}objectif de cette note est d{\textquoteright}{\'e}valuer le risque de conflit autour des eaux duSASS {\`a} travers un indice global exprim{\'e} num{\'e}riquement sur la base de lacombinaison de poids et de cotes de plusieurs indicateurs qui ont, directementou indirectement, un impact sur le risque de conflit.L{\textquoteright}indice global de risque de conflit obtenu pour le cas du SASS semble refl{\'e}tercorrectement la situation quiypr{\'e}vaut actuellement.La comparaison de cer{\'e}sultat avec ceux obtenus pour les eaux transfrontali{\`e}res du bassin du Jourdain(risque {\'e}lev{\'e}) et ceux du syst{\`e}me aquif{\`e}re du Guarani (risque faible), confortel{\textquoteright}{\'e}chelle des valeurs adopt{\'e}e dans cette m{\'e}thode d{\textquoteright}indexation num{\'e}rique.},
	url = {http://lab.univ-biskra.dz/Larhyss/images/pdf/JOURNAL\%C2\%B022/6.Menani.Gire.pdf },
	author = {MENANI Mohamed redha}
}
@article {1904,
	title = {Sinkholes stability assessment in Cheria area, NE Algeria, ISSN 1112-3680},
	journal = {Larhyss Journal},
	number = {n{\textdegree}21},
	year = {2015},
	pages = {pp. 123-132},
	abstract = {This research work deals with the problem of karst sinkhole collapse occurringin the last few years in Cheria area. This newly revealed phenomenon is of amajor constrain in land use planning and urbanization, it has become necessarytoassess the stability of these underground features before any planningoperation. Laboratory testing and field work were undertaken in order todetermine both intact rock and rock mass properties. All the rock mechanicstesting and measurement were undertaken according to the ISRMrecommendations.It has been found that under imposed loading, the stability of the karst cavitiesdepends on the geo-mechanical parameters (Rock Masse Rating; RMR,Geological Strength Index; GSI, and Young Modulus; E) of the host rock aswell as the depth and dimensions of the gallery. It increases with RMR, GSI, Eand depth and decreases as the cavity becomes wider. Furthermore, thecalculation results show that a ratio (roof thickness to gallery width) of 0.3 andmore indicate, a stable conditions.The results obtained in this work allow identifying and assessing the stability ofunderground karst cavities. The methodology followed in this paper can betaken as a road map in the establishment of a hazard map related to the studiedphenomenon. This map will be a useful tool for the future urban extensionplanning in Cherea area.},
	url = {http://larhyss.net/ojs/index.php/larhyss/article/view/258},
	author = {Azizi Yacine and Boumezbeur Abderrahmane and MENANI Mohamed redha and Boucenna Fatih}
}
@article {1903,
	title = {Pollution des eaux souterraines par le flux azot{\'e} sous un climat semi-aride, cas de la plaine septentrionale de Zana-Chott Saboun, Est alg{\'e}rien.},
	journal = {International Journal of Environment \& Water},
	volume = {Vol 3},
	number = {Issue 1},
	year = {2015},
	author = {ATHAMENA Ali and Boudoukha Abderahmane and MENANI Mohamed redha and Bilalite Halima}
}
@article {1897,
	title = {Impact de la mobilisation des ressources hydriques dans les zones semi- arides sur le d{\'e}veloppement durable, Cas du bassin de Timgad, Alg{\'e}rie nord oriental},
	journal = {International Journal of Environment and Water},
	volume = {Vol.2},
	number = {Issue 4},
	year = {2015},
	abstract = {
	La retenue collinaire est un ouvrage destin{\'e} g{\'e}n{\'e}ralement {\`a} am{\'e}liorer une agriculture existante par l{\textquoteright}irrigation de petits p{\'e}rim{\`e}tres et par cons{\'e}quent am{\'e}liorer les terres irrigu{\'e}es, elle peut avoir d{\textquoteright}autres objectifs. L{\textquoteright}{\'e}tude de faisabilit{\'e} de tout terrain (r{\'e}gion) reste fondamentale avant d{\textquoteright}entreprendre tout projet de recherche appliqu{\'e}e. Notre travail propos{\'e} rev{\^e}t une importance socio-{\'e}conomique pour la r{\'e}gion de Timgad. Les r{\'e}sultats de ce travail constituent un apport scientifique utilisable aussi bien par les op{\'e}rateurs socio-{\'e}conomiques que les d{\'e}cideurs pour tout plan d{\textquoteright}am{\'e}nagement. Dans la r{\'e}gion {\'e}tudi{\'e}e, Les ressources hydriques sont en {\'e}troite relation avec les formations g{\'e}ologiques de la r{\'e}gion, donc l{\textquoteright}analyse de ces derniers est primordial. L{\textquoteright}objectif principal de l{\textquoteright}implantation de la retenue de Foum Toub est de contribuer {\`a} l{\textquoteright}irrigation de la plaine de Foum Toub, de r{\'e}gulariser le d{\'e}bit de l{\textquoteright}Oued Foum Toub et de minimiser le ph{\'e}nom{\`e}ne d{\textquoteright}envasement du barrage de Koudiet Lemdaour. Pour cela, les sites retenus pour la construction de cet ouvrage sont repr{\'e}sent{\'e}s par un substratum imperm{\'e}able. Les mat{\'e}riaux meubles, favorable pour servir de zones d{\textquoteright}emprunt sont localis{\'e}s dans les d{\'e}pressions avoisinantes ainsi que les gr{\`e}s qui peuvent {\^e}tre utilis{\'e}s comme mat{\'e}riaux de construction de la digue. 

},
	url = {http://armspark.msem.univ-montp2.fr/medfriend/Hammamet2015/8-ManEnvironment/ATHAMENA_article.doc},
	author = {ATHAMENA Ali and MENANI Mohamed redha and ATHAMENA Malika and DJAIZ Fouad}
}
@article {4892,
	title = {Caract{\'e}risation g{\'e}ologique et g{\'e}otechnique des glissements de la ville de Bougaa. Est Alg{\'e}rien, ISSN 1112-3338},
	journal = {courrier de savoir },
	number = {N{\textdegree}18},
	year = {2014},
	pages = {pp.63-67},
	abstract = {La r{\'e}gion de Bougaa est affect{\'e}e par un glissement d{\'e}pla{\c c}ant un volume consid{\'e}rable de mat{\'e}riaux d{\'e}tritiques form{\'e}s par des colluvions, des {\'e}boulis {\`a} gros blocs et des {\'e}boulis de pente argilo-limoneux rouge{\^a}tre reposant sur un substratum imperm{\'e}able d{\textquoteright}argilite schisteuse. Ce glissement est fa{\c c}onn{\'e} dans des formations g{\'e}ologiques particuli{\`e}rement sensibles {\`a} ce type de mouvement {\`a} cause de l{\textquoteright}h{\'e}t{\'e}rog{\'e}n{\'e}it{\'e} de leurs faci{\`e}s, de l{\textquoteright}imperm{\'e}abilit{\'e} de certaines couches et de l{\textquoteright}effet de la tectonique cassante et de la karstification. Le but de cette {\'e}tude est de caract{\'e}riser ces glissements {\`a} l{\textquoteright}aide d{\textquoteright}outils g{\'e}ologiques, g{\'e}otechniques et g{\'e}omorphologiques. Le r{\^o}le des eaux d{\textquoteright}infiltration est primordial dans le d{\'e}clenchement de ces glissements o{\`u} la lithologie, la disposition structurale,le climat sont des facteurs favorables. La pr{\'e}sence de pentes \&gt; 20 \%, de sources {\'e}mergeant du r{\'e}servoir karstique de Guergour, cr{\'e}ant des zones humides qui permettent le d{\'e}clenchement du mouvement du sol dans cette r{\'e}gion.},
	url = {https://pdfs.semanticscholar.org/6e67/266c856297aafe31a4861faea99507a79ea9.pdf},
	author = {Boudoukha Abderrahmane and Djenba Samir and Jean-Sylvain Magagnosc}
}
@proceedings {4851,
	title = {Caract{\'e}risation g{\'e}ologique et apport de la g{\'e}ophysique pour la mobilisation des ressources hydriques dans le bassin de ain Djasser (Sud s{\'e}tifien, Algerie NE)},
	journal = {Colloque international Eau{\textendash}Soci{\'e}t{\'e}{\textendash}Climat{\textquoteright}2017 (ESC-2017)  Hammamet, Tunis},
	year = {2014},
	author = {ATHAMENA Ali}
}
@mastersthesis {2524,
	title = {Caract{\'e}risation hydrochimique de l\&rsquo;aquif{\`e}re alluvial de la plaine de Ain Djasser, Wilaya de Batna. M{\'e}moire de Master, Universit{\'e} Hadj Lakhdar, Batna},
	year = {2014},
	author = {Sellam H}
}
@mastersthesis {2523,
	title = {Suivi pi{\'e}zom{\'e}trique et essais de pompage dans la plaine d\&rsquo;Ain Djasser, Wilaya de Batna. M{\'e}moire de Master, Universit{\'e} Hadj Lakhdar, Batna - Encadreur principal.},
	year = {2014},
	author = {Fartas FZ}
}
@mastersthesis {2522,
	title = {Suivi pi{\'e}zom{\'e}trique et hydrochimie dans la plaine de Ain Djasser, Wilaya de Batna. M{\'e}moire de Master, Universit{\'e} Hadj Lakhdar, Batna .},
	year = {2014},
	author = {Mechri Ali}
}
@mastersthesis {2460,
	title = {Contribution {\`a} l\&rsquo;{\'e}tude g{\'e}ologique et g{\'e}otechnique du barrage d\&rsquo;oued mellague (T{\'e}bessa), digue et mat{\'e}riaux de construction.},
	year = {2014},
	author = {Tafrount A and Benmenzer L~}
}
@mastersthesis {2459,
	title = {Contribution {\`a} l\&rsquo;{\'e}tude g{\'e}ologique et g{\'e}otechnique du site du projet de la cimenterie BISKRIA, Biskra.},
	year = {2014},
	author = {Abid A and Benaldjia H~}
}
@mastersthesis {2456,
	title = {Fonctionnement de la station de traitement d\&rsquo;oued EL ATHMANIA (MILA) et la qualit{\'e} physico-chimique et bact{\'e}riologique des eaux en amont (brutes) et en avale (apr{\`e}s traitement).},
	year = {2014},
	author = {Bensakhria D}
}
@mastersthesis {2455,
	title = {Contribution {\`a} L\&rsquo;{\'e}tude de la qualit{\'e} physico-chimique des eaux Destin{\'e}es {\`a} l\&rsquo;AEP de la ville D\&rsquo;EL-OUED.},
	year = {2014},
	author = {Aya B~}
}
@mastersthesis {2454,
	title = {Contribution {\`a} l\&rsquo;{\'e}tude du fluor dans les eaux souterraines de la r{\'e}gion de Hassi Messaoud.},
	year = {2014},
	author = {Laabed C~}
}
@proceedings {2430,
	title = {Cartography of the vulnerability to pollution, Application to alluvial aquifer of Tebessa-Morsott - Eastern  Algeria },
	journal = {International Multidisciplinary Academic Conference 11 to 13 May, Paris, France },
	year = {2014},
	author = {Drias Tarek}
}
@proceedings {2414,
	title = {Risque de pollution des eaux souterraines de la plaine de Zana, Est Alg{\'e}rien},
	journal = {3{\'e}m{\'e} colloque international Eau-Climat, REGARD CROISES NORD- SUD] Ressources en Eau \& Changement Climatique en R{\'e}gion M{\'e}diterran{\'e}enne 21, 22 \& 23 Octobre },
	year = {2014},
	address = {Hammamet (Tunisie)},
	author = {ATHAMENA Ali and ATHAMENA Malika and DJAIZ Fouad}
}
@proceedings {2413,
	title = {caract{\'e}risation g{\'e}ologique, hydrologique et hydrog{\'e}ologique du bassin de timgad (Aur{\`e}s, Alg{\'e}rie NE),  pour la mobilisation des ressources hydrique},
	journal = {3{\'e}m{\'e} colloque international Eau-Climat, REGARD CROISES NORD- SUD] Ressources en Eau \& Changement Climatique en R{\'e}gion M{\'e}diterran{\'e}enne 21, 22 \& 23 Octobre Hammamet (Tunisie)},
	volume = {Vol. 5},
	number = {No. 1},
	year = {2014},
	address = { Hammamet (Tunisie)},
	author = {DJAIZ Fouad and ATHAMENA Ali and ATHAMENA Malika and Marmi Ramdane and Brinis Nafaa and MENANI Mohamed redha}
}
@proceedings {2299,
	title = {Conditions hydrog{\'e}ologiques et hydrochimiques de l\&rsquo;oasis de Tolga (Nord-Est Alg{\'e}rien). Ressources en eau \&amp; changements climatiques en r{\'e}gion m{\'e}diterran{\'e}enne},
	journal = { 3{\`e}me colloque international Eau-Climat{\textquoteright}2014 : REGARDS CROISES NORD-SUD. Hammamet (Tunisie), 21, 22 \& 23 Octobre},
	year = {2014},
	address = {Hammamet, Tunisie},
	author = {Zouaoui Siham and MENANI Mohamed redha and Bouabid Abd Ennasser and Naidji. A. N}
}
@proceedings {2298,
	title = {Etude de la salinit{\'e} des eaux souterraines dans les zones arides Cas de l\&rsquo;aquif{\`e}re d\&rsquo;El-Outaya R{\'e}gion Nord ouest de Biskra  \&ndash; Algerie.},
	journal = {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},
	year = {2014},
	address = {Amman Jordan},
	author = {Brinis Nafaa and Boudoukha Abderahmane and DJAIZ Fouad}
}
@proceedings {2068,
	title = {Evaluation of the groundwater vulnerability to pollution of the Ksar Belezma aquifer (Algeria Northeast). September 2014},
	journal = {IAHS Conference, Marrakech, Morocco},
	year = {2014},
	address = {Marrakech, Morocco},
	author = {Mansouri Zineb and MENANI Mohamed redha}
}
@proceedings {2067,
	title = {Hydrogeologic study of Bouzina watershed (Algeria Northeast). September 2014.},
	journal = {IAHS Conference, Marrakech, Morocco},
	year = {2014},
	address = {Marrakech, Morocco},
	author = {Rihani A and MENANI Mohamed redha}
}
@proceedings {2066,
	title = {Caract{\'e}risation g{\'e}ologique, hydrologique et hydrog{\'e}ologique du bassin de timgad (Aur{\`e}s, Alg{\'e}rie NE), pour la mobilisation des ressources hydrique},
	journal = {3{\'e}m{\'e} colloque international Eau-Climat, REGARD CROISES [NORD- SUD] Ressources en Eau \& Changement Climatique en R{\'e}gion M{\'e}diterran{\'e}enne Hammamet (Tunisie)},
	year = {2014},
	address = { Hammamet (Tunisie)},
	author = {DJAIZ Fouad and ATHAMENA Ali and ATHAMENA Malika and Marmi Ramdane and MENANI Mohamed redha}
}
@proceedings {2065,
	title = {Conditions hydrog{\'e}ologiques et hydrochimiques de l\&rsquo;oasis de Tolga (Nord-Est Alg{\'e}rien). Ressources en eau \&amp; changements climatiques en r{\'e}gion m{\'e}diterran{\'e}enne. 21, 22 \&amp; 23 Octobre},
	journal = {3{\`e}me colloque international Eau-Climat: REGARDS CROISES NORD-SUD. Hammamet (Tunisie)},
	year = {2014},
	address = {Hammamet (Tunisie)},
	author = {Zouaoui Siham and MENANI Mohamed redha and Bouabid AN and Nadji R}
}
@proceedings {2064,
	title = {Analysis of the risk of conflict around the transboundary water resources of the Northern Saharian Aquifer System (NSAS). 19-21 November},
	journal = {GEOMATE international conference, Brisbane, Australia },
	year = {2014},
	address = {Brisbane, Australia, },
	author = {MENANI Mohamed redha}
}
@proceedings {2063,
	title = {Les eaux transfrontali{\`e}res du Syst{\`e}me Aquif{\`e}re du Sahara Septentrional (SASS) : Estimation du risque de conflit. 21-23 Octobre 2014.},
	journal = {3rd International conference Eau-Climat 2014, Hammamet, Tunisie},
	year = {2014},
	address = {Hammamet, Tunisie},
	author = {MENANI Mohamed redha}
}
@article {2003,
	title = {Caract{\'e}risation g{\'e}ologique et g{\'e}otechnique des glissements de la ville de Bougaa. Est alg{\'e}rien, Mars 2014},
	journal = {Courrier du Savoir},
	number = {N{\textdegree}18},
	year = {2014},
	pages = {pp 63-67},
	abstract = {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\&gt; 20\%, emerging sources of karst reservoir Guergour, creating wetlands that allow triggering of ground motion in this region.},
	url = {https://www.google.dz/url?sa=t\&rct=j\&q=\&esrc=s\&source=web\&cd=1\&cad=rja\&uact=8\&ved=2ahUKEwi_xq7m78PgAhVGxYUKHd-NBXkQFjAAegQIABAC\&url=http\%3A\%2F\%2Frevues.univ-biskra.dz\%2Findex.php\%2Fcds\%2Farticle\%2Fview\%2F650\%2F604\&usg=AOvVaw18Us5RIOfsC2lfNU6ndlpe},
	author = {Djenba Samir and Boudoukha Abderahmane}
}
@article {1999,
	title = {Importance des ressources hydriques et leurs impacts sur le d{\'e}veloppement durable dans le bassin de Timgad (Alg{\'e}rie nord orientale), ISSN 2170-1318,D{\'e}cembre 2014},
	journal = {Journal of Arid And Environment (AJAE)},
	volume = {vol. 4},
	number = {n{\textdegree} 2},
	year = {2014},
	pages = {pp 78-87},
	abstract = {Located in the Aures mountains Foum Toub is characterized by an annual average rainfall of\&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.},
	url = {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},
	author = {DJAIZ Fouad and ATHAMENA Ali and ATHAMENA Malika}
}
@article {1989,
	title = {Etude de la salinit{\'e} des eaux souterraines dans les zones arides Cas de l\&rsquo;aquif{\`e}re d\&rsquo;El-Outaya R{\'e}gion Nord ouest de Biskra \&ndash; ALGERIE; ISSN 2052-3408,},
	journal = {International Journal of Environment \& Water },
	volume = {Vol 3},
	number = {Issue 1},
	year = {2014},
	abstract = {Le bassin d{\textquoteright}El-Outaya se trouve dans la wilaya de BISKRA, une zone aride au sud alg{\'e}rien {\`a} environ 500 Km au sud de la capital Alger. Il constitue une ressource importante pour l{\textquoteright}eau d{\textquoteright}irrigation en plus d{\textquoteright}un barrage {\`a} l{\textquoteright}amont. La population de la plaine d{\'e}passe 11 000 habitants, leur activit{\'e} principale est l{\textquoteright}agriculture.La plaine {\'e}tudi{\'e}e correspond {\`a} un bassin subsident orient{\'e} sensiblement E.NE {\textendash} W.SW et situ{\'e} entre deux anticlinaux. Il se trouve au nord de l{\textquoteright}anticlinal du Dj.Bou Rhezel (Biskra) et au sud du d{\^o}me de Dj. El Melah. Il a fonctionn{\'e} comme un bassin de s{\'e}dimentation pendant tout le N{\'e}og{\`e}ne. Il est constitu{\'e} {\`a} la base par un mioc{\`e}ne laguno-marin, recouvert par du messinien (pontien) gr{\'e}seux fluviatile, puis par des poudingues plioc{\`e}nes. Les termes sup{\'e}rieurs, plus particuli{\`e}rement plioc{\`e}nes, sont fortement inclin{\'e}s vers le centre du bassin o{\`u} ils disparaissent sous une {\'e}paisseur consid{\'e}rable du Quaternaire.Le d{\'e}pouillement des analyses chimiques a aboutit {\`a} trois faci{\`e}s chimiques: Le faci{\`e}s chlorur{\'e} sodique, le faci{\`e}s sulfat{\'e} magn{\'e}sien et le faci{\`e}s sulfat{\'e} sodique.Le suivi des variables chimiques dominant selon les axes des {\'e}coulements souterrains permet de suivre l{\textquoteright}{\'e}volution des faci{\`e}s dans aquif{\`e}re ainsi que l{\textquoteright}origine de chaque faci{\`e}s.},
	url = {http://ijew.ewdr.org/component/k2/item/261-case-of-aquifer-of-el-outaya-north-west-of-biskra-algeria.html},
	author = {Brinis Nafaa and Boudoukha Abderahmane and DJAIZ Fouad}
}
@article {1969,
	title = {Modeling Groundwater Flow of the Mio-Pliocene Aquifer in the El-Outaya Plain, Biskra (Algeria) ISSN 2307-4531, (Print \&amp; Online).},
	journal = {International Journal of Sciences: Basic and Applied Research (IJSBAR)},
	volume = {Vol 17},
	number = {No 2 },
	year = {2014},
	abstract = {
	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.



	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.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.

},
	url = {https://www.google.com/url?sa=t\&rct=j\&q=\&esrc=s\&source=web\&cd=1\&cad=rja\&uact=8\&ved=2ahUKEwjcn76xvsLgAhWB2qQKHcRnCwAQFjAAegQIBBAC\&url=http\%3A\%2F\%2Fgssrr.org\%2Findex.php\%3Fjournal\%3DJournalOfBasicAndApplied\%26page\%3Darticle\%26op\%3Ddownload\%26path\%255B\%255D\%},
	author = {Boudjema Abderrezak and Hacini Messaoud and Guettaia Sabrine and Zahrouna Abderrezak and Baba Sy Lamine and Brinis Nafaa}
}
@article {1966,
	title = {Etude de la salinit{\'e} des eaux souterraines dans les zones arides Cas de l\&rsquo;aquif{\`e}re d\&rsquo;El-Outaya R{\'e}gion Nord ouest de Biskra \&ndash; ALGERIE, 2014. ISSN 2052-3408.},
	journal = { International Journal of Environment \& Water},
	volume = {Vol 3},
	number = {Issue 1},
	year = {2014},
	author = {Brinis Nafaa and Boudoukha Abderahmane and DJAIZ Fouad}
}
@article {1906,
	title = {Karst Sinkholes Stability Assessment in Cheria Area, NE Algeria. Geotechnical and Geological Engineering Review, April 2014},
	journal = {Springer},
	volume = {Volume 32},
	number = {Issue 2},
	year = {2014},
	pages = {pp 363-374},
	abstract = {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{\textendash}232, 2002)] 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.},
	url = {http://www.springerprofessional.de/karst-sinkholes-stability-assessment-in-cheria-area-ne-algeria/5004782.html },
	author = {Azizi Yacine and MENANI Mohamed redha and Hemila Med Laid and Boumezbeur Abderrahmane}
}
@article {1888,
	title = {Cartography of the vulnerability to pollution, Application to alluvial aquifer of Tabessa-Morsott - Eastern Algeria.},
	journal = {Review of strategic and international studies},
	volume = {Volume VI},
	number = {Number 1},
	year = {2014},
	pages = { pp 96-107.},
	author = {Drias Tarek}
}
@proceedings {2751,
	title = {Geological and geotechnical characteristics of the soils in the region of Setif },
	journal = {publication internationale European scientific journal},
	year = {2013},
	author = {Djenba Samir and Boudoukha Abderahmane}
}
@proceedings {2750,
	title = {Geological and geotechnical characteristics of the soils in the region of Setif},
	journal = {~1 st annuel international interdiscplinary conference avril Azores Portugal},
	year = {2013},
	author = {Djenba Samir}
}
@proceedings {2713,
	title = {Lithostratigraphie des calcaires aptien du Dj Bouroumane (Algerie oriental nord)},
	year = {2013},
	author = {Bentahar Fahima}
}
@proceedings {2712,
	title = {Accident probablement responsable de la pr{\'e}sence des sources thermales, Cas de la source thermale de Guergima, Batna Est Alg{\'e}rien},
	journal = {The 5th Tunisian days of Applied Geology.JTGA. 2013. International Conference of Applied geology and Geomatics. ICNHG, 2013. Hammamet, Tunisia 17-20 May},
	year = {2013},
	author = {ATHAMENA Ali and ATHAMENA Malika and DJAIZ Fouad}
}
@proceedings {2711,
	title = {La contribution de la g{\'e}ophysique dans les {\'e}tudes thermales, cas des sources des monts des Aures},
	journal = {Colloque International sur les applications g{\'e}ophysiques de Sub surface {\textendash} CIAGS- 26 27 Octobre 2013. Laboratoire de g{\'e}ologie et d{\textquoteright}environnement/ FSTGAT/Uni. De Constantine 1},
	year = {2013},
	author = {ATHAMENA Ali and ATHAMENA Malika and DJAIZ Fouad}
}
@proceedings {2710,
	title = {G{\'e}othermie des eaux souterraines cas de la source thermale de Guergima, Batna est-alg{\'e}rien },
	journal = {S{\'e}minaire international sur  l{\textquoteright}hydrog{\'e}ologie et l{\textquoteright}environnement SIHE 2013, Ouargla 5-7 Novembre },
	year = {2013},
	author = {ATHAMENA Ali and ATHAMENA Malika and DJAIZ Fouad}
}
@proceedings {2709,
	title = {Importance de la mobilisation des ressources hydriques et l\&rsquo;impact sur le d{\'e}veloppement durable dans le bassin de Timgad Alg{\'e}rie nord orientale},
	journal = {The 5th Tunisian days of Applied Geology.JTGA. 2013. International Conference of Applied geology and Geomatics. ICNHG, 2013. Hammamet, Tunisia 17-20 May},
	year = {2013},
	author = {DJAIZ Fouad and ATHAMENA Malika and ATHAMENA Ali}
}
@proceedings {2708,
	title = {Risque naturel li{\'e}e au mouvements des terrains affaissables dans une zone urbaine \&ndash;Batna},
	journal = {The 5th Tunisian days of Applied Geology.JTGA. 2013. International Conference of Applied geology and Geomatics. ICNHG, 2013. Hammamet, Tunisia 17-20 May},
	year = {2013},
	author = {DJAIZ Fouad and Marmi Ramdane and BOUMEZBEUR A}
}
@proceedings {2706,
	title = {L\&rsquo;apport de la g{\'e}ophysique {\`a} la g{\'e}om{\'e}trie des couches profondes et les aquif{\`e}res potentiels du bassin de timgad (Atlas Saharien Alg{\'e}rien Oriental)},
	journal = {2{\`e}me Colloque International sur La Gestion Int{\'e}gr{\'e}e des Ressources en Eau GIRE{\textquoteright}2013 22-23 Octobre 2013/ / D{\'e}p. Sc. de la Terre et de l{\textquoteright}Univers / Facult{\'e} des Sciences - Universit{\'e} Hadj Lakhdar - Batna},
	year = {2013},
	author = {DJAIZ Fouad and Brinis Nafaa and Inal Ahmed and Marmi Ramdane and MENANI Mohamed redha}
}
@proceedings {2705,
	title = {Les mouvements des sols,G{\'e}orisques et Urbanisation},
	journal = {2{\`e}me Colloque International sur La Gestion Int{\'e}gr{\'e}e des Ressources en Eau GIRE{\textquoteright}2013 22-23Octobre 2013/ / D{\'e}p. Sc. de la Terre et de l{\textquoteright}Univers / Facult{\'e} des Sciences - Universit{\'e} Hadj Lakhdar {\textendash} Batna},
	year = {2013},
	author = {DJAIZ Fouad and BOUMEZBEUR A and Marmi Ramdane and ATHAMENA Ali and MENANI Mohamed redha}
}
@mastersthesis {2529,
	title = {Contribution {\`a} l\&rsquo;{\'e}tude hydrog{\'e}ologique de la plaine de Tadjenent. Wilaya de Mila. M{\'e}moire de Master, Universit{\'e} Hadj Lakhdar, Batna},
	year = {2013},
	author = {Mohamedi A}
}
@mastersthesis {2528,
	title = {Caract{\'e}risation hydrodynamique de l\&rsquo;aquif{\`e}re alluvial de la plaine de Ain Djasser, Wilaya de Batna. M{\'e}moire de Master, Universit{\'e} Hadj Lakhdar, Batna},
	year = {2013},
	author = {Mensouri. Z}
}
@mastersthesis {2527,
	title = {Qualit{\'e} des eaux du barrage de Koudiet Medaouer et aptitude {\`a} l\&rsquo;irrigation des terres agricoles de la plaine de chemora. M{\'e}moire de Master, Universit{\'e} Hadj Lakhdar},
	year = {2013},
	author = {Maache T}
}
@mastersthesis {2526,
	title = {Caract{\'e}risation hydrochimique de l\&rsquo;aquif{\`e}re alluvial de la plaine de Zana, Wilaya de Batna. M{\'e}moire de Master, Universit{\'e} Hadj Lakhdar, Batna},
	year = {2013},
	author = {Bilalite Halima}
}
@mastersthesis {2525,
	title = {Caract{\'e}risation hydrodynamique de l\&rsquo;aquif{\`e}re alluvial de la plaine de Zana, Wilaya de Batna. M{\'e}moire de Master, Universit{\'e} Hadj Lakhdar, Batna},
	year = {2013},
	author = {Labchek S}
}
@mastersthesis {2462,
	title = {Etude de la stabilit{\'e} de la digue du barrage Bouzina. Univ Batna},
	year = {2013},
	author = {Bouzzafa A and Benyekken D~}
}
@mastersthesis {2461,
	title = {Contribution {\`a} l\&rsquo;{\'e}tude g{\'e}ologique et g{\'e}otechnique du barrage Tabellout. Univ de Batna},
	year = {2013},
	author = {Zkara Ibtissem and Snina S}
}
@mastersthesis {2458,
	title = {Fonctionnement de la station de traitement de Timgad (W) de Batna et {\'e}tude de la qualit{\'e} physic-chimique des eaux en amont et en aval. Univ de Batna.},
	year = {2013},
	author = {Selem R}
}
@mastersthesis {2457,
	title = {Fonctionnement de la STEP d\&rsquo;oued Souf et l\&rsquo;{\'e}tude de l\&rsquo;effluent en amont et en aval.},
	year = {2013},
	author = {Zid.G}
}
@proceedings {2442,
	title = {Cartographie de la vuln{\'e}rabilit{\'e} {\`a} la pollution de la nappe alluviale de T{\'e}bessa-Morsott (BV d\&rsquo;oued ksob), extr{\^e}me Est Alg{\'e}rie},
	journal = {2{\`e}me colloque international sur la gestion int{\'e}gr{\'e}e des ressources en eau. 22-23 Octobre 2013. Batna. Alg{\'e}rie},
	year = {2013},
	author = {Drias Tarek}
}
@proceedings {2415,
	title = {Le Bassin n{\'e}og{\`e}ne de Timgad et son aspect structural (atlas saharien alg{\'e}rien oriental)},
	journal = {3eme colloque international. Les g{\'e}osciences au service du DEVELOPPEMENT DURABLE. 20-21 NOVEMBRE, TEBESSA {\textendash}ALGERIE},
	year = {2013},
	address = {TEBESSA {\textendash}ALGERIE},
	author = {DJAIZ Fouad and Marmi Ramdane}
}
@proceedings {2303,
	title = {Etude hydrog{\'e}ologique de l\&rsquo;\&rsquo;oasis de Tolga (R{\'e}gion de Biskra, NE Alg{\'e}rien). Modes d\&rsquo;exploitations des r{\'e}serves et incidences de l\&rsquo;usage agricole},
	journal = {2{\`e}me colloque international sur la gestion int{\'e}gr{\'e}e des ressources en Eau ; GIRE{\textquoteright}2013. Batna (Alg{\'e}rie), 22 et 23 Octobre},
	year = {2013},
	author = {Zouaoui Siham and MENANI Mohamed redha}
}
@proceedings {2302,
	title = {Etude des faci{\`e}s chimiques des eaux souterraines de la plaine  d\&rsquo;El-Outaya  au sud alg{\'e}rien. Types et {\'e}volution dans l\&rsquo;espace aquif{\`e}re},
	journal = {The 5th Tunisian Days of Applied Geology -- Hammamet, Tunisie, May 17th - 19th},
	year = {2013},
	author = {Brinis Nafaa and Boudoukha Abderahmane and DJAIZ Fouad}
}
@proceedings {2301,
	title = {Etude du ph{\'e}nom{\`e}ne d\&rsquo;eutrophisation dans les eaux du barrage de Koudiet Medouar, Timgad, Wilaya de Batna (Est \&ndash; Alg{\'e}rien)},
	journal = {2{\`e}me Colloque International sur La Gestion Int{\'e}gr{\'e}e des Ressources en Eau GIRE{\textquoteright}2013 22-23 Octobre / D{\'e}p. Sc. de la Terre et de l{\textquoteright}Univers / Facult{\'e} des Sciences - Universit{\'e} Hadj Lakhdar - Batna.},
	year = {2013},
	author = {Brinis Nafaa}
}
@proceedings {2300,
	title = {L\&rsquo;apport de la g{\'e}ophysique a la g{\'e}om{\'e}trie des couches profondes et les aquif{\`e}res potentiels du bassin de timgad (Atlas Saharien Alg{\'e}rien Oriental)},
	journal = {2{\`e}me Colloque International sur La Gestion Int{\'e}gr{\'e}e des Ressources en Eau GIRE{\textquoteright}2013 22-23 Octobre / D{\'e}p. Sc. de la Terre et de l{\textquoteright}Univers / Facult{\'e} des Sciences - Universit{\'e} Hadj Lakhdar - Batna},
	year = {2013},
	author = {DJAIZ Fouad and Brinis Nafaa and Inal Ahmed and Marmi Ramdane and MENANI Mohamed redha}
}
@proceedings {2078,
	title = {Aper{\c c}u sur les ressources en eau souterraines du bassin versant d\&rsquo;Oued Labiod (Massif des Aur{\`e}s). Com},
	journal = {Poster GIRE },
	year = {2013},
	address = {Batna},
	url = {http://gire-batna.netai.net/GIRE2013/gire2013.html },
	author = {Rihani A and MENANI Mohamed redha}
}
@proceedings {2077,
	title = {Apport de la mod{\'e}lisation g{\'e}ologique 3D dans la compr{\'e}hension du mode de fonctionnement des sources d\&$\#$39;eau de la terminaison p{\'e}riclinale orientale du grand pli atlasique du Ravin Bleu (NE alg{\'e}rien). Cas de la source de Djerma. Com},
	journal = {Poster GIRE, ID 913},
	year = {2013},
	address = {Batna},
	url = {http://gire-batna.netai.net/GIRE2013/Posters/ID\%20913.pdf },
	author = {Benagoune F and MENANI Mohamed redha}
}
@proceedings {2076,
	title = {Etude hydrog{\'e}ologique de l\&$\#$39;Oasis de Tolga (r{\'e}gion de Biskra - NE alg{\'e}rien). Mode d\&$\#$39;exploitation des r{\'e}serves et incidences de l\&$\#$39;usage agricole. Com},
	journal = {Poster GIRE, ID 666},
	year = {2013},
	address = {Batna},
	url = {http://gire-batna.netai.net/GIRE2013/Posters/ID\%20666.pdf },
	author = {Zouaoui Siham}
}
@proceedings {2075,
	title = {Etude hydrog{\'e}ologique de l\&rsquo;\&rsquo;oasis de Tolga (R{\'e}gion de Biskra, NE Alg{\'e}rien). Modes d\&rsquo;exploitations des r{\'e}serves et incidences de l\&rsquo;usage agricole. 22 et 23 Octobre 2013},
	journal = {2{\`e}me colloque international sur la gestion int{\'e}gr{\'e}e des ressources en Eau, GIRE, Batna (Alg{\'e}rie)},
	year = {2013},
	address = {Batna},
	author = {Zouaoui Siham and MENANI Mohamed redha}
}
@proceedings {2074,
	title = {L\&rsquo;apport de la g{\'e}ophysique a la g{\'e}om{\'e}trie des couches profondes et les aquif{\`e}res potentiels du bassin de timgad (Atlas Saharien Alg{\'e}rien Oriental). 22-23 Octobre 2013},
	journal = {2{\`e}me Colloque International sur La Gestion Int{\'e}gr{\'e}e des Ressources en Eau GIRE,D{\'e}p. Sc.de la Terre et de l{\textquoteright}Univers / Facult{\'e} des Sciences - Universit{\'e} Hadj Lakhdar - Batna},
	year = {2013},
	address = {Batna},
	author = {DJAIZ Fouad and Brinis Nafaa and Inal Ahmed and Marmi Ramdane and MENANI Mohamed redha}
}
@proceedings {2073,
	title = {Les mouvements des sols, G{\'e}orisques et Urbanisation. 2{\`e}me Colloque International sur La Gestion Int{\'e}gr{\'e}e des Ressources en Eau, 22-23 Octobre 2013},
	year = {2013},
	publisher = {GIRE, D{\'e}p. Sc. de la Terre et de l{\textquoteright}Univers / Facult{\'e} des Sciences - Universit{\'e} Hadj Lakhdar {\textendash} Batna. },
	author = {DJAIZ Fouad and BOUMEZBEUR A and Marmi Ramdane and ATHAMENA Ali and MENANI Mohamed redha}
}
@proceedings {2072,
	title = {KARST SINKHOLES STABILITY ASSESSMENT IN CHERIA AREA, NE ALGERIA. Com},
	journal = {Orale GIRE 2013 ID 514, Batna},
	year = {2013},
	address = { Batna},
	url = {http://gire-batna.netai.net/GIRE2013/Orales/ID\%20514.pdf },
	author = {AZIZI Y and BOUMEZBEUR A and MENANI Mohamed redha and Boucenna Fatih}
}
@proceedings {2071,
	title = {Evaluation du risque de conflit autour des eaux transfrontali{\`e}res du syst{\`e}me aquif{\`e}re du Sahara septentrional (SASS).  Com},
	journal = {Orale ID 921, GIRE, Batna},
	year = {2013},
	address = {Batna},
	url = {http://gire-batna.netai.net/GIRE2013/Orales/ID\%20921.pdf },
	author = {MENANI Mohamed redha}
}
@proceedings {2070,
	title = {The artificial recharge of the aquifers by considering the groundwater vulnerability to pollution. Com. 22 et 23 Octobre 2013.},
	journal = { Orale ID 919, GIRE, Batna},
	year = {2013},
	address = {Batna},
	url = {http://gire-batna.netai.net/GIRE2013/Orales/ID\%20919.pdf},
	author = {MENANI Mohamed redha}
}
@proceedings {2069,
	title = {Assessment of the risk of conflict around the transboundary water resources of the Northern Saharan Aquifer System. Com. 22-23 may},
	journal = {Orale IJAS conference,Toronto},
	year = {2013},
	address = {Toronto},
	author = {MENANI Mohamed redha}
}
@article {1995,
	title = {Qualit{\'e} des eaux souterraines dans l\&rsquo;Atlas saharien: Cas du bassin n{\'e}og{\`e}ne d\&rsquo;El-Outaya (Sud alg{\'e}rien), ISSN 2170-1318 Juin 2013,},
	journal = { Algerian Journal of Arid Environment {\textquotedblleft}AJAE{\textquotedblleft}},
	volume = {Volume 3},
	number = {num{\'e}ro 1},
	year = {2013},
	pages = {pp 89-97},
	abstract = {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. 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.\&nbsp; Evaporation in the area is very important and consumes the majority of the precipitations.\&nbsp; 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.\&nbsp; The analysis of groundwater samples indicates the presence in strong concentrations of Cl-, SO42-, Na+ and Mg2+.},
	url = {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},
	author = {Brinis Nafaa and Boudoukha Abderahmane}
}
@article {1990,
	title = {Le remplissage s{\'e}dimentaire du bassin de Timgad et aquif{\`e}res potentiels (atlas saharien Alg{\'e}rien oriental). ISSN 1813-548X.},
	journal = {Afrique SCIENCE },
	volume = {Vol 09},
	number = {Issue 3},
	year = {2013},
	pages = {pp 66{\textendash}76},
	abstract = {
	Le bassin de Timgad, orient{\'e} suivant une direction sub-latitudinale, appartient {\`a} l{\textquoteright}Atlas Saharien nord-oriental. Il est bord{\'e} au nord par Dj. Bou Arif-Dj. Fedjoudj-Dj. Tarf et au sud par les Monts des Aur{\`e}s.



	Il comprend un substratum m{\'e}sozo{\"\i}que correspondant {\`a} une s{\'e}rie marine gr{\'e}so-carbonat{\'e}e, surmont{\'e} en discordance par des formations du N{\'e}og{\`e}ne. Ces derniers sont repr{\'e}sent{\'e}s \&nbsp;essentiellement par des s{\'e}diments d{\'e}tritiques o{\`u} dominent les d{\'e}p{\^o}ts silicoclastiques. La puissance de toute la s{\'e}rie d{\'e}passe les 1000 m{\`e}tres. Le contact, entre les deux s{\'e}ries \&nbsp;lithostratigraphiques, m{\'e}sozo{\"\i}que et n{\'e}og{\`e}nes, est soulign{\'e} par une discordance majeure marqu{\'e}e tant{\^o}t par des conglom{\'e}rats polyg{\'e}niques, tant{\^o}t par des niveaux calcaires souvent gr{\'e}seux. Le Plio-Quaternaire, repr{\'e}sent{\'e} surtout par des s{\'e}diments d{\'e}tritiques grossiers, surmonte en discordance les s{\'e}ries ant{\'e}rieures.



	Du point de vue structurale, le bassin est affect{\'e} par une tectonique polyphas{\'e}e qui l{\textquoteright}a compartiment{\'e} en blocs dont les accidents transverses NW-SE et NE-SW sont nettement exprim{\'e}s. La phase compressive, situ{\'e}e {\`a} la limite plioc{\`e}ne-quaternaire, serait {\`a} l{\textquoteright}origine du model{\'e} du relief actuel.



	L{\textquoteright}{\'e}tude g{\'e}ophysique, consistant en l{\textquoteright}exploitation \&nbsp;des profils sismiques et des coupes g{\'e}o {\'e}lectriques, a permis de mettre en {\'e}vidence d{\textquoteright}une part la g{\'e}om{\'e}trie profonde des diff{\'e}rents accidents dans le bassin et les aquif{\`e}res potentiels d{\textquoteright}autre part. Une formation relativement r{\'e}sistante, correspond {\`a} un intervalle gr{\'e}seux du Mioc{\`e}ne, rev{\^e}t un int{\'e}r{\^e}t particulier sur le plan hydrog{\'e}ologique.

},
	url = {http://www.afriquescience.info/document.php?id=2929.},
	author = {DJAIZ Fouad and Brinis Nafaa and Marmi Ramdane}
}
@article {1970,
	title = {Le remplissage s{\'e}dimentaire du bassin de Timgad et aquif{\`e}res potentiels (Atlas saharien Alg{\'e}rien oriental)\&raquo;.1 septembre 2013, ISSN 1813-548X.},
	journal = { Afrique Science},
	volume = {Vol.09},
	number = { N{\textdegree}03},
	year = {2013},
	abstract = {
	Le bassin de Timgad, orient{\'e} suivant une direction sub-latitudinale, appartient {\`a} l{\textquoteright}Atlas Saharien nord-oriental. Il est bord{\'e} au nord par Dj. Bou Arif-Dj. Fedjoudj-Dj. Tarf et au sud par les Monts des Aur{\`e}s.



	Il comprend un substratum m{\'e}sozo{\"\i}que correspondant {\`a} une s{\'e}rie marine gr{\'e}so-carbonat{\'e}e, surmont{\'e} en discordance par des formations du N{\'e}og{\`e}ne. Ces derniers sont repr{\'e}sent{\'e}s \&nbsp;essentiellement par des s{\'e}diments d{\'e}tritiques o{\`u} dominent les d{\'e}p{\^o}ts silicoclastiques. La puissance de toute la s{\'e}rie d{\'e}passe les 1000 m{\`e}tres. Le contact, entre les deux s{\'e}ries \&nbsp;lithostratigraphiques, m{\'e}sozo{\"\i}que et n{\'e}og{\`e}nes, est soulign{\'e} par une discordance majeure marqu{\'e}e tant{\^o}t par des conglom{\'e}rats polyg{\'e}niques, tant{\^o}t par des niveaux calcaires souvent gr{\'e}seux. Le Plio-Quaternaire, repr{\'e}sent{\'e} surtout par des s{\'e}diments d{\'e}tritiques grossiers, surmonte en discordance les s{\'e}ries ant{\'e}rieures.



	Du point de vue structurale, le bassin est affect{\'e} par une tectonique polyphas{\'e}e qui l{\textquoteright}a compartiment{\'e} en blocs dont les accidents transverses NW-SE et NE-SW sont nettement exprim{\'e}s. La phase compressive, situ{\'e}e {\`a} la limite plioc{\`e}ne-quaternaire, serait {\`a} l{\textquoteright}origine du model{\'e} du relief actuel.



	L{\textquoteright}{\'e}tude g{\'e}ophysique, consistant en l{\textquoteright}exploitation \&nbsp;des profils sismiques et des coupes g{\'e}o {\'e}lectriques, a permis de mettre en {\'e}vidence d{\textquoteright}une part la g{\'e}om{\'e}trie profonde des diff{\'e}rents accidents dans le bassin et les aquif{\`e}res potentiels d{\textquoteright}autre part. Une formation relativement r{\'e}sistante, correspond {\`a} un intervalle gr{\'e}seux du Mioc{\`e}ne, rev{\^e}t un int{\'e}r{\^e}t particulier sur le plan hydrog{\'e}ologique.

},
	url = {http://www.afriquescience.info/document.php?id=2929.},
	author = {DJAIZ Fouad and Brinis Nafaa and Marmi R}
}
@proceedings {2715,
	title = {Etude g{\'e}ologique du bassin de Timgad},
	journal = {La G{\'e}ologie du Sahara: Ressources min{\'e}rales, en hydrocarbures et en eau ; 03, 04 et 05 D{\'e}cembre {\`a} l{\textquoteright}universit{\'e} KASDI Merbah-Ouargla},
	year = {2012},
	author = {DJAIZ Fouad and Brinis Nafaa}
}
@proceedings {2714,
	title = {Caract{\'e}risation g{\'e}ologique et hydrog{\'e}ologique du bassin de Timgad},
	journal = {La G{\'e}ologie du Sahara: Ressources min{\'e}rales, en hydrocarbures et en eau ; 03, 04 et 05 D{\'e}cembre {\`a} l{\textquoteright}universit{\'e} KASDI Merbah-Ouargla},
	year = {2012},
	author = {DJAIZ Fouad and Marmi Ramdane}
}
@mastersthesis {2530,
	title = {Cartographie g{\'e}otechnique du POS N\&deg; 08. N\&rsquo;gaous. Batna},
	year = {2012},
	author = {Kerboub A and Labchek S}
}
@mastersthesis {2464,
	title = {Caract{\'e}ristiques g{\'e}ologiques, hydrog{\'e}ologiques et g{\'e}otechniques de la localit{\'e} d\&rsquo;El-Hdeb (W) ouargla. Univ de Batna.},
	year = {2012},
	author = {Righat Z and Morghad B~}
}
@proceedings {2440,
	title = {analyse microfaciologique et d{\'e}coupage s{\'e}quentiel de la s{\'e}rie c{\'e}nomanienne de la coupe de Mennchar Ali Guera (nord-est Alg{\'e}rie)},
	journal = {La G{\'e}ologie du Sahara: Ressources min{\'e}rales, en hydrocarbures et en eau" ; 03, 04 et 05 D{\'e}cembre {\`a} l{\textquoteright}universit{\'e} KASDI Merbah-Ouargla },
	year = {2012},
	author = {Benmansour S and DJAIZ Fouad and Yahaoui Abedel Ouahab}
}
@proceedings {2309,
	title = {Mise en {\'e}vidence de la qualit{\'e} des eaux de la nappe alluviale de tebessa (Est alg{\'e}rien)},
	journal = {Troisi{\`e}me Forum de l{\textquoteright}eau, Tunisie 26 -28 mars },
	year = {2012},
	address = {Tunisie},
	author = {Bouchagoura I and Rouabhia A and Djabri Larbi and Brinis Nafaa}
}
@proceedings {2308,
	title = {Etude de la qualit{\'e} des eaux souterraines utilis{\'e}es pour l\&rsquo;irrigation de la plaine d\&rsquo;El-Outaya au sud Alg{\'e}rien},
	journal = {2eme colloque international sur la g{\'e}ologie du Sahara Alg{\'e}rien: Ressources min{\'e}rales, en hydrocarbures et en eaux, Ouargla, D{\'e}cembre },
	year = {2012},
	address = {Ouargla, Alger},
	author = {Brinis Nafaa and Boudoukha Abderahmane}
}
@proceedings {2307,
	title = {Etude de la qualit{\'e} chimique des eaux souterraines dans les Aur{\`e}s (Cas de la vall{\'e}e de l\&rsquo;oued Abiod), Alg{\'e}rie},
	journal = {2eme colloque international sur la g{\'e}ologie du Sahara Alg{\'e}rien: Ressources min{\'e}rales, en hydrocarbures et en eaux, Ouargla, D{\'e}cembre },
	year = {2012},
	address = {Ouargla, Alger},
	author = {Brinis Nafaa and Boudoukha Abderahmane and Hamel Ahmed}
}
@proceedings {2306,
	title = {Etude g{\'e}ologique du bassin de Timgad 2},
	journal = {eme colloque international sur la g{\'e}ologie du Sahara Alg{\'e}rien: Ressources min{\'e}rales, en hydrocarbures et en eaux, Ouargla, D{\'e}cembre},
	year = {2012},
	address = {Ouargla,Alger},
	author = {DJAIZ Fouad and Brinis Nafaa and Inal Ahmed}
}
@proceedings {2305,
	title = {Incidence des pluies exceptionnelles de l\&rsquo;{\'e}t{\'e} 2002 sur la nappe alluviale de Tebessa. Alg{\'e}rie},
	journal = {2eme colloque international sur la g{\'e}ologie du Sahara Alg{\'e}rien: Ressources min{\'e}rales, en hydrocarbures et en eaux, Ouargla, D{\'e}cembre },
	year = {2012},
	address = {Ouargla, Alger},
	author = {Bouchagoura I and Djabri Larbi and Brinis Nafaa}
}
@proceedings {2304,
	title = {Etude g{\'e}ologique du bassin de Timgad},
	journal = {La G{\'e}ologie du Sahara: Ressources min{\'e}rales, en hydrocarbures et en eau 03, 04 et 05 D{\'e}cembre {\`a} l{\textquoteright}universit{\'e} KASDI Merbah-Ouargla. },
	year = {2012},
	author = {DJAIZ Fouad and Brinis Nafaa}
}
@proceedings {2081,
	title = {Les risques de conflit autour des eaux transfrontali{\`e}res -Caract{\'e}risation du risque par une indexation num{\'e}rique. 6-7 juin 2012},
	journal = {Communication orale au colloque  international sur la gestion int{\'e}gr{\'e}e des ressources en eau, ABH-CSM, Constantine},
	year = {2012},
	address = {Constantine},
	author = {MENANI Mohamed redha}
}
@proceedings {2080,
	title = {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},
	journal = {Orale Communication at the Sixteenth International Water Technology Conference (IWTC16), Istanbul {\textendash} Turkey},
	year = {2012},
	address = {Istanbul {\textendash} Turkey},
	url = {www.iwtc.info },
	author = {MENANI Mohamed redha}
}
@proceedings {2079,
	title = {The artificial recharge of the aquifers by considering the groundwater vulnerability to pollution. 7-10 May 2012},
	journal = {Orale Communication at the Sixteenth International Water Technology Conference (IWTC16), Istanbul {\textendash} Turkey},
	year = {2012},
	address = {Istanbul {\textendash} Turkey},
	url = {www.iwtc.info},
	author = {MENANI Mohamed redha}
}
@proceedings {2753,
	title = {Alluvial Flow modeling of the aquifer of Tebessa - Extrem eastern of Algeria 2nd international water forum. (3 to 5 may 2011). Istanbul, Turky.},
	journal = {2nd international water forum. (3 to 5 may). Istanbul, Turky},
	year = {2011},
	author = {Drias Tarek and Toubal Ahmed Ch{\'e}rif}
}
@proceedings {2716,
	title = {Impact, importance et mobilisation des ressources hydriques dans le bassin mioc{\`e}ne de Timgad},
	journal = {3{\`e}me Edition du Congr{\`e}s International sur l{\textquoteright}eau, D{\'e}chets et Environnement (EDE3). 21-22 Novembre Troisi{\`e}me Edition du Congr{\`e}s International : Eau, D{\'e}chets et Environnement (EDE3), F{\`e}s- Maroc},
	year = {2011},
	author = {DJAIZ Fouad and Brinis Nafaa and Inal Ahmed and ATHAMENA Ali and ATHAMENA Malika}
}
@mastersthesis {2532,
	title = {Caract{\'e}risation du syst{\`e}me d\&rsquo;auscultation du barrage d\&rsquo;Ourkiss (Willaya d\&rsquo;Oum El Bouaghi).},
	year = {2011},
	author = {Lebghil A and Djedai Y}
}
@mastersthesis {2465,
	title = {Contribution {\`a} l\&rsquo;{\'e}tude g{\'e}otechnique du barrage Yabous \&ndash;Khenchela. Univ de Batna.},
	year = {2011},
	author = {Benaicha H and Righi Asma}
}
@proceedings {2431,
	title = {Une approche des indicateurs de conflits li{\'e}s aux  eaux transfrontali{\`e}res -D{\'e}veloppement d\&rsquo;une indexation num{\'e}rique du risque de conflit},
	journal = {Communication Orale, CIRED{\textquoteright}4, Alger, 22-23 Fevrier 2011},
	year = {2011},
	author = {MENANI Mohamed redha}
}
@proceedings {2311,
	title = {Caract{\'e}risation chimique des effluents d\&rsquo;un complexe de transformation de sel : cas du complexe ENASEL d\&rsquo;El-Outaya au sud \&ndash;Est alg{\'e}rien },
	journal = {Troisi{\`e}me congr{\`e}s international sur l{\textquoteright}eau, d{\'e}chet et environnement, Maroc : 21 et 22 Nov },
	year = {2011},
	address = {Maroc },
	author = {Brinis Nafaa and Boudoukha Abderahmane}
}
@proceedings {2310,
	title = {Impact, importance et mobilisation des ressources hydriques dans le bassin mioc{\`e}ne de Timgad  },
	journal = {3{\`e}me Edition du Congr{\`e}s  International sur l{\textquoteright}eau, D{\'e}chets et Environnement (EDE3). 21-22 Novembre. Troisi{\`e}me Edition du Congr{\`e}s International : Eau, D{\'e}chets et Environnement (EDE3), F{\`e}s- Maroc},
	year = {2011},
	address = {F{\`e}s- Maroc},
	author = {DJAIZ Fouad and Brinis Nafaa and Inal Ahmed and ATHAMENA Ali and Athamena. S}
}
@proceedings {2082,
	title = {Assessment of the risk of conflict around the water resources of the Guarani aquifer system. Com 25-29 septembre 2011},
	journal = {Orale, XIVth World Water Congress of IWRA, Porto de Galinhas},
	year = {2011},
	url = { http://worldwatercongress.com/programa_wwc_silusba_site.pdf},
	author = {MENANI Mohamed redha and Da Silva HL and Lepri LR and Franco ILC}
}
@article {1996,
	title = {Classification statistique et hydrochimique des eaux souterraines de la plaine d\&$\#$39;El-Outaya. (W) de Biskra. Alg{\'e}rie. Mars 2011, .},
	journal = {Publication au courrier du savoir, Univ-Biskra},
	number = {N{\textdegree}11},
	year = {2011},
	pages = {pp 41-46},
	abstract = {The plain of El-Outaya is in arid zone in southern Algeria. The groundwater are characterized by an Important and variabilityin its salinity. This work is presented to improve knowledge on these waters by proceeding to their statistical andhydrochemical classifications. Method C.A.H (hierarchical ascending classification) takes of three tendencies based on theimportance of the mineralization. The salt rocks are responsible of this height salinity. Concerning the hydrochemicalsynthesis, the statistical information is confirmed. There is three dominant groups.},
	url = {https://www.google.dz/url?sa=t\&rct=j\&q=\&esrc=s\&source=web\&cd=1\&cad=rja\&uact=8\&ved=2ahUKEwjxuZfk08PgAhVMWxoKHTWGD-4QFjAAegQIARAC\&url=http\%3A\%2F\%2Frevues.univ-biskra.dz\%2Findex.php\%2Fcds\%2Farticle\%2Fview\%2F463\%2F430\&usg=AOvVaw1mnRGClc7vjxfQx5pyZijR},
	author = {Brinis Nafaa and Boudoukha Abderahmane}
}
@proceedings {2718,
	title = {D{\'e}couverte de nouveaux gisements de Mammif{\`e}res dans le Constantinois (Alg{\'e}rie nord-orientale) : Int{\'e}r{\^e}t biostratigraphique},
	journal = {1er Congr{\`e}s International sur la G{\'e}ologie du Maghreb 5 G{\'e}oMag 1), Tlemcen 10-12 novembre},
	year = {2010},
	author = {Marmi Ramdane and Benabbas C and DJAIZ Fouad}
}
@proceedings {2717,
	title = {Importance des carri{\`e}res dans la vie socio-{\'e}conomique et leurs impacts sur l\&rsquo;environnement (Batna-Ain Touta)},
	journal = {1er Congr{\`e}s sur la G{\'e}ologie du Maghreb. 10-12 Novembre Tlemcen, Alg{\'e}rie.},
	year = {2010},
	author = {DJAIZ Fouad and Brinis Nafaa and Inal Ahmed}
}
@mastersthesis {2533,
	title = {{\'E}tude g{\'e}otechnique du POS de Bardo. Constantine},
	year = {2010},
	author = {Bounouara M and Hani F}
}
@mastersthesis {2467,
	title = {Caract{\'e}risation du syst{\`e}me d\&rsquo;auscultation du barrage Beni Haroun \&ndash;MILA. Univ de Batna},
	year = {2010},
	author = {Touka A and Rahmani A~}
}
@mastersthesis {2466,
	title = {Etude des caract{\'e}ristiques des granulats des carri{\`e}res sur l\&rsquo;axe Ain Touta \&ndash;Batna. Univ de Batna},
	year = {2010},
	author = {Laib Y and Touka A}
}
@proceedings {2315,
	title = {Zouaoui.S, Boumazbeur.A.R : Etude g{\'e}ologique et g{\'e}otechnique des glissements de terrains dans le bassin n{\'e}og{\`e}ne de Mila : Glissement de SIBARI},
	journal = {1{\`e}re s{\'e}minaire Euro-M{\'e}diterran{\'e}en. LRNAT{\textquoteright}2010{\textquoteright}. Batna (Alg{\'e}rie).27.28.29Avril },
	year = {2010},
	address = { Batna , Alg{\'e}rie},
	author = {Zouaoui Siham and Boumazbeur. A. R}
}
@proceedings {2314,
	title = {Arguments hydrog{\'e}ochimiques  de  l\&$\#$39;origine  {\'e}vaporitique  des  eaux  de  l\&$\#$39;aquif{\`e}re  n{\'e}og{\`e}ne d\&$\#$39;El-Outaya,  Biskra  -Alg{\'e}rie-},
	journal = {5eme conf{\'e}rence internationale sur les ressources en eau dans le bassin m{\'e}diterran{\'e}en WATMED 5, Lille France , Mai },
	year = {2010},
	address = { Lille France},
	author = {Brinis Nafaa and Boudoukha Abderahmane and Djabri Larbi}
}
@proceedings {2313,
	title = { Caract{\'e}risation du syst{\`e}me d\&$\#$39;auscultation du barrage r{\'e}servoir d\&$\#$39;Oued Athmania wilaya de Mila (Alg{\'e}rie nord orientale)},
	journal = {1er colloque international sur la g{\'e}ologie du Sahara Alg{\'e}rien: Ressources min{\'e}rales, en hydrocarbures et en eaux, Ouargla, D{\'e}cembre },
	year = {2010},
	address = {Ouargla, Alger},
	author = {Azizi Yacine and Brinis Nafaa}
}
@proceedings {2312,
	title = {Importance des carri{\`e}res dans la vie socio-{\'e}conomique et leurs impact sur l\&$\#$39;environnement (Batna\&ndash;Ain Touta)},
	journal = {1er Congr{\`e}s  sur la G{\'e}ologie du Maghreb; Tlemcen },
	year = {2010},
	address = {Tlemcen, Alger},
	author = {DJAIZ Fouad and Brinis Nafaa and Inal Ahmed and Cheriet Manel}
}
@proceedings {2083,
	title = {Choice of the artificial recharge zones and the groundwater Vulnerability to pollution.  2-5 juin 2010},
	journal = {Communication Orale, GEOMED Conference, Kemer, Turquie},
	year = {2010},
	address = {Kemer, Turquie},
	url = {http://web.deu.edu.tr/geomed2010/WebEN/index.html},
	author = {MENANI Mohamed redha}
}
@article {2004,
	title = {Caract{\'e}risation hydrodynamique d\&rsquo;un aquif{\`e}re h{\'e}t{\'e}rog{\`e}ne sous climat semi-aride. Exemple de la plaine de T{\'e}bessa.},
	journal = {Bulletin du service g{\'e}ologique de l{\textquoteright}ANGCM},
	volume = {Volume 21},
	number = {N{\textdegree} 3},
	year = {2010},
	abstract = {La zone {\'e}tudi{\'e}e fait partie du sous bassin du Mell{\`e}gue situ{\'e} au nord- est de l{\textquoteright}Alg{\'e}rie. Cette zone est caract{\'e}ris{\'e}e par un climat semi-aride. Le syst{\`e}me aquif{\`e}re y est form{\'e} par des alluvions plio-quaternaires reposant sur un substratum marneux d{\textquoteright}{\^a}ge eoc{\`e}ne. L {\'e}tude g{\'e}ostatistique des param{\`e}tres hydrodynamiques (charge hydraulique, transmissivit{\'e}) a permis d{\textquoteright}appr{\'e}hender leur {\'e}volution spatiale par la m{\'e}thode du krigeage par bloc et d{\textquoteright}identifier les zones {\`a} potentialit{\'e}s aquif{\`e}res. A cet {\'e}gard, la carte des transmissivit{\'e}s montre une zone pr{\'e}f{\'e}rentielle dans le secteur d{\textquoteright}A{\"\i}n Chabro, situ{\'e} au sud de la plaine. Ce secteur pr{\'e}sente les meilleures valeurs de la transmissivit{\'e} (103 {\`a} 5x1(L2 m2/s). L{\textquoteright}utilisation d{\textquoteright}un mod{\`e}le bidimensionnel aux diff{\'e}rences finies, a permis d{\textquoteright}{\'e}tablir le bilan global de la nappe et d{\textquoteright}affiner le champ des transmissivit{\'e}s. Celles-ci varieraient plut{\^o}t entre KL4 {\`a} KL2 m2/s. La d{\'e}marche m{\'e}thodologique, associant l{\textquoteright}approche probabiliste sous-tendue par la th{\'e}orie des variables r{\'e}gionalis{\'e}es {\`a} celle d{\'e}terministe du mod{\`e}le, conduit {\`a} une meilleure connaissance de l{\textquoteright}hydrog{\'e}ologie de cette zone semi aride.},
	url = {https://www.asjp.cerist.dz/en/article/3152},
	author = {Drias Tarek and Toubal Ahmed Ch{\'e}rif}
}
@article {1991,
	title = {D{\'e}termination des sites de recharge artificielle de l\&rsquo;aquif{\`e}re alluvial de la plaine d\&rsquo;El Madher (R{\'e}gion de Batna, Nord-Est alg{\'e}rien).},
	journal = {Bulletin du Service G{\'e}ologique National de l{\textquoteright}ANGCM},
	volume = {Vol. 21},
	number = {n{\textdegree}3},
	year = {2010},
	pages = {pp. 329-347},
	url = {http://www.energy.gov.dz/francais/index.php?page=478},
	author = {MENANI Mohamed redha}
}
@article {1980,
	title = {Evolution des Facies Chimiques des Eaux Souterraines dans da Plaine D\&rsquo;el-Outaya, Biskra, Alg{\'e}rie. Dec. 2010.},
	journal = {Journal International Environmental Conflict Management, Santa Catarina {\textendash} Brazil},
	volume = {Vol 1},
	number = {N{\textdegree}1},
	year = {2010},
	pages = {pp. 98-105},
	author = {Brinis Nafaa and Boudoukha Abderahmane and Djabri Larbi}
}
@article {1912,
	title = {Les conflits transfrontaliers sur l\&rsquo;eau : Tendances actuelles. S{\'e}cheresse, Janvier-mars 2010, John Libbey Eurotext Paris},
	journal = {S{\'e}cheresse},
	volume = {Vol. 21},
	number = {N{\textdegree}1},
	year = {2010},
	pages = {pp. 22-27},
	abstract = {
	
		\&nbsp;
	

	
		
			Du fait qu{\textquoteright}elle est indispensable, l{\textquoteright}eau a {\'e}t{\'e} utilis{\'e}e depuis l{\textquoteright}Antiquit{\'e} comme arme dans les conflits. Par exemple, en 596 av. J.-C., lors du si{\`e}ge de la cit{\'e} de Tyr, Nabuchodonosor avait d{\'e}truit une partie de l{\textquoteright}aqueduc qui l{\textquoteright}approvisionnait. En 1938, afin d{\textquoteright}inonder les zones menac{\'e}es par l{\textquoteright}arm{\'e}e japonaise, Tchang Ka{\"\i}-Chek ordonne la destruction des digues d{\textquoteright}{\'e}cr{\^e}tement des crues sur une partie du fleuve Jaune. L{\textquoteright}inondation d{\'e}truisit une partie des forces d{\textquoteright}invasion, mais noya {\'e}galement des milliers de Chinois. D{\textquoteright}autres violations, qui se sont d{\'e}roul{\'e}es pendant la seconde guerre mondiale ou la durant la guerre du Vietnam, avaient trait aux {\'e}quipements hydro{\'e}lectriques et aux digues qui {\'e}taient prises comme cibles lors des bombardements. Dans d{\textquoteright}autres cas, c{\textquoteright}est l{\textquoteright}insuffisance de la ressource qui est la cause de tensions extr{\^e}mes et de strat{\'e}gies expansionnistes, comme c{\textquoteright}est le cas de l{\textquoteright}{\'e}ternel conflit transfrontalier entre Isra{\"e}l et les pays arabes voisins, autour des eaux du Jourdain. {\`A} l{\textquoteright}{\'e}chelle locale, voire parcellaire, le principal argument de conflit rel{\`e}ve de l{\textquoteright}usage qui concerne notamment l{\textquoteright}irrigation des terres et le respect des quotas impos{\'e}s par des r{\`e}gles ancestrales. Cet ingr{\'e}dient prend une autre dimension lorsqu{\textquoteright}il est m{\^e}l{\'e} {\`a} l{\textquoteright}espace politique ou ethnique d{\textquoteright}une population donn{\'e}e, et ce m{\^e}me si la ressource est abondante. M{\^e}me si certaines {\'e}tudes alarmistes, telles celles qui concernent particuli{\`e}rement les zones arides du Proche-Orient, pr{\'e}disent des conflits violents autour de l{\textquoteright}eau, des initiatives reposant sur des consid{\'e}rations juridiques, humanitaires, {\'e}conomiques et scientifiques sont men{\'e}es par la communaut{\'e} internationale afin de pr{\'e}venir le p{\'e}ril que constituent les conflits li{\'e}s {\`a} l{\textquoteright}eau en plusieurs endroits sensibles de la plan{\`e}te.
		
	

},
	url = {http://www.secheresse.info/spip.php?article10060},
	author = {MENANI Mohamed redha}
}
@article {1889,
	title = {Heterogeneous aquifer system modelization under semi-arid climate. Geophysical Research Abstracts, EGU2010-178,},
	journal = {EGU General Assembly},
	volume = {Vol. 12},
	year = {2010},
	abstract = {The studied zone is a part of the Mellegne{\textquoteright}s (North-East of Algeria) under pound, this zone is characterised by itssemi-arid climate.The water bearing system is formed by the plio-quaternairy alluviums resting on a marley substratuim of ageEocene.The geostatiscitcs approach of the hydrodynamics parameters (Hydrolic load, transmisivity) allowed the studyof their spatial distrubution (casting) by the method of Krigeage by blocks and the identification of zones withwater-bearing potentialities.In this respect, the zone of Ain Chabro which, is situated in the South of the plain shows the best values of thetransmisivity......The use of a bidimensinnel model in the differences ended in the permanent regime allowed us to establish theglobal balence sheet (overall assessment) of the tablecloth and to refine the transmisivity field. These would varymore exactley between 10-4 to 10-2 m2/s.The method associating the probability appraoch of Krigeage to that determining the model has facilited thewedging of the model and clarified the inflitration value},
	url = {ftp://ftp.gfz-potsdam.de/home/cegit/egu/pdf/EGU2010-178.pdf },
	author = {Drias Tarek and Toubal Ahmed Ch{\'e}rif}
}
@proceedings {2755,
	title = {Hydrodynamical characterization of a heterogeneous aquifer system under semi-arid climate Example of the plain of  T{\'e}bessa },
	journal = {The First international symposium of the petroleum and geological resources in the tethys realm. Cairo, Egypt},
	year = {2009},
	author = {Drias Tarek and Toubal Ahmed Ch{\'e}rif}
}
@proceedings {2721,
	title = {Impact des ressources hydriques sur le d{\'e}veloppement durable dans le basin de Timgad-Alg{\'e}rie Nord Orientale},
	journal = {1er Colloque International sur la Gestion Int{\'e}gr{\'e}e des Ressources. en eau. 10 {\textendash} 11 Novembre D{\'e}partement des Sciences de la Terre {\textendash} Facult{\'e} des Sciences Universit{\'e} de Batna.},
	year = {2009},
	author = {DJAIZ Fouad and ATHAMENA Ali}
}
@mastersthesis {2468,
	title = {Etude g{\'e}otechnique du barrage de Ourkis \&ndash;Oum El-Bouaghi. Univ de Batna},
	year = {2009},
	author = {Yellouz H and Seghiri M~}
}
@proceedings {2316,
	title = {Evolution des Facies Chimiques des Eaux Souterraines dans da Plaine D\&rsquo;el-Outaya, Biskra, Alg{\'e}rie },
	journal = {Colloque international gestion int{\'e}gr{\'e}e des ressources en eau (GIRE), Batna},
	year = {2009},
	address = {Batna, Alger},
	author = {Brinis Nafaa and Boudoukha Abderahmane and Djabri Larbi}
}
@proceedings {2088,
	title = {Hydrog{\'e}ologie d\&rsquo;une vall{\'e}e Auressienne \&ndash; Cas de la Vall{\'e}e de Bouzina. 10-11 novembre 2009},
	journal = {Communication affich{\'e}e, 1er Colloque International sur la Gestion Int{\'e}gr{\'e}e des Ressources en eau, Batna },
	year = {2009},
	pages = {p 71},
	address = {Batna},
	author = {Rihani A and MENANI Mohamed redha}
}
@proceedings {2087,
	title = {Evolution de la pi{\'e}zom{\'e}trie de la ville de Oued Souf (entre 1993, 2002 et 2007) - Perspectives de la maitrise du ph{\'e}nom{\`e}ne de remont{\'e}e de la nappe phr{\'e}atique. 10-11 novembre },
	journal = {Communication orale, 1er Colloque International sur la Gestion Int{\'e}gr{\'e}e des Ressources en eau, Batna },
	year = {2009},
	pages = {p 47},
	address = {Batna},
	author = {Messekher I and MENANI Mohamed redha}
}
@proceedings {2086,
	title = { Retrospective sur les conflits transfrontaliers sur l\&rsquo;eau, 10-11 novembre 2009},
	journal = {Communication orale 1er Colloque International sur la Gestion Int{\'e}gr{\'e}e des Ressources en eau, Batna },
	year = {2009},
	pages = {p 38},
	address = {Batna},
	author = {MENANI Mohamed redha}
}
@proceedings {2085,
	title = {Contribution au choix des sites de recharge artificielle de l\&rsquo;aquif{\`e}re alluvial de la plaine d\&rsquo;El Madher (r{\'e}gion de Batna, nord-est alg{\'e}rien) 10-11 novembre 2009},
	journal = {Communication orale 1er Colloque International sur la Gestion Int{\'e}gr{\'e}e des Ressources en eau, Batna },
	year = {2009},
	pages = {p 26},
	address = {Batna},
	author = {MENANI Mohamed redha}
}
@proceedings {2084,
	title = {Can we classify the conflict risks around the transboundary water resources? Case of the Jordan basin. 04-06 mars 2009},
	journal = {Communication orale Encontro Internacional de Direito ambiental na Amazonia, Macap{\'a} {\textendash} Amap{\'a}, Brazil},
	year = {2009},
	address = {Macap{\'a} {\textendash} Amap{\'a}, Brazil},
	author = {MENANI Mohamed redha}
}
@article {1997,
	title = {La salinit{\'e} des eaux souterraines de la zone Est de la plaine d\&rsquo;El-Outaya (R{\'e}gion de Biskra, Alg{\'e}rie). .14 fig., 2 tabl.},
	journal = {Bulletin du Service G{\'e}ologique National},
	volume = {Vol.20},
	number = {N{\textdegree}1},
	year = {2009},
	pages = {pp 49-61},
	abstract = {Ce travail a {\'e}t{\'e} r{\'e}alis{\'e} en zone aride et concerne la salinit{\'e} des eaux de la nappe du MioPlio- Quaternaire de la plaine d{\textquoteright}El-Outaya (r{\'e}gion de Biskra au sud alg{\'e}rien). Cette plaine est le r{\'e}sultat d un remplissage n{\'e}og{\`e}ne qui repose en discordance sur tous les terrains ant{\'e}rieurs m{\'e}sozo{\"\i}ques et pal{\'e}og{\`e}nes. Le Trias avec son diapir de sel reste un {\'e}l{\'e}ment tr{\`e}s important dans cette plaine par sa composition lithologique et ses contacts anormaux avec les autres formations. Le contact de l aquif{\`e}re {\'e}tudi{\'e} avec le substratum se fait soit par des conglom{\'e}rats, soit par des argiles. L{\textquoteright}h{\'e}t{\'e}rog{\'e}n{\'e}it{\'e} de la nappe du Mio-Plioc{\`e}ne se caract{\'e}rise par la pr{\'e}sence d argile dans des proportions variables. L{\textquoteright}{\'e}vaporation dans la r{\'e}gion est tr{\`e}s intense et consomme la majorit{\'e} des pr{\'e}cipitations. La combinaison entre les outils, g{\'e}ologique, g{\'e}ophysique, statistique et chimique dans l{\textquoteright}{\'e}tude du probl{\`e}me de la salinit{\'e} permet de d{\'e}terminer l{\textquoteright}origine et l {\'e}volution dans l{\textquoteright}espace de cette derni{\`e}re. Les analyses effectu{\'e}es indiquent la pr{\'e}sence en fortes concentrations des {\'e}l{\'e}ments CT, S042\ Na + et Mg+. Dans la partie nord et ouest, les eaux sont caract{\'e}ris{\'e}es par un faci{\`e}s chlorur{\'e} sodique (influence de la halite), {\`a} Test, le faci{\`e}s sulfat{\'e} magn{\'e}sien domine (influence du gypse). Entre ces deux faci{\`e}s, on note une zone o{\`u} les eaux sont mixtes, caract{\'e}ris{\'e}es par un faci{\`e}s sulfat{\'e} sodique ({\'e}change de base). L{\textquoteright}interpr{\'e}tation thermodynamique a permis la d{\'e}termination de l{\textquoteright}influence des min{\'e}raux {\'e}vaporitiques {\`a} des degr{\'e}s variables dans la composition chimique des eaux. Ces min{\'e}raux sont {\`a} l{\textquoteright}origine de la salinit{\'e} des eaux de la r{\'e}gion. Les min{\'e}raux carbonat{\'e}s se trouvent sursatur{\'e}s dans l{\textquoteright}eau.},
	url = {https://www.asjp.cerist.dz/en/article/1921},
	author = {Brinis Nafaa and Boudoukha Abderahmane and Djabri Larbi and Mania Jacky}
}
@article {1935,
	title = {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},
	journal = {Springer},
	volume = {Vol. 36},
	number = { N{\textdegree}6},
	year = {2009},
	pages = {pp. 731-742},
	abstract = {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.},
	url = {https://doi.org/10.1134/S0097807809060128},
	author = {MENANI Mohamed redha}
}
@article {1927,
	title = {The Artificial Recharge and the Groundwater Vulnerability to Pollution-Case of the El Madher Plain (North East of Algeria)},
	journal = {European Journal of Scientific Research},
	volume = {Vol.32},
	number = {No.3},
	year = {2009},
	pages = {pp.288-303},
	abstract = {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: {\textbullet} mobilisation of this resource in zones were it{\textquoteright}s very available; {\textbullet} injection by different means in aquifer zones whose characteristics are known; {\textbullet} 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; {\textbullet} 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).},
	url = {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},
	author = {MENANI Mohamed redha}
}
@article {1921,
	title = {Statistical approach of the physiographical parameters influence on runoffs observed at the exit of basins - a case of Algerian basins. May 2009},
	journal = {ARPN Journal of Engineering and Applied Science},
	volume = {Vol. 4},
	number = {N{\textdegree} 3},
	year = {2009},
	pages = {pp. 48-53},
	abstract = {The predetermination of the runoff in the non gauged basins constitutes the objective of numerous researches because of a lack of data covering them. Thus, the use of mathematical models became the suitable approach. Runoffs at the exit of basins, in addition to being influenced logically by rainfalls and their intensities, they are under the influence of other factors which condition the surface discharge such as the physiographical parameters of the basins, lithology, vegetation cover and evaporation. The aim of this work is to seek statistical relations which bind runoff observed at the exit of basins to rainfalls and some physiographical factors for basins of Algeria between September 1985 and September 1993. The simple and multiple correlations carried out on 23 basins made it possible to emphasize that some physiographicalcharacteristics are explanatory of the variance of the runoff to significant thresholds.},
	url = {http://www.arpnjournals.com/jeas/research_papers/rp_2009/jeas_0509_184.pdf},
	author = {MENANI Mohamed redha and Bennedjai Nassima}
}
@proceedings {2759,
	title = {Caract{\'e}risation g{\'e}ologique et g{\'e}otechnique des glissements de la ville de Bougaa N.W S{\'e}tif},
	journal = {~33{\`e}mes journ{\'e}es scientifiques internationales du GFHN Avignon France les 19-20 Novembre},
	year = {2008},
	author = {Djenba Samir}
}
@proceedings {2757,
	title = {Caract{\'e}risation g{\'e}ologique et g{\'e}otechnique des glissements de la ville de Bougaa N.W S{\'e}tif },
	journal = {Colloque international Terre-Eau Annaba les 17, 18,19 Novembre},
	year = {2008},
	author = {Djenba Samir and khadidja A}
}
@proceedings {2723,
	title = {The impact of hydraulic resources on sustainable development of the Timgad basin north-east of Algerie},
	journal = {3rd Environmental physics conference Aswan 19-23 F{\'e}vrier Egypte [Egyptian Nuclear Physics Association (ENPA)]},
	year = {2008},
	author = {DJAIZ Fouad and ATHAMENA Ali}
}
@mastersthesis {2534,
	title = {Contribution {\`a} l\&rsquo;{\'e}tude de stabilit{\'e} d\&rsquo;un tron{\c c}on de l\&rsquo;autoroute Est-ouest, section (4-2), Elmeridj- Didouch. Constantine.},
	year = {2008},
	author = {Djaraf G and Djebar S}
}
@mastersthesis {2471,
	title = {Caract{\'e}risation du syst{\`e}me d\&$\#$39;auscultation du barrage r{\'e}servoir d\&$\#$39;Oued Athmania wilaya de Mila (Alg{\'e}rie nord orientale) Univ de Batna},
	year = {2008},
	author = {Azizi Yacine and Kerboub D}
}
@mastersthesis {2469,
	title = {Contribution {\`a} l\&rsquo;{\'e}tude des mat{\'e}riaux de construction du barrage Bouggous El Taref. Univ de Batna},
	year = {2008},
	author = {Maalem M and Telali Y}
}
@proceedings {2439,
	title = {La salinit{\'e} des eaux souterraines dans la r{\'e}gion d\&rsquo;El-Outaya (Biskra) Alg{\'e}rie},
	journal = {Journ{\'e}e d{\textquoteright}{\'e}tude et de sensibilisation {\`a} la gestion de la ressource en eau dans les r{\'e}gions arides et semi arides. CRSTRA, Biskra le 15 Mars},
	year = {2008},
	author = {Brinis Nafaa}
}
@proceedings {2438,
	title = {Traitement de la fondation du barrage de fontaine des gazelles-(Biskra) par des injections d\&rsquo;{\'e}tanch{\'e}it{\'e}. M{\'e}thodologie et r{\'e}sultats},
	journal = {Journ{\'e}e d{\textquoteright}{\'e}tude sur les applications des Donn{\'e}es G{\'e}ologiques, G{\'e}omorphologiques aux plans d{\textquoteright}Am{\'e}nagement. Laboratoire de G{\'e}ologie et Environnement. Constantine 29 juin},
	year = {2008},
	author = {Brinis Nafaa}
}
@proceedings {2432,
	title = {Assurer la durabilit{\'e} du partenariat Universit{\'e} - Environnement Socio-{\'e}conomique {\`a} travers une cellule de veille},
	journal = {Communication orale programm{\'e}e aux Journ{\'e}es Nationales d{\textquoteright}Etudes et d{\textquoteright}Information Sur Le Partenariat Universit{\'e}-Environnement Socio-{\'e}conomique: D{\'e}fis et Perspectives. Batna, 14 - 15 d{\'e}cembre},
	year = {2008},
	author = {MENANI Mohamed redha}
}
@proceedings {2091,
	title = {Numerical indexing of risks of conflicts around the transboundary water resources},
	journal = {Communication orale au IV International Symposium on Transboundary Water Management. Thessaloniki, Greece,15th-18th October},
	year = {2008},
	address = {Thessaloniki, Greece},
	author = {MENANI Mohamed redha}
}
@proceedings {2090,
	title = {Le ph{\'e}nom{\`e}ne de la remont{\'e}e des eaux de la nappe phr{\'e}atique de la cuvette de Ouargla (Sahara alg{\'e}rien),24- 26  juin 2008},
	journal = { Communication orale, 10{\`e}me  Symposium International de l{\textquoteright}eau, Cannes},
	year = {2008},
	address = {Cannes},
	author = {MENANI Mohamed redha}
}
@proceedings {2089,
	title = {Approche d\&rsquo;une m{\'e}thode d\&rsquo;indexation num{\'e}rique des risques de conflits autour des ressources en eau transfrontali{\`e}res,  24- 26  juin 2008},
	journal = {Communication orale, 10{\`e}me  Symposium International de l{\textquoteright}eau, Cannes},
	year = {2008},
	address = {Cannes},
	author = {MENANI Mohamed redha}
}
@article {2000,
	title = {Contribution {\`a} l\&rsquo;{\'e}tude p{\'e}tro-structurale de la bordure Est et Sud Est du socle de la Petite Kabylie Nord-Est Alg{\'e}rie. Juin (2008)},
	journal = {Sciences \& Technologie },
	number = {N{\textdegree}27},
	year = {2008},
	pages = {pp. 71-76},
	abstract = {
	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 {\'e}pizonale to m{\'e}sozonale of low pressure and high temperature. This last estimated at P=4-5 Kbar and T=650-700{\textdegree}C is underlined by the presence of the veins of leucozones and the myrm{\'e}kite thus near to the field of partial fusion.



	The structural draft shows the superposition of schisto-sandy units {\'e}pizonales on units of higher rank. This area is overcome in its Western and Eastern part by formations of Oligo-Mioc{\`e}ne-Kabyle.



	The study of the syn-schistous deformation highlights an extensive component at vergency is and of the lin{\'e}ations 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-Fergu{\`e}ne towards the NW. Alpine and eo-alpine post-schistous deformations of lower (Pt), at vergency East and South, are



	highlighted.

},
	url = {http://revue.umc.edu.dz/index.php/d/article/viewFile/482/589},
	author = {DJAIZ Fouad}
}
@proceedings {2764,
	title = {De la caract{\'e}risation hydrochimique d\&rsquo;un syst{\`e}me aquif{\`e}re sous climat semi-aride. Cas de la plaine de T{\'e}bessa },
	journal = {2{\`e}me colloque international sur l{\textquoteright}eau et l{\textquoteright}environnement. 30-31 Janvier ~ENSH. Alger. Alg{\'e}rie},
	year = {2007},
	author = {Drias Tarek and Toubal Ahmed Ch{\'e}rif}
}
@proceedings {2763,
	title = {Caract{\'e}risation g{\'e}ologique et g{\'e}otechnique du gonflement du sol de la r{\'e}gion de N\&rsquo;Gaous NE Algerien},
	journal = {32{\`e}mes journ{\'e}es scientifiques internationales du GFHN Nantes France les 21-22 Novembre},
	year = {2007},
	author = {Djenba Samir}
}
@proceedings {2761,
	title = {Caract{\'e}risation hydrodynamique d\&rsquo;un aquif{\`e}re h{\'e}t{\'e}rog{\`e}ne sous climat semi-aride, exemple de la plaine de T{\'e}bessa},
	journal = {4{\`e}me journ{\'e}es internationales des g{\'e}osciences de l{\textquoteright}environnement. 08-10 Juin T{\'e}touan. Maroc},
	year = {2007},
	author = {Drias Tarek and Toubal Ahmed Ch{\'e}rif}
}
@proceedings {2726,
	title = {Cons{\'e}quences de la phase tectonique alpine sur les d{\'e}formations syn-schisteuses tardi-hercyniennes du socle de la Petite Kabylie (Alg{\'e}rie Nord-orientale)},
	journal = {Second International Conf{\'e}rence on the Geology of the Tethys. 19-23 March The T{\'e}thys Geological Society at Cairo university},
	year = {2007},
	author = {DJAIZ Fouad and Mahdjoub Y}
}
@proceedings {2724,
	title = {L\&rsquo;hypoth{\`e}se de l\&rsquo;existence d\&rsquo;un d{\^o}me gneissique extensif dans le secteur de Bouchtata-Tamalous bordure orientale du socle de la Petite Kabylie (Alg{\'e}rie nord-orientale)},
	journal = {The 5th session of the international symposium 3MA (Magmatisme, M{\'e}tamorphisme et Min{\'e}ralisations Associ{\'e}es. 10-12 Mai Le D{\'e}partement de G{\'e}ologie de la Facult{\'e} des Sciences- F{\`e}s Dhar El mehraz~ Maroc},
	year = {2007},
	author = {DJAIZ Fouad and Marmi Ramdane}
}
@mastersthesis {2535,
	title = {Contribution {\`a} l\&rsquo;{\'e}tude g{\'e}otechnique du pont d\&rsquo;Oued Gueiss- Kais. Willaya de Khenchela.},
	year = {2007},
	author = {Saoudi A}
}
@mastersthesis {2472,
	title = {Contribution {\`a} l\&rsquo;{\'e}tude g{\'e}otechnique de la retenue collinaire de Tallilit. Dpt des sciences de la terre, Univ de Batna},
	year = {2007},
	author = {Arrous.A and Tey.Y}
}
@proceedings {2443,
	title = {De la caract{\'e}risation hydrochimique d\&rsquo;un syst{\`e}me aquif{\`e}re sous climat semi-aride. Cas de la plaine de T{\'e}bessa},
	journal = {2{\`e}me colloque international sur l{\textquoteright}eau et l{\textquoteright}environnement. 30-31 Janvier 2007.  ENSH. Alger. Alg{\'e}rie},
	year = {2007},
	author = {Drias Tarek and Toubal Ahmed Ch{\'e}rif}
}
@proceedings {2441,
	title = {Etude stratigraphique et s{\'e}dimentologique de Manchar Ali Guera, versant Nord de Djebel Bou Arif (Aur{\`e}s, Nord est D\&rsquo;Alg{\'e}rie)},
	journal = { Communication au 3{\`e}me S{\'e}minaire National de Stratigraphie. 19-20-21 et 22 F{\'e}vrier, ANGCM/DSGN/ Minist{\`e}re des {\'e}nergies/Laghouat},
	year = {2007},
	author = {DJAIZ Fouad and Benmansour S}
}
@proceedings {2318,
	title = {Aspect g{\'e}ochimique de la qualit{\'e} des eaux souterraines exploit{\'e}es dans les aur{\`e}s (cas de la vall{\'e}e de l\&rsquo;oued abiod) Alg{\'e}rie},
	journal = {2eme conf{\'e}rence internationale de la g{\'e}ologie de la T{\'e}thys 19-23 mars Caire Egypte},
	year = {2007},
	address = {Caire Egypte},
	author = {Brinis Nafaa and Shoot H and Hamel Ahmed and Nezli IE}
}
@proceedings {2317,
	title = {L\&$\#$39;utilisation du facteur de concentration (Fc) pour le suivi des {\'e}l{\'e}ments caract{\'e}risant les faci{\`e}s chimiques des eaux des aur{\`e}s ALGERIE},
	journal = {4eme Journ{\'e}es internationales des g{\'e}osciences de l{\textquoteright}environnement. Tetouan 8-10 juin },
	year = {2007},
	author = {Brinis Nafaa and Hamel Ahmed and Nezli IE}
}
@proceedings {2092,
	title = {Les Conflits Transfrontaliers sur l\&rsquo;Eau},
	journal = {Communication orale 9{\`e}me Symposium International de l{\textquoteright}eau, Cannes, 26-28 juin},
	year = {2007},
	address = { Cannes},
	author = {MENANI Mohamed redha}
}
@proceedings {2733,
	title = {Observations g{\'e}ologiques des glissements de terrain dans le Constantinois : cas du tron{\c c}on d\&rsquo;autoroute Massinissa, Didouche Mourad et Anouche Ali. (Alg{\'e}rie nord-orientale)},
	journal = {S{\'e}minaire International sur les G{\'e}osciences au Service du D{\'e}veloppement Durable (26, 27 et 28 novembre) Centre Universitaire de T{\'e}bessa},
	year = {2006},
	author = {Marmi Ramdane and BOUMEZBEUR A and DJAIZ Fouad}
}
@proceedings {2730,
	title = {Caract{\'e}ristiques g{\'e}ologiques, g{\'e}otechniques et hydrologiques d\&rsquo;un site destin{\'e} {\`a} l\&rsquo;am{\'e}nagement d\&rsquo;un ouvrage hydraulique (Aur{\`e}s, Alg{\'e}rie Nord-Orientale)},
	journal = {Third International Conference on water Resources in Mediterranean Basin. 1-3 November Watmed 3 Tripoli- Lebanon},
	year = {2006},
	author = {DJAIZ Fouad and Marmi Ramdane and ATHAMENA Ali}
}
@proceedings {2728,
	title = {Caract{\'e}ristiques g{\'e}ologiques, g{\'e}otechniques et hydrologiques d\&rsquo;un site destin{\'e} {\`a} l\&rsquo;am{\'e}nagement d\&rsquo;un ouvrage hydraulique (Aur{\`e}s, Alg{\'e}rie Nord-Orientale) },
	journal = {S{\'e}minaire International sur les G{\'e}osciences au Service du D{\'e}veloppement Durable. 26-27 et 28 Novembre Centre Uni de T{\'e}bessa / Institut des Sciences de la Terre},
	year = {2006},
	author = {DJAIZ Fouad and Marmi Ramdane and ATHAMENA Ali}
}
@mastersthesis {2536,
	title = {Influence des conditions g{\'e}ologiques sur la stabilit{\'e} du barrage de Hammam Grouz, Oued El Athemania. Constantine.},
	year = {2006},
	author = {Bouchene. N}
}
@mastersthesis {2473,
	title = {Num:13-, , (2006): Contribution {\`a} l\&$\#$39;{\'e}tude de la stabilit{\'e} de la digue du barrage Saf-Saf Ouesra Tebessa.D{\'e}partement des scs de la terre, Univ- Batna.},
	year = {2006},
	author = {Hoggas D and Nabti H and Yahiaoui K}
}
@proceedings {2321,
	title = {Caract{\'e}risation de la qualit{\'e} chimique des eaux souterraines de l\&$\#$39;oued Abiod},
	journal = {journ{\'e}es d{\textquoteright}{\'e}tude internationales sur "la d{\'e}sertification et le d{\'e}veloppement durable". CRSTRA et universit{\'e} de Biskra},
	year = {2006},
	author = {Brinis Nafaa and Hamel Ahmed and Nezli IE}
}
@proceedings {2320,
	title = {Aspects G{\'e}ochimiques de la Salinit{\'e} des Eaux du Mio-Plio-Quaternaire et Equilibres Entre Min{\'e}raux et Solutions dans la Plaine d\&$\#$39;El-Outaya . ALGERIE},
	journal = {Watmed 3. Tripoli. Liban},
	year = {2006},
	author = {Brinis Nafaa and Boudoukha Abderahmane and Djabri Larbi}
}
@proceedings {2319,
	title = {Etude des types chimiques des eaux exploit{\'e}es dans les Aur{\`e}s (cas de la vall{\'e}e de l\&rsquo;oued Abiod)},
	journal = {Seminaire international sur les g{\'e}osciences au service du d{\'e}veloppement durable 26,27 et 28 Nov Tebessa},
	year = {2006},
	address = {Tebessa, Alger},
	author = {Brinis Nafaa and Hamel Ahmed and Nezli IE}
}
@proceedings {2093,
	title = {Using numerical indexes for mapping the groundwater pollution potential},
	journal = {Communication orale, 8{\`e}me  Symposium International de l{\textquoteright}eau, Cannes, 26-30  juin},
	year = {2006},
	address = {Cannes},
	author = {MENANI Mohamed redha}
}
@article {1998,
	title = {La salinit{\'e} des eaux souterraines de la plaine d\&rsquo;El-Outaya (Biskra, Alg{\'e}rie). Biskra, ann{\'e}e 2006.},
	journal = {Journal Alg{\'e}rien des R{\'e}gions Arides},
	year = {2006},
	pages = {pp 261-265},
	author = {Brinis Nafaa and Djabri Larbi and Kardache Ramdane}
}
@proceedings {2778,
	title = {Faisabilit{\'e} g{\'e}ologique de la retenue collinaire de Foum toub },
	journal = {1erseminaire national sur la mobilisation et l{\textquoteright}exploitation des ressources en eau.Dpt d{\textquoteright}Hydraulique en collaboration avec le laboratoire de recherche en Hydraulique appliqu{\'e}e. Univ.Batna},
	year = {2005},
	author = {DJAIZ Fouad and Marmi Ramdane and BOUMEZBEUR A and Brinis Nafaa}
}
@proceedings {2777,
	title = {L\&rsquo;apport g{\'e}otechnique {\`a} l\&rsquo;{\'e}tude du ph{\'e}nom{\`e}ne du mouvement du sol : retrait gonflement},
	journal = {Communication au 1er S{\'e}minaire sur L{\textquoteright}apport de la g{\'e}otechnique face aux risques naturels. 08/09 Novembre Laboratoire National de l{\textquoteright}Habitat et de la Construction/ Batna},
	year = {2005},
	author = {DJAIZ Fouad and BOUMEZBEUR A and Marmi Ramdane}
}
@proceedings {2776,
	title = {Faisabilit{\'e} de la retenue collinaire de Foum Toub : Etude g{\'e}ologique et g{\'e}otechnique (Aur{\`e}s, Batna)},
	journal = {Communication au Premier s{\'e}minaire national sur la mobilisation et l{\textquoteright}exploitation des ressources en eau. 12-13 D{\'e}cembre Lab. LARHYA / Uni. De Batna},
	year = {2005},
	author = {DJAIZ Fouad and BOUMEZBEUR A and Marmi Ramdane and Brinis Nafaa and ATHAMENA Ali}
}
@proceedings {2774,
	title = {Caract{\'e}risation lithologique {\`a} base de mesures de K: repr{\'e}sentation graphique (Cas du site de Beni Haroun)},
	year = {2005},
	author = {Cheriet Manel and Benzagouta Mohamed Said}
}
@proceedings {2773,
	title = {Influence des roches evaporitiques sur la d{\'e}gradation des eaux souterraines de la plaine d\&rsquo;el-outaya },
	journal = {1er s{\'e}minaire national sur la mobilisation et l{\textquoteright}exploitation des ressources en eau. Dpt d{\textquoteright}Hydraulique en collaboration avec le laboratoire de recherche en Hydraulique appliqu{\'e}e. Univ.Batna},
	year = {2005},
	author = {Brinis Nafaa and Boudoukha Abderahmane and Djabri Larbi}
}
@proceedings {2772,
	title = {Faisabilit{\'e} g{\'e}ologique de la retenue collinaire de Foum toub },
	journal = {1erseminaire national sur la mobilisation et l{\textquoteright}exploitation des ressources en eau.Dpt d{\textquoteright}Hydraulique en collaboration avec le laboratoire de recherche en Hydraulique appliqu{\'e}e. Univ.Batna},
	year = {2005},
	author = {DJAIZ Fouad and Marmi Ramdane and BOUMEZBEUR A and Brinis Nafaa}
}
@proceedings {2771,
	title = {M{\'e}canismes d\&$\#$39;acquisition de la salinit{\'e} des eaux de la nappe phr{\'e}atique de la basse Vall{\'e}e de l\&rsquo;Oued Mya (Ouargla) },
	journal = {1er seminaire national sur la mobilisation et l{\textquoteright}exploitation des ressources en eau.Dpt d{\textquoteright}Hydraulique en collaboration avec le laboratoire de recherche en Hydraulique appliqu{\'e}e. Univ.Batna},
	year = {2005},
	author = {Nezli IE and Achour S and Brinis Nafaa}
}
@proceedings {2770,
	title = {Faisabilit{\'e} de la retenue collinaire de Foum Toub : Etude g{\'e}ologique et g{\'e}otechnique (Aur{\`e}s, Batna)},
	journal = {Communication au Premier s{\'e}minaire national sur la mobilisation et l{\textquoteright}exploitation des ressources en eau. 12-13 D{\'e}cembre 2005. Lab. LARHYA / Uni. De Batna},
	year = {2005},
	author = {DJAIZ Fouad and BOUMEZBEUR A and Marmi Ramdane and Brinis Nafaa and ATHAMENA Ali}
}
@proceedings {2767,
	title = {Fluctuation pi{\'e}zom{\'e}trique interannuelle de la nappe superficielle de Beida bordj (W.S{\'e}tif) },
	journal = {premier s{\'e}minaire national sur la mobilisation et l{\textquoteright}exploitation des ressources en eau Batna les 12-13 d{\'e}cembre~},
	year = {2005},
	author = {Djenba Samir and Boudoukha Abderahmane}
}
@proceedings {2740,
	title = {Tectonique compressive polyphas{\'e}e dans la cha{\^\i}ne alpine en Alg{\'e}rie : l\&rsquo;exemple du M{\^o}le Constantinois et de son avant-pays},
	journal = {2{\textdegree} S{\'e}minaire international sur la G{\'e}ologie du Grand Constantinois et des Confins alg{\'e}ro-tunisiens SGGC-2, Universit{\'e} de Constantine, 9-11 mai},
	year = {2005},
	author = {Marmi Ramdane and Guiraud R and DJAIZ Fouad}
}
@proceedings {2738,
	title = {Contribution {\`a} l\&rsquo;{\'e}tude p{\'e}tro-structurale du secteur Bouchtata-Tamalous situ{\'e} dans la bordure orientale du socle de la Petite Kabylie},
	journal = {S{\'e}minaire International "la G{\'e}ologie du ~Grand Constantinois~ et des Confins Alg{\'e}ro-Tunisiens". 09-10 et -11 Mai D{\'e}pt Sc Terre/ Uni de Constantine/Laboratoire de G{\'e}ologie et Environnement/Sonatrach},
	year = {2005},
	author = {DJAIZ Fouad and Marmi Ramdane}
}
@proceedings {2735,
	title = {Risque naturels li{\'e}e au ph{\'e}nom{\`e}ne retrait-gonflement des sols \&laquo; Cas de Djerma-Batna \&raquo;},
	journal = {S{\'e}minaire international sur les Risques Naturels li{\'e}s aux glissements de terrains et d{\textquoteright}{\'e}boulement rocheux. 15-16 Novembre Universit{\'e} de 08 Mai 45 Guelma / Laboratoire G{\'e}nie Civil et Habitat},
	year = {2005},
	author = {DJAIZ Fouad and BOUMEZBEUR A and Marmi Ramdane}
}
@mastersthesis {2474,
	title = {Contribution {\`a} l\&$\#$39;{\'e}tude g{\'e}otechnique d\&$\#$39;un barrage en terre \&quot;Fontaine des gazelles sur oued El-Hai wilaya de Biskra. D{\'e}partement sciences de la terre, Univ. de Batna.},
	year = {2005},
	author = {Meziani A and Soltani~~H}
}
@proceedings {2094,
	title = {Etude de la pollution d\&rsquo;une nappe P{\'e}riurbaine, cas de la plaine d\&rsquo;El Madher (Nord-Est Alg{\'e}rie)},
	journal = {Communication orale, 7{\`e}me  Symposium International de l{\textquoteright}eau, Cannes, 27 juin-02 juillet },
	year = {2005},
	address = {Cannes},
	author = {MENANI Mohamed redha}
}
@proceedings {2780,
	title = {Etude des pal{\'e}o-courants dans les formations du barr{\'e}mien et du mioc{\`e}ne : Nouvelle hypoth{\`e}se sur les apports d{\'e}tritiques mioc{\`e}nes dans l\&rsquo;Aur{\`e}s Nord},
	journal = {Communication au 1er S{\'e}minaire National des Sciences de la Terre au Service du D{\'e}veloppement durable. Universit{\'e} Cheikh Larbi Tebessi/ T{\'e}bessa 26/27 Avril},
	year = {2004},
	author = {Marmi Ramdane and DJAIZ Fouad}
}
@proceedings {2779,
	title = {Pal{\'e}o-environnement des calcaires {\`a} Rudistes d\&rsquo;{\^a}ge Coniacien inf{\'e}rieur (Berriche) des Monts de Belezma (Alg{\'e}rie orientale)},
	journal = {Communication au 1er S{\'e}minaire National des Sciences de la Terre au Service du D{\'e}veloppement durable. Universit{\'e} Cheikh Larbi Tebessi/ T{\'e}bessa 26/27 Avril},
	year = {2004},
	author = {Yahiaoui K and Inal Ahmed and DJAIZ Fouad}
}
@proceedings {2775,
	title = {Salinit{\'e} des eaux souterraines de la r{\'e}gion Est de la plaine d\&$\#$39;El-Outaya},
	journal = { Colloque international, terre, eau Annaba du 04 au 06 d{\'e}cembre. Dpt des sciences de la terre. Univ de Annaba},
	year = {2004},
	author = {Brinis Nafaa and Djabri Larbi and Kardache Ramdane}
}
@proceedings {2433,
	title = {Approche statistique de l\&rsquo;Influence des caract{\'e}ristiques physiques des bassins versants sur les {\'e}coulements aux exutoires},
	journal = {Communication orale, Journ{\'e}es d{\textquoteright}2tudes sur les Risques Naturels : Inondations, Pr{\'e}vision, Protection. Batna, Alg{\'e}rie, 15-16 D{\'e}cembre},
	year = {2004},
	author = {MENANI Mohamed redha and BENNEDJAI N}
}
@proceedings {2323,
	title = {Salinit{\'e} des eaux souterraines de la r{\'e}gion Est de la plaine d\&$\#$39;El-Outaya},
	journal = {Colloque international, terre, eau Annaba du 04 au 06 d{\'e}cembre. Dpt des sciences de la terre. Univ de Annaba},
	year = {2004},
	author = {Brinis Nafaa and Djabri Larbi and Kardache Ramdane}
}
@proceedings {2322,
	title = {Origines de la salinit{\'e} des eaux de la nappe phr{\'e}atique de la basse Vall{\'e}e de l\&rsquo;Oued Mya (Ouargla)},
	journal = {Journ{\'e}es scientifiques alg{\'e}ro-francaises (colloque de Ouargla JSAF2004). Univ de Ouargla},
	year = {2004},
	author = {Nezli IE and Brinis Nafaa and Labar S}
}
@proceedings {2097,
	title = {Etude de la pollution de la plaine alluviale de la plaine d\&rsquo;El Madher par les rejets de la ville de Batna (Nord-Est Alg{\'e}rie)},
	journal = {Communication orale, Colloque International Terre et Eau, Annaba, Alg{\'e}rie, 04-06 D{\'e}cembre},
	year = {2004},
	pages = {pp372-375},
	address = {Annaba, Alg{\'e}rie},
	author = {MENANI Mohamed redha and Zouita N}
}
@proceedings {2096,
	title = {Influence des param{\`e}tres physiques sur les d{\'e}bits aux exutoires des bassins versants},
	journal = {Communication orale, Colloque International Terre et Eau, Annaba, Alg{\'e}rie, 04-06 D{\'e}cembre},
	year = {2004},
	pages = {pp 485-488},
	address = {Annaba, Alg{\'e}rie},
	author = {MENANI Mohamed redha and BENNEDJAI N}
}
@proceedings {2095,
	title = {La recharge artificielle et la vuln{\'e}rabilit{\'e} {\`a} la pollution des eaux souterraines : Combinaison des approches pour le choix des sites de recharge},
	journal = {Communication orale, 6{\`e}me Symposium International de l{\textquoteright}eau, Cannes, 29 juin-02 juillet},
	year = {2004},
	address = {Cannes},
	author = {MENANI Mohamed redha}
}
@proceedings {2324,
	title = {La qualit{\'e} chimique des eaux souterraines de la nappe du mio-pliocene d\&rsquo;El Outaya ( Biskra )},
	journal = {Colloque international, eau, oasis, population Biskra du 22 au 24 septembre. Laboratoire LARHYSS . Univ de Biskra },
	year = {2003},
	author = {Brinis Nafaa and Djabri Larbi and Kardache Ramdane}
}
@proceedings {2098,
	title = {Pr{\'e}vention des risques de pollution des eaux souterraines par l\&rsquo;{\'e}valuation et la cartographie de leur vuln{\'e}rabilit{\'e} : Traitement de la m{\'e}thode DRASTIC sous Matlab},
	journal = {Communication orale, Colloque Hydrotop, Marseille, France, 22-24 Oct},
	year = {2003},
	address = {Marseille, France},
	author = {MENANI Mohamed redha}
}
@proceedings {2099,
	title = {Approche du bilan hydrodynamique de l\&rsquo;aquif{\`e}re alluvial de la plaine d\&rsquo;El Madher (Nord-Est alg{\'e}rien) par une mod{\'e}lisation en r{\'e}gime permanent},
	journal = {Communication orale, S{\'e}minaire International en mod{\'e}lisation num{\'e}rique en structures et g{\'e}o mat{\'e}riaux, Batna, Alg{\'e}rie, 22-24 Oct},
	year = {2001},
	pages = {pp 340-353},
	address = {Batna, Alg{\'e}rie},
	author = {MENANI Mohamed redha}
}
@article {1946,
	title = {Evaluation et cartographie de la vuln{\'e}rabilit{\'e} {\`a} la pollution de l\&rsquo;aquif{\`e}re alluvionnaire de la plaine d\&rsquo;El Madher, Nord-Est alg{\'e}rien, selon la m{\'e}thode DRASTIC, John Libbey Eurotext France.},
	journal = {S{\'e}cheresse},
	volume = {Vol.12},
	number = {n{\textdegree}2},
	year = {2001},
	pages = { pp.95-101},
	abstract = {
	
		La cartographie de la vuln{\'e}rabilit{\'e} {\`a} la pollution des eaux souterraines permet d{\textquoteright}identifier les zones {\`a} haut risque de contamination, ind{\'e}pendamment du type de polluant. Elle devrait en principe conditionner les plans d{\textquoteright}occupation des sols ou, du moins, permettre de cibler les zones o{\`u} des mesures rigoureuses de protection devraient {\^e}tre adopt{\'e}es. La m{\'e}thode Drastic, qui a {\'e}t{\'e} d{\'e}velopp{\'e}e en 1987 aux {\'E}tats-Unis par la NWWA (Natural Water Well Association), permet cette approche. C{\textquoteright}est une m{\'e}thode standardis{\'e}e d{\textquoteright}{\'e}valuation et de cartographie de la vuln{\'e}rabilit{\'e} des eaux souterraines ind{\'e}pendamment du type de polluant et qui prend en compte la majeure partie des facteurs hydrog{\'e}ologiques qui affectent et contr{\^o}lent l{\textquoteright}{\'e}coulement des eaux souterraines : la profondeur de l{\textquoteright}eau, la recharge efficace, les mat{\'e}riaux de l{\textquoteright}aquif{\`e}re, le type de sol, la topographie, l{\textquoteright}impact de la zone vadose (zone a{\'e}r{\'e}e) et la perm{\'e}abilit{\'e} de l{\textquoteright}aquif{\`e}re. Ces facteurs sont repr{\'e}sent{\'e}s par des poids et des cotes qui d{\'e}pendent respectivement de leur importance relative et des conditions hydrog{\'e}ologiques locales. La combinaison des poids et cotes des divers param{\`e}tres aboutit {\`a} une valeur num{\'e}rique qui est l{\textquoteright}indice Drastic. La cartographie de l{\textquoteright}indice de vuln{\'e}rabilit{\'e} repose sur la superposition de 7 cartes indicielles. Si le mode manuel, long et fastidieux, para{\^\i}t inadapt{\'e} pour cette op{\'e}ration, la cartographie automatique par des logiciels qui traitent la variation progressive d{\textquoteright}un param{\`e}tre ne peut {\'e}galement repr{\'e}senter valablement le ph{\'e}nom{\`e}ne, du fait que l{\textquoteright}indice de vuln{\'e}rabilit{\'e} est attribu{\'e}e {\`a} la zone elle-m{\^e}me et non pas {\`a} son contour. L{\textquoteright}utilisation de matrices de calcul dont les {\'e}l{\'e}ments repr{\'e}sentent le domaine discr{\'e}tis{\'e} permet une cartographie rigoureuse de la vuln{\'e}rabilit{\'e} {\`a} la pollution. Cet article repr{\'e}sente une application de cette m{\'e}thode {\`a} l{\textquoteright}aquif{\`e}re alluvionnaire de la plaine d{\textquoteright}El Madher qui est situ{\'e}e {\`a} environ 15 km au nord-est de la ville de Batna. La cartographie de l{\textquoteright}indice Drastic par l{\textquoteright}utilisation de matrices sous Matlab a permis de d{\'e}limiter les zones vuln{\'e}rables {\`a} la pollution.
	

},
	url = {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\&type=text.html},
	author = {MENANI Mohamed redha}
}
@proceedings {2781,
	title = {Etude p{\'e}tro-structurale de la bordure sud est du socle de la Petite Kabylie \&ndash;r{\'e}gion de Sidi Mezghiche, Alg{\'e}rie},
	journal = {Communication au 4eme S{\'e}minaire de G{\'e}ologie P{\'e}troli{\`e}re/CRD/ Minist{\`e}re des {\'e}nergies 13,14 et 15 Novembre Boumerdes},
	year = {2000},
	author = {DJAIZ Fouad and Mahdjoub Y}
}
@article {1992,
	title = {Caract{\'e}risation du syst{\`e}me aquif{\`e}re alluvionnaire de la plaine d\&$\#$39;El Madher (Nord-Est Alg{\'e}rien) en vue de l\&rsquo;expression de son bilan hydrodynamique au moyen d\&rsquo;un mod{\`e}le de simulation en r{\'e}gime permanent.},
	journal = {Bulletin du Service G{\'e}ologique de l{\textquoteright}Alg{\'e}rie},
	volume = {Vol.11},
	number = {n{\textdegree}1},
	year = {2000},
	pages = {pp. 107-117},
	abstract = {L objectif de cet article est la caract{\'e}risation de l aquif{\`e}re alluvionnaire de la plaine d{\textquoteright}El Madher qui est situ{\'e}e {\`a} environ 15 Kms au Nord-Est de la ville de Batna et {\`a} 450 Kms au SudEst d{\textquoteright}Alger, en vue d{\textquoteright}exprimer par la suite son bilan hydrodynamique au moyen d{\textquoteright}un mod{\`e}le de simulation des {\'e}coulements souterrains en r{\'e}gime permanent. La caract{\'e}risation d{\'e}taill{\'e}e du syst{\`e}me aquif{\`e}re du point de vue g{\'e}ologique, morphologique, structural et hydrodynamique, a permis de d{\'e}terminer l{\textquoteright}ensemble des conditions aux limites et des conditions internes pr{\'e}conis{\'e}es pour la mise en oeuvre de la simulation.},
	url = {https://www.asjp.cerist.dz/en/article/5041},
	author = {MENANI Mohamed redha}
}
@article {1950,
	title = {Simulation en r{\'e}gime permanent des {\'e}coulements souterrains de l\&rsquo;aquif{\`e}re alluvionnaire de la plaine d\&rsquo;El Madher (Nord-Est Alg{\'e}rien), Rock View Ltd 2000, France.},
	journal = {Africa Geosciences Review},
	volume = {Vol.7},
	number = {n{\textdegree} 4},
	year = {2000},
	pages = {pp. 383-392},
	url = {https://scholar.google.com/citations?user=GKY-YYAAAAAJ\&hl=en\&oi=sra},
	author = {MENANI Mohamed redha}
}
@proceedings {2103,
	title = {Groundwater pollution potential in the valley of the Oued Seybouse, NE Algeria},
	journal = {Intern. Conf. On Geochemistry, Alex. thCommunication orale, 4Univ., Egypt, 15-16 Sept},
	year = {1999},
	pages = {pp 389-400},
	address = { Egypt},
	author = {Djabri Larbi and MENANI Mohamed redha}
}
@proceedings {2102,
	title = {Identification des aquif{\`e}res profonds par la prospection electrique. Application {\`a} l\&rsquo;Est Alg{\'e}rien},
	journal = {Communication orale 2{\`e}me Colloque International sur l{\textquoteright}Eau et l{\textquoteright}Environnement, Agadir, Maroc, 25-27 fev},
	year = {1999},
	address = { Agadir, Maroc},
	author = {Boudoukha Abderahmane and El Dounia A and MENANI Mohamed redha}
}
@proceedings {2101,
	title = {Using matrices for mapping the groundwater pollution potential. Case of the DRASTIC method applied to the El Madher plain (North East of Algeria)},
	journal = {Communication orale, 4th Intern. Conf. On Geochemistry, Alex. Univ., Egypt, 15-16 Sept},
	year = {1999},
	address = { Alex. Univ., Egypt},
	author = {MENANI Mohamed redha and Djabri Larbi}
}
@proceedings {2100,
	title = {Evaluation et cartographie de la vuln{\'e}rabilit{\'e} {\`a} la pollution des eaux souterraines selon la m{\'e}thode DRASTIC. Cas de la plaine d\&rsquo;El Madher (Nord-Est Alg{\'e}rien)},
	journal = {Communication orale 2{\`e}me Colloque International sur l{\textquoteright}Eau et l{\textquoteright}Environnement, Agadir, Maroc, 25-27 fev},
	year = {1999},
	address = {Agadir, Maroc},
	author = {MENANI Mohamed redha and Boudoukha Abderahmane}
}
@article {1953,
	title = {Cartographie de la vuln{\'e}rabilit{\'e} {\`a} la pollution des eaux souterraines selon la m{\'e}thode DRASTIC. Cas de la plaine d\&rsquo;El Madher (Nord-Est Alg{\'e}rien), Janvier 1999, Alger.},
	journal = {Bulletin International de l{\textquoteright}Eau et de l{\textquoteright}Environnement - EDIL Infeau},
	number = { n{\textdegree} 21},
	year = {1999},
	author = {MENANI Mohamed redha}
}
@proceedings {2434,
	title = {La cartographie de la vuln{\'e}rabilit{\'e} des eaux souterraines : Outil de gestion et d\&rsquo;am{\'e}nagement des bassins versants},
	journal = {Communication S{\'e}minaire Scientifique et Technique sur les Bassins Versants, Batna 03-04 D{\'e}cembre},
	year = {1998},
	author = {MENANI Mohamed redha}
}
@article {1993,
	title = {Mod{\'e}lisation en r{\'e}gime permanent des {\'e}coulements souterrains de l\&$\#$39;aquif{\`e}re alluvionnaire de la plaine d\&$\#$39;El Madher (Nord-Est alg{\'e}rien).},
	journal = {Bulletin du Service G{\'e}ologique de l{\textquoteright}Alg{\'e}rie},
	volume = {Vol.9},
	number = {n{\textdegree} 2},
	year = {1998},
	pages = {pp. 201-213},
	abstract = {La plaine d El Madher est un bassin s{\'e}dimentaire {\`a} remplissage alluvionnaire mio-plioquaternaire qui est le si{\`e}ge d un {\'e}coulement souterrain. Elle est situ{\'e}e {\`a} environ 15 Kms au NordEst de la ville de Batna dont elle constitue un des champs de captage. La caract{\'e}risation de cet aquif{\`e}re a permis notamment de d{\'e}terminer les conditions aux limites du syst{\`e}me et les conditions internes (zones de transmissivit{\'e}s et pr{\'e}l{\`e}vements) . Apr{\`e}s un test de coh{\'e}rence concluant sur cette base de donn{\'e}es , la mod{\'e}lisation des {\'e}coulements souterrains en r{\'e}gime permanent par la m{\'e}thode des diff{\'e}rences finies a permis d aboutir au calage de la pi{\'e}zom{\'e}trie de r{\'e}f{\'e}rence de la nappe et {\`a} l {\textquoteright}approche de l{\textquoteright}expression de son bilan hydrodynamique moyen annuel.},
	url = {https://www.asjp.cerist.dz/en/article/9101},
	author = {MENANI Mohamed redha}
}
@proceedings {2436,
	title = {Diagnostic et R{\'e}novation des forages},
	journal = {S{\'e}minaire National sur l{\textquoteright}Hydraulique, Universit{\'e} de Biskra, D{\'e}cembre },
	year = {1994},
	author = {MENANI Mohamed redha}
}
@proceedings {2437,
	title = {Pi{\'e}zom{\'e}trie de la nappe phr{\'e}atique de la plaine de Ain Touta  (Alg{\'e}rie orientale)},
	journal = {Communication orale, S{\'e}minaire national sur l{\textquoteright}Hydraulique et l{\textquoteright}environnement, Batna},
	year = {1987},
	author = {MENANI Mohamed redha}
}
