<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Righi Asma</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution au Suivi piézométrique et hydrochimie  dans la plaine de Belezma (W, de Batna)</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Touahria Kamel</style></author><author><style face="normal" font="default" size="100%">Khabar Ali</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Étude stratigraphique et sédimentologique du Campanien supérieur du massif d&amp;#39;El Kantara</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Toumi.A</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à l&amp;rsquo;étude hydrogéologique de la nappe Mio-Pliocène de la région de Tolga</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Ghemima. Z</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Impact des plans d&amp;rsquo;eau artificiels sur les régimes hydrologiques - Cas du barrage de beni haroune - mila - Est algérien</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Azizi Yacine</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Les effondrements dans les terrains karstiques du plateau de Cheria (NE de l&amp;#39;Algérie), impacts gotechnique et environnementaux et cartographie des zones vulnérables au phénomène.</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://www.secheresse.info/spip.php?article79566</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Les effondrements des cavités souterraines dans les calcaires karstifiés constituent un aléa géologique sérieux qui continue à recevoir une intention particulière à l’échelle de la planète. Il s’agit d’un phénomène très connus, lié à la présence de vides souterrains dans les terrains calcaires, dolomitiques et gypsifères. Le plateau de Chéria correspond à une structure synclinale, grossièrement triangulaire d’orientation NE – SW affecté par une fracturation orthogonale à l‘axe du pli. Il est essentiellement formé de calcaires Eocène largement karstifié et recouvert de matériaux meubles, essentiellement des alluvions, des argiles et des encroutements calcaires. Ce bassin en question abrite trois aquifères superposés, l’aquifère du Maastrichtien, l’Eocène et la nappe alluviale du Moi-Plio-Quaternaire. Celle qui fait l’objet de cette étude est la nappe de l’Eocène. Le sens d’écoulement générale dans les nappes souterraines notamment les alluvions et l’Eocène est sensiblement Nord-Sud. La surexploitation actuelle des eaux souterraines a rendu la nappe des alluvions sans intérêt hydrogéologique, et a causé un grand rabattement dans les calcaires de l’Eocène. Les méthodes directes et indirectes d’explorations du sous-sol de la région ont révélés la présence de plusieurs cavités souterraines de dimensions importantes. La méthode de tomographie électrique, Géoradar et les sondages mécaniques ont montré l’existence à faible profondeur des cavités dans la région d’étude. La stabilité de ces cavités dépend d’un côté des propriétés mécaniques de la masse rocheuse formant le toit de la galerie, et les dimensions de cette dernière. Cette étude nous a permis d’établir des relations entre l’épaisseur du toit, largeur de cavité, et la charge pour un RMR (Rock masse rating) variable. La cartographie menée à l’échelle de la région a pu délimiter les zones susceptibles de présenter des cavités naturelles instables et cela va permet en conséquence de trouver des solutions au problème de l’effondrement à l’échelle de la région</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Chafou Nasereddine</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">APPROCHES HYDROGEOCHIMIQUES ET GEOTHERMOMETRIQUES POUR L&amp;rsquo;ETUDE DES EAUX THERMALES  CAS DU SYSTEME GEOTHERMAL EXPLOITE DANS LA REGION DE BISKRA AU SUD ALGERIEN</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Benmansour Sana</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Étude tectono-sédimentaire de la série campanienne de Dj. Lekhal (plaine d&amp;#39;ain Touta)</style></title><secondary-title><style face="normal" font="default" size="100%">La 4eme édition du Congrès des Doctorants 2017 de la FSTGAT se tiendra le 24 et 25 Avril 2017, &amp;aacut la maison de la science, USTHB, Alger</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Slami Rafika</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Sedimentology, Geochemistry and Various Microfaunal Component Responses to Environmental Fluctuations of the Cenomanian-Turonian Boundary at Thénièt El Manchar (Batna, NE Algeria)</style></title><secondary-title><style face="normal" font="default" size="100%">19th International Conference on Geological and Earth Sciences, Word Academy of Science Energinee Ring and Technology, Rome, Italy </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Belalit Halima</style></author><author><style face="normal" font="default" size="100%">Guemima. Z</style></author><author><style face="normal" font="default" size="100%">Toufaha. S</style></author><author><style face="normal" font="default" size="100%">Kihel. K</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Les impactes des plans d&amp;rsquo;eaux artificielles sur les régimes climatiques et hydrologiques à l&amp;rsquo;échelle. Cas d&amp;rsquo;un bassin versant du barrage de Beni Haroune, (Mila Est Algérien)</style></title><secondary-title><style face="normal" font="default" size="100%">Colloque International Eau-Société-Climat 2017(ESC- 2017) Hammamet 2-3-4 Octobre 2017.</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Géométrie de l&amp;rsquo;aquifère Néogène dans le bassin d&amp;rsquo;El Outaya, Atlas saharien au sud algérien</style></title><secondary-title><style face="normal" font="default" size="100%">Colloque International Eau-Société-Climat 2017(ESC- 2017) Hammamet 2-3-4 Octobre 2017</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">caracterisation hydrogeologique et hydro-chimique du bassin neogene de timgad (nord-est algerien)</style></title><secondary-title><style face="normal" font="default" size="100%">The 1st International Symposium (WREIANA 2017) Water Resources and Environmental Impact Assessment in North Africa, Gafsa, Tunisie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Lebchek Soumia</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation hydrogéologique et hydrochimique du bassin néogèn,e de Timgad, NE algérien</style></title><secondary-title><style face="normal" font="default" size="100%">1er International symposium - WREIANA, 24-26, Gafsa, Tunisie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Benmansour Sana</style></author><author><style face="normal" font="default" size="100%">Yahiaoui Abdelouahab</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Le campanien -Maastrichtien du bassin des Aurès, Algérie: Biostratigraphie, Paléoenvironnements et leurs implications.</style></title><secondary-title><style face="normal" font="default" size="100%">Annal de paléontologie , Science Direct-Elsevier masson France</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://doi.org/10.1016/j.annpal. 2017.11.001</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Mansouri Zineb</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">EVALUATION OF THE WATER NEEDS OF CROPS UNDER ARID CLIMATIC CONDITIONS. CASE OF TINIBAOUINE REGION (NORTH EAST OF ALGERIA), Feb, ISSN / e-ISSN: 2186-2990 / 2186-2990 </style></title><secondary-title><style face="normal" font="default" size="100%">International Journal of GEOMATE</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.researchgate.net/publication/313316435_Assessment_of_the_water_needs_of_apricot_and_olive_crops_under_arid_climatic_conditions_Case_study_of_Tinibaouine_region_Northeast_of_Algeria</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Vol. 12</style></volume><pages><style face="normal" font="default" size="100%">pp. 1 - 7</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">The Tinibaouine region, located in north-eastern Algeria on the borders of the Batna-Belezma Mountains, is characterized by a semi-arid to arid climate with an average annual rainfall not exceeding 465 mm and an average annual temperature of around 22 C. This region is characterized by the cultivation of apricots as essential crop followed by that of olives, whose plots are all irrigated with the Tinibaouine spring water. These are 450 Ha of trees for apricot and 108 Hectare for olives which constitute the principal revenue of the citizens of this small village. This paper estimated the crop reference and actual evapotranspiration (ETO) respectively and the irrigation water requirement of apricot trees and olive trees. The long recorded climatic data, crop and soil data, effective water allocation and planning, the information about crop water requirements, irrigation withdrawals were computed with the Cropwat model which is based on the United Nations’ Food and Agriculture Organization (FAO), the Penman-Monteith method was used to estimate ETo. Crop coefficients (Kc) from the phenomenological stages of apricot and olive were applied to adjust and estimate the actual evapotranspiration ETc through a water balance of the irrigation water requirements (IR). The results showed that the annual reference evapotranspiration (ETO) was estimated at 3.71 mm/day. The irrigation requirements were estimated at 35800 m3/hectare for apricot, 6980 m3/hectare for olive, also Irrigation needs estimated on land at 14185, 05 m3/hectare for olive and apricot.</style></abstract><issue><style face="normal" font="default" size="100%">Issue 30</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Bentahar Fahima</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etudes sédimentologiques de la série coniacienne du Dj Metlili (Algerie nord oriental)</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brikat</style></author><author><style face="normal" font="default" size="100%">Sehtal Sami</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude Paléo-Environnemental de la Région de Ain Touta Au Quaternaire : Terrasses Fluviatiles d&amp;rsquo;Oued El Hai.</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Bekkari Sif eddine</style></author><author><style face="normal" font="default" size="100%">Adel Abdelhak</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude Paléo-Environnemental de la Région d&amp;rsquo;El Mather Au Quaternaire : Terrasses Fluviatiles d&amp;rsquo;Oued El Gourzi</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Saada Brahim Oussama</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à l&amp;rsquo;étude hydrogéologique de la région du Droh (w) Biskra</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Saber A</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à l&amp;rsquo;étude hydrogéologique du champ captant de l&amp;rsquo;oued Biskra</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Drias Tarek</style></author><author><style face="normal" font="default" size="100%">Fehdi Chemseddine</style></author><author><style face="normal" font="default" size="100%">Belloula Moufida</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">hydrochemical analysis and evaluation of groundwater quality of an alluvial aquifer. algeria</style></title><secondary-title><style face="normal" font="default" size="100%">1st Euro-Mediterranean Conference for Environmental Integration (EMCEI) Springer, Sousse. Tunisia</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.emcei.net</style></url></web-urls></urls><pub-location><style face="normal" font="default" size="100%">Sousse. Tunisia</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Qualité chimique des eaux de l&amp;rsquo;aquifère Moi-pliocène utilisé pour l&amp;rsquo;irrigation de la plaine d&amp;rsquo;El Outaya au sud Algérien</style></title><secondary-title><style face="normal" font="default" size="100%">Colloque International Eau-Société-Climat 2017(ESC- 2017) Hammamet 2-3-4 Octobre </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Zouaoui Siham</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">Bouabid Abd Ennasser</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Qualité des eaux du Complexe Terminale du Nord-Est Algérien. Région de Tolga</style></title><secondary-title><style face="normal" font="default" size="100%">The 1St Atlas Georessources International Congress, (AGIC). 20-22 March, Hammet, Tunisia.</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><pub-location><style face="normal" font="default" size="100%"> Hammet, Tunisia.</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Benzagouta Mohammed Said</style></author><author><style face="normal" font="default" size="100%">Belhouchet Houssam</style></author><author><style face="normal" font="default" size="100%">Achi. N</style></author><author><style face="normal" font="default" size="100%">Amro.M</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Rock Typing: Reservoir Determination from rock &amp;ndash; fluid interaction and dynamic behavior : Case Study from an Algerian Oil Field Reservoir</style></title><secondary-title><style face="normal" font="default" size="100%">DGMK/ÖGEW-Frühjahrstagung, Fachbereich Aufsuchung und Gewinnung Celle, 5./6. April</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;
	Rock typing is a process of rock classification based on mineralogical composition, grainshape pore size distribution (PSD) and communication. In addition to rock-fluid interaction, dynamic behavior and the capillary effect are also considered. In that purpose data need process involve: integrating, analyzing and synthesizing data brought out from different source: Petrophysics, cores analysis, well tests, MDT tooland production profiles. Achievement of rock typing reservoir based on fluid - solid behavior and their relation constitute an important issue not only for making distinguished different rock types but also for fluid gas contacts.&lt;br&gt;For the case study, our investigation is concerned with the determination of the rock type dynamism resulting in reservoir rocks having similar dynamic behavior. Outcome from this process is to establish a representative petrophysical model able to predict any effect own to the change of the rock properties or fluid characteristics. Establishment of numerical model in&amp;nbsp; that context, and its relative changes can be ascribed to rapid petrophysical variation characteristics: related to pore size, geometry, grain size distribution, fluid behavior and circulation with essential reference to permeability. This latter can affect the simulation time and consequently, the accuracy in the calculation process.
&lt;/p&gt;

&lt;p&gt;
	In this conducted investigation, application of linear regression method is involving permeability and porosity core measurement, stressing on their coefficient of correlation. Results have led to different clusters classification according to the linearity regarding permeability-porosity changes. Extrapolation can be made for the non-cored reservoir sections or non-cored boreholes associated to the considered field. In that principle geological models can be set.
&lt;/p&gt;

&lt;p&gt;
	Application of these listed method for TAGI (TriasArgilo-GreseuxInferieur: Lower Shaly – SansdtoneTriasic Formation) in B-H Basin (Algeria) has revealed the presence of six main rock types: sand type 1 (RT-1), sand Type 2 (RT-2), sand type 3 (RT-3), sand type 4 (RT-4), sand type 5 (RT-5) and sand type 6 (RT-6).
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Defaflia Nabil</style></author><author><style face="normal" font="default" size="100%">Boushaba Abdellah</style></author><author><style face="normal" font="default" size="100%">Marmi Ramdane</style></author><author><style face="normal" font="default" size="100%">Dardakhe Mohamed</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Malika</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation géologique et apport de la géophysique pour la mobilisation des ressources hydrique dans le bassin d&amp;#39;Ain Djasser (Sud-setifien, Algérien NE)</style></title><secondary-title><style face="normal" font="default" size="100%">Colloque international Eau–Société–Climat’2017 (ESC-2017), Hammamet, Tunis le 2, 3 et 4 Octobre .</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><pub-location><style face="normal" font="default" size="100%">Hammamet, Tunis</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Bilalite Halima</style></author><author><style face="normal" font="default" size="100%">Ghenima Z</style></author><author><style face="normal" font="default" size="100%">Teffaha S</style></author><author><style face="normal" font="default" size="100%">Kihel K</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Impacts des plans d&amp;#39;Eau sur les régimes hydro-climatiques a l&amp;#39;échelle d&amp;#39;un bassin verssant, cas du barrage de Beni Haroun, Milan Est Algerien</style></title><secondary-title><style face="normal" font="default" size="100%">Colloque international Eau–Société–Climat’2017 (ESC-2017), Hammamet, Tunis le 2, 3 et 4 Octobre</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><pub-location><style face="normal" font="default" size="100%">Hammamet, Tunis</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Géométrie de l&amp;rsquo;aquifère Néogène dans le bassin d&amp;rsquo;El-Outaya, Atlas saharien au sud algérien </style></title><secondary-title><style face="normal" font="default" size="100%">Colloque international Eau–Société–Climat’2017 (ESC-2017), Hammamet, Tunis le 2, 3 et 4 Octobre </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><pub-location><style face="normal" font="default" size="100%">Hammamet, Tunis </style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Qualité chimique des eaux de l&amp;rsquo;aquifère Mio-pliocène utilisées pour l&amp;rsquo;irrigation de la plaine d&amp;rsquo;El-Outaya au sud algérien</style></title><secondary-title><style face="normal" font="default" size="100%">Colloque international Eau–Société–Climat’2017 (ESC-2017),Hammamet, Tunis le 2, 3 et 4 Octobre </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><pub-location><style face="normal" font="default" size="100%">Hammamet, Tunis </style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Boulahbal Souad</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation des écoulements souterrains dans le socle precambrien fissure  de la region de tamanrasset</style></title><secondary-title><style face="normal" font="default" size="100%">The 1st international symposium WREIANA, Gafsa 24-26 mars </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><pub-location><style face="normal" font="default" size="100%"> Gafsa </style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Boulahbal Souad</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude des ecoulements souterrains dans les gneiss schisteux fissurés du précambrien de la region de tamanrasset</style></title><secondary-title><style face="normal" font="default" size="100%">The 1st Atlas Georesources International Congress, Hammamet, tunisia 20-22 mars</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><pub-location><style face="normal" font="default" size="100%">Hammamet, tunisia</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Mansouri Zineb</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Assessment of water requirements of olive and apricots trees in Tinibaouine region (north-eastern of Algeria). Impacts of Global Change on Western Mediterranean Aquifers,</style></title><secondary-title><style face="normal" font="default" size="100%">Proceedings Congress on Groundwater and Global Change in the Western Mediterranean, Granada </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://www.aih-ge.org/index.php/gwm-change-2017/</style></url></web-urls></urls><pub-location><style face="normal" font="default" size="100%">Granada </style></pub-location><pages><style face="normal" font="default" size="100%">pp 277-282</style></pages><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Bilalite Halima</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Influence des variations climatiques sur les réserves d&amp;rsquo;eau souterraine des plaines de Zana Chott Saboun et Gadaine (Nord-Est Algérien)</style></title><secondary-title><style face="normal" font="default" size="100%">Proceedings Congress on Groundwater and Global Change in the Western Mediterranean Granada. Impacts of Global Change on Western Mediterranean Aquifers</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://www.aih-ge.org/index.php/gwm-change-2017/</style></url></web-urls></urls><pub-location><style face="normal" font="default" size="100%">Granada</style></pub-location><pages><style face="normal" font="default" size="100%">pp 171-176</style></pages><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">BOUHADEB</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">BOUGUERRA H</style></author><author><style face="normal" font="default" size="100%">DERDOUS O</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Assessing soil loss using GIS based RUSLE methodology. Case of the Bou Namoussa watershed &amp;ndash; North-East of Algeria, 2018, PL ISSN 1429&amp;ndash;7426., Polish Academy of Sciences (PAN), Committee on Agronomic Sciences, Degruyte, DOI: 10.2478/jwld-2018</style></title><secondary-title><style face="normal" font="default" size="100%">Journal of Water and Land Development </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://www.itp.edu.pl/wydawnictwo/journal/36_2018_I_III/Bouhadeb.pdf</style></url></web-urls></urls><pages><style face="normal" font="default" size="100%">pp 27–35</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;span style=&quot;left:131.333px;top:688.416px;14.9711px;serif;transform:scaleX(1.00015);&quot;&gt;This study aims to estimating annual soil erosion rate and its &lt;/span&gt;&lt;span style=&quot;left:497.629px;top:688.416px;14.9711px;serif;transform:scaleX(1.00136);&quot;&gt;spatial distribution in the Bou Namoussa water-&lt;/span&gt;&lt;span style=&quot;left:105.963px;top:705.538px;14.9711px;serif;transform:scaleX(1.03121);&quot;&gt;shed located in the North-East of Algeria by applying the revis&lt;/span&gt;&lt;span style=&quot;left:493.416px;top:705.538px;14.9711px;serif;transform:scaleX(1.02336);&quot;&gt;ed universal soil loss equation (RUSLE) within &lt;/span&gt;&lt;span style=&quot;left:105.963px;top:722.751px;14.9711px;serif;transform:scaleX(0.998512);&quot;&gt;a Geographical Information System environment (GIS). The applic&lt;/span&gt;&lt;span style=&quot;left:507.581px;top:722.751px;14.9711px;serif;transform:scaleX(0.999618);&quot;&gt;ation of the RUSLE model in different natural &lt;/span&gt;&lt;span style=&quot;left:105.963px;top:739.963px;14.9711px;serif;transform:scaleX(1.00806);&quot;&gt;environments and on every scale takes into account five key fac&lt;/span&gt;&lt;span style=&quot;left:491.354px;top:739.963px;14.9711px;serif;transform:scaleX(1.01094);&quot;&gt;tors namely: the rainfall erosivity, the soil erodi-&lt;/span&gt;&lt;span style=&quot;left:105.963px;top:757.085px;14.9711px;serif;transform:scaleX(1.03489);&quot;&gt;bility, the steepness and length of slopes, the vegetation cove&lt;/span&gt;&lt;span style=&quot;left:482.837px;top:757.085px;14.9711px;serif;transform:scaleX(1.02999);&quot;&gt;r and the conservation support practices. Each of &lt;/span&gt;&lt;span style=&quot;left:105.963px;top:774.298px;14.9711px;serif;transform:scaleX(1.01278);&quot;&gt;these factors was generated in GIS as a raster layer, their com&lt;/span&gt;&lt;span style=&quot;left:478.982px;top:774.298px;14.9711px;serif;transform:scaleX(1.01092);&quot;&gt;bination, resulted in the development of a soil loss &lt;/span&gt;&lt;span style=&quot;left:105.963px;top:791.42px;14.9711px;serif;transform:scaleX(0.988245);&quot;&gt;map indicating an average erosion rate of 7.8 tꞏha&lt;/span&gt;&lt;span style=&quot;left:407.536px;top:789.41px;9.68188px;serif;transform:scaleX(1.00157);&quot;&gt;–1&lt;/span&gt;&lt;span style=&quot;left:417.217px;top:791.42px;14.9711px;serif;transform:scaleX(0.612241);&quot;&gt;ꞏy&lt;/span&gt;&lt;span style=&quot;left:429.678px;top:789.41px;9.68188px;serif;transform:scaleX(1.00157);&quot;&gt;–1&lt;/span&gt;&lt;span style=&quot;left:439.36px;top:791.42px;14.9711px;serif;transform:scaleX(1.01647);&quot;&gt;. The obtained soil loss map was classified into four ero-&lt;/span&gt;&lt;span style=&quot;left:105.963px;top:808.632px;14.9711px;serif;transform:scaleX(1.02139);&quot;&gt;sion severity classes; low, moderate, high and very high severi&lt;/span&gt;&lt;span style=&quot;left:487.32px;top:808.632px;14.9711px;serif;transform:scaleX(1.01543);&quot;&gt;ty representing respectively 40, 30.48, 22.59 and &lt;/span&gt;&lt;span style=&quot;left:105.963px;top:825.845px;14.9711px;serif;transform:scaleX(1.01372);&quot;&gt;6.89% of the total surface. The a&lt;/span&gt;&lt;span style=&quot;left:303.993px;top:825.845px;14.9711px;serif;transform:scaleX(1.00953);&quot;&gt;reas, showing moderate, high a&lt;/span&gt;&lt;span style=&quot;left:491.893px;top:825.845px;14.9711px;serif;transform:scaleX(1.00919);&quot;&gt;nd very high erosion rates which represent more &lt;/span&gt;&lt;span style=&quot;left:105.963px;top:842.967px;14.9711px;serif;transform:scaleX(1.0084);&quot;&gt;than half of the basin area were found generally located in reg&lt;/span&gt;&lt;span style=&quot;left:480.148px;top:842.967px;14.9711px;serif;transform:scaleX(1.00558);&quot;&gt;ions having high erodibility soils, steep slopes and &lt;/span&gt;&lt;span style=&quot;left:105.963px;top:860.179px;14.9711px;serif;transform:scaleX(1.01828);&quot;&gt;low vegetation cover. These areas should be considered as prior&lt;/span&gt;&lt;span style=&quot;left:494.403px;top:860.179px;14.9711px;serif;transform:scaleX(1.01575);&quot;&gt;ities in future erosion control programs in order &lt;/span&gt;&lt;span style=&quot;left:105.963px;top:877.392px;14.9711px;serif;transform:scaleX(0.998794);&quot;&gt;to decrease the siltation rate&lt;/span&gt;&lt;span style=&quot;left:272.795px;top:877.392px;14.9711px;serif;transform:scaleX(1.00459);&quot;&gt; in the Cheffia reservoir. &lt;/span&gt;</style></abstract><issue><style face="normal" font="default" size="100%">No. 36 (I–III)</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJEMMAL S</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">CHAMEKH K</style></author><author><style face="normal" font="default" size="100%">BAALI F</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">The contribution of fracturations in the emergence of the thermal springs in Setif city, Eastern Algeria, Carbonates Evaporites</style></title><secondary-title><style face="normal" font="default" size="100%">Springer</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.researchgate.net/publication/318603314_The_contribution_of_fracturations_in_the_emergence_of_the_thermal_springs_in_Setif_city_Eastern_Algeria</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Setif city covers an area of 6550&amp;nbsp;km&lt;sup&gt;2&lt;/sup&gt;; it is located about 300&amp;nbsp;km southeast of Algiers and 100&amp;nbsp;km to the south of the Mediterranean sea. The aim of our study is to know the tectonic mechanisms responsible for the emergencies and to highlight their chemical characteristics of water springs in Setif. Wherein thermalism is characterized by the presence of a number of thermal springs, the latest are usually related to recent large fractures deeply affecting the sedimentary formations and sometimes even crystallin basement. These fractures are often injected by Triassic evaporates; their directions are NNW–SSE, NW–SE, and NE–SW and limiting great structural units. Four groundwater facies were identified: the high percentage of sources, staking major accidents related to limestone mountains or to the basement, shows a calcium or sodium sulfate facies; and the sources are often hot (meso or hyperthermal). A second group, related to terrigenous saliferous formations, shows a sodium bicarbonate or sodium chloride facies. The geothermic interpretation allows us to conclude that the reservoir supplies the two aquifer systems of the thermal complex, and is stored in fissured Jurassic limestone, where water storage and circulation is beyond 2600&amp;nbsp;m deep.</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Mensouri Z</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Assessment of the water needs of apricot and olive crops under arid climatic conditions: case study of Tinibaouine Region (northeast of Algeria), Special Issue on Science, Engineering &amp;amp; Environment, ISSN: 2186-2990, Japan. Feb,2017</style></title><secondary-title><style face="normal" font="default" size="100%">International Journal of GEOMATE</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.geomatejournal.com/sites/default/files/articles/46-52-160424-Zineb-Feb-2017.pdf</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%"> Vol. 12</style></volume><pages><style face="normal" font="default" size="100%">pp. 46 - 52. </style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;span style=&quot;left:237.991px;top:383.527px;16.6px;serif;transform:scaleX(1.01562);&quot;&gt;The Tinibaouine region, located in north&lt;/span&gt;&lt;span style=&quot;left:515.194px;top:383.527px;16.6px;serif;transform:scaleX(1.01416);&quot;&gt;-eastern Algeria on the borders of the Batna&lt;/span&gt;&lt;span style=&quot;left:810.392px;top:383.527px;16.6px;serif;transform:scaleX(1.00298);&quot;&gt;-Belezma &lt;/span&gt;&lt;span style=&quot;left:141.794px;top:402.534px;16.6px;serif;transform:scaleX(1.01773);&quot;&gt;Mountains, is characterized by a semi&lt;/span&gt;&lt;span style=&quot;left:397.201px;top:402.534px;16.6px;serif;transform:scaleX(1.02308);&quot;&gt;-arid to arid climate with an average annual rainfall not exceeding 465 &lt;/span&gt;&lt;span style=&quot;left:141.794px;top:421.741px;16.6px;serif;transform:scaleX(0.931907);&quot;&gt;mm and an average annual temperature of around 22 ° C. This region is char&lt;/span&gt;&lt;span style=&quot;left:670.188px;top:421.741px;16.6px;serif;transform:scaleX(1.03469);&quot;&gt;acterized by the cultivation of &lt;/span&gt;&lt;span style=&quot;left:141.794px;top:440.947px;16.6px;serif;transform:scaleX(1.01482);&quot;&gt;apricots as essential crop followed by th&lt;/span&gt;&lt;span style=&quot;left:412.191px;top:440.947px;16.6px;serif;transform:scaleX(1.01725);&quot;&gt;at of olives, whose plots are all irrigated with the Tinibaouine spring &lt;/span&gt;&lt;span style=&quot;left:141.794px;top:460.153px;16.6px;serif;transform:scaleX(1.01054);&quot;&gt;water. These are 450 Ha of trees for apricot and 108 Hectare&lt;/span&gt;&lt;span style=&quot;left:546.801px;top:460.153px;16.6px;serif;transform:scaleX(1.00782);&quot;&gt; for olives which constitute the principal revenue &lt;/span&gt;&lt;span style=&quot;left:141.794px;top:479.359px;16.6px;serif;transform:scaleX(0.953916);&quot;&gt;of the citizens of this small village. This paper estimated the crop refe&lt;/span&gt;&lt;span style=&quot;left:631.394px;top:479.359px;16.6px;serif;transform:scaleX(0.97168);&quot;&gt;rence and actual evapotranspiration &lt;/span&gt;&lt;span style=&quot;left:141.794px;top:498.565px;16.6px;serif;transform:scaleX(0.956391);&quot;&gt;(ETO) respectively and the irrigation water requirement of apricot trees an&lt;/span&gt;&lt;span style=&quot;left:654.601px;top:498.565px;16.6px;serif;transform:scaleX(0.939249);&quot;&gt;d olive tree&lt;/span&gt;&lt;span style=&quot;left:732.604px;top:498.565px;16.6px;serif;transform:scaleX(0.937488);&quot;&gt;s. The long recorded &lt;/span&gt;&lt;span style=&quot;left:141.81px;top:517.572px;16.6px;serif;transform:scaleX(0.951769);&quot;&gt;climatic data, crop and soil data, effective water allocation and planning, the information about crop water &lt;/span&gt;&lt;span style=&quot;left:141.81px;top:536.779px;16.6px;serif;transform:scaleX(1.00641);&quot;&gt;req&lt;/span&gt;&lt;span style=&quot;left:163.208px;top:536.779px;16.6px;serif;transform:scaleX(0.949313);&quot;&gt;uirements, irrigation withdrawals were computed with the Cropwat model which is based on the United &lt;/span&gt;&lt;span style=&quot;left:141.81px;top:555.985px;16.6px;serif;transform:scaleX(1.0089);&quot;&gt;Nations’ Food and Agriculture Organization (FAO), the Penman&lt;/span&gt;&lt;span style=&quot;left:574.008px;top:555.985px;16.6px;serif;transform:scaleX(1.01081);&quot;&gt;-Monteith method was used to estimate ETo. &lt;/span&gt;&lt;span style=&quot;left:141.81px;top:575.191px;16.6px;serif;transform:scaleX(0.977037);&quot;&gt;Crop coefficients (Kc) from the phenomenological stag&lt;/span&gt;&lt;span style=&quot;left:525.204px;top:575.191px;16.6px;serif;transform:scaleX(0.957203);&quot;&gt;es of apricot and olive were applied to adjust and &lt;/span&gt;&lt;span style=&quot;left:141.81px;top:594.397px;16.6px;serif;transform:scaleX(1.01635);&quot;&gt;estimate the actual evapotranspiration ETc through a water balance of the irrigation water requirements (IR). &lt;/span&gt;&lt;span style=&quot;left:141.81px;top:613.603px;16.6px;serif;transform:scaleX(1.02307);&quot;&gt;The results showed that the&lt;/span&gt;&lt;span style=&quot;left:327.813px;top:613.603px;16.6px;serif;transform:scaleX(1.02412);&quot;&gt; annual reference evapotranspiration (ETO) was estimated at &lt;/span&gt;&lt;span style=&quot;left:745.005px;top:613.603px;16.6px;serif;transform:scaleX(1.00205);&quot;&gt;3.71mm&lt;/span&gt;&lt;span style=&quot;left:799.801px;top:613.603px;16.6px;serif;transform:scaleX(0.966408);&quot;&gt; / day. The &lt;/span&gt;&lt;span style=&quot;left:141.794px;top:632.61px;16.6px;serif;transform:scaleX(0.983996);&quot;&gt;irrigation requirements were estimated at 35800 &lt;/span&gt;&lt;span style=&quot;left:482.5917999999999px;top:632.6104000000004px;16.6px;serif;&quot;&gt;m&lt;/span&gt;&lt;span style=&quot;left:495.2px;top:632.768px;10.799999999999999px;serif;&quot;&gt;3&lt;/span&gt;&lt;span style=&quot;left:500.6px;top:632.536px;16.6px;serif;transform:scaleX(0.989751);&quot;&gt;/ hectare&lt;/span&gt;&lt;span style=&quot;left:560.609px;top:632.536px;16.6px;serif;transform:scaleX(0.973416);&quot;&gt; for apricot, 6980 &lt;/span&gt;&lt;span style=&quot;left:691.8154px;top:632.5359999999998px;16.6px;serif;&quot;&gt;m&lt;/span&gt;&lt;span style=&quot;left:704.3999999999999px;top:632.768px;10.799999999999999px;serif;&quot;&gt;3&lt;/span&gt;&lt;span style=&quot;left:709.8px;top:632.536px;16.6px;serif;transform:scaleX(0.984352);&quot;&gt;/ hectare &lt;/span&gt;&lt;span style=&quot;left:776.598px;top:632.536px;16.6px;serif;transform:scaleX(0.965348);&quot;&gt;for olive, also &lt;/span&gt;&lt;span style=&quot;left:141.798px;top:651.742px;16.6px;serif;transform:scaleX(1.00386);&quot;&gt;Irrigation needs estimated on land at &lt;/span&gt;&lt;span style=&quot;left:389.005px;top:651.742px;16.6px;serif;transform:scaleX(1.009);&quot;&gt;14185, 05&lt;/span&gt;&lt;span style=&quot;left:455.803px;top:651.742px;16.6px;serif;transform:scaleX(1.00281);&quot;&gt; m&lt;/span&gt;&lt;span style=&quot;left:472.59999999999997px;top:651.968px;10.799999999999999px;serif;&quot;&gt;3&lt;/span&gt;&lt;span style=&quot;left:478px;top:651.736px;16.6px;serif;transform:scaleX(1.00541);&quot;&gt;/ hectare &lt;/span&gt;&lt;span style=&quot;left:539.204px;top:651.736px;16.6px;serif;transform:scaleX(1.00584);&quot;&gt;for olive and apricot&lt;/span&gt;</style></abstract><issue><style face="normal" font="default" size="100%">Issue 30</style></issue></record></records></xml>