<?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%">Belaloui souad</style></author><author><style face="normal" font="default" size="100%">Seba sakina</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">les caracteristiques physicovhimiques des eaux de continentale intercalaire et de complexe ternimale daans la région d&amp;#39;oued Righ</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Nezzar Badreddine</style></author><author><style face="normal" font="default" size="100%">Bezai Abderahim</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution hydrogéologique de la plaine de Ain Djasser</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Guetafi Anfal</style></author><author><style face="normal" font="default" size="100%">Touati Zina</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude Téctono- sédimentaire de la série Campanienne de Dj. Lekhal (Plaine d&amp;rsquo;Ain-Touta)</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Benmansour Sana</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">La série compano-maestrichtienne de l&amp;rsquo;anticlinal de Djebel El Azreg : Lithostratigraphie, Paléodiversité et Sédimentologie (Aurès, Algérie oriental</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Khelil.M</style></author><author><style face="normal" font="default" size="100%">Fedel.W</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude de la qualité des eaux souterraines de la nappe profonde destinées a l&amp;rsquo;irrigation cas de la région de Tolga (W de Biskra)</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Boukhnissa.F</style></author><author><style face="normal" font="default" size="100%">Ahmadi. L</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude de la qualité des eaux souterraines de la nappe du quaternaire de la région de Tolga (W de Biskra)</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Mansouri Zineb</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude hydrogéologique et gestion intégrée des eaux de la source de Tinibaouine (Wilaya de Batna -NE Algérien)</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://www.secheresse.info/spip.php?article67759</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">La région de Tinibaouine est située au Nord-est de l’Algérie, en bordure Septentrionale des Monts de Batna-Belezma, Elle est caractérisée par un climat de type semi-aride à aride avec une précipitation moyenne annuelle qui n’excède pas 465mm, et une température moyenne annuelle de l’ordre de 22°C. Cette région est caractérisée par la culture de l’abricot comme culture essentielle suivie des olives, dont les parcelles sont toutes irriguées à partir de la source. Il s’agit en effet de 450 Ha d’arbres destinés à l’abricotier et de 108 Ha aux olives. L’émergence naturelle des eaux qui ont pour le réservoir Dj. Refaa situé en contrefort Sud de la plaine de Tinibaouine où émerge la source. Son débit actuel est de l’ordre de 100 à 110 l/s (mesuré en Mars 2015) alors qu’il pouvait atteindre 200 l/s par le passé en 1971. L’objectif de ce travail est de cerner les contraintes naturelles et anthropiques ayant une incidence directe sur l’usage de la source et de chercher le mode de gestion approprié, qui tienne compte non seulement des solutions techniques qui s’inspire également des règles sociales qui régissent l’usage et les conflits qui leurs sont liés.</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Mekaoussi Adel</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">ORIGINES ET MÉCANISMES D&amp;#39;ACQUISITION DE LA MINERALISATION DES EAUX SOUTERRAINES EXPLOITEES DANS LES AURES.  Cas de la vallée de l&amp;rsquo;Oued Abdi (w) de Batna (Nord-Est Algérien)</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Slami Rafika</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Stratigraphie, géochimie et réponses microfaunistiques aux changement environnementals autour de la limite Cénomanien-Turonien dans les monts Bellezma-Batna, NE Algérie</style></title><secondary-title><style face="normal" font="default" size="100%">Le 1er Colloque International sur la géologie de la chaîne des Maghrébides et des régions voisines (CIGCM 2016), Université Ferhat Abbas -Sétif 1</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Slami Rafika</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude micropaléontologique (foraminifères, ostracodes) et paléoenvironnementale de la limite Cénomano-Turonienne dans les monts de Batna (Exemple : coupe de Thénièt El Manchar, Nord-Est Algérie)</style></title><secondary-title><style face="normal" font="default" size="100%">1st Arabian Geosciences Union International Conference AIC1, USTHB Alger </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Intérêt de l&amp;rsquo;étude géologique et hydrogéologique pour la mobilisation des ressources hydriques dans le bassin de Timgad (Aurès, algérie NE)</style></title><secondary-title><style face="normal" font="default" size="100%">Le 1er séminaire national sur l’eau et l’environnement (SNEE, 2016). Mila, Algérie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Belalit Halima</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Les variations climatiques sur les eaux souterraines de la plaine de Gadaine (nord-est algérien)</style></title><secondary-title><style face="normal" font="default" size="100%">1er Séminaire National sur l'eau</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Lebchek Soumia</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Approche hydrogéologique du bassin néogène de Timgad, NE algérien</style></title><secondary-title><style face="normal" font="default" size="100%">2nd Ionternational conference on water resources, ICWR, Ouragla, 21-22 Nov </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Rihani Abla</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation hydrochimique et isotopique des eaux souterraines du sous bassin de Oued Labiod, massif des aurès, NE Algérien </style></title><secondary-title><style face="normal" font="default" size="100%">5ème conférence internationale du réseau eaux et climats, Fes, 12-13 Oct </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">IWRM in north Eastern Batna plains</style></title><secondary-title><style face="normal" font="default" size="100%">43rd IAH congress, Montpellier 25-29 sept</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">www.iah.org</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Benmansour Sana</style></author><author><style face="normal" font="default" size="100%">Yahiaoui Abdelouahab</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">The Campaniane Maastrichtian of the Aures basin, Algeria  Paleobiogeographical distrubution of Ostracods</style></title><secondary-title><style face="normal" font="default" size="100%">Elsevier Cretaceous Research </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.1016/j.cretres.2015.09.015</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Vol. 58</style></volume><pages><style face="normal" font="default" size="100%">pp.86-107</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">A detailed biostratigraphic study of four sections (El Kantara, Menaa, Tighanimine and El Gaâga) in the Campanian–Maastrichtian of the Aures Basin in Algeria allows the identification of 109&amp;nbsp;&lt;a href=&quot;https://www.sciencedirect.com/topics/earth-and-planetary-sciences/ostracod&quot; title=&quot;Learn more about Ostracod from ScienceDirect's AI-generated Topic Pages&quot;&gt;ostracod&lt;/a&gt;&amp;nbsp;species belonging to 50 genera. From a biochronostratigraphic point of view, none of the identified ostracod assemblages are typically restricted to the&amp;nbsp;&lt;a href=&quot;https://www.sciencedirect.com/topics/earth-and-planetary-sciences/campanian&quot; title=&quot;Learn more about Campanian from ScienceDirect's AI-generated Topic Pages&quot;&gt;Campanian&lt;/a&gt;&amp;nbsp;or to the&amp;nbsp;&lt;a href=&quot;https://www.sciencedirect.com/topics/earth-and-planetary-sciences/maastrichtian&quot; title=&quot;Learn more about Maastrichtian from ScienceDirect's AI-generated Topic Pages&quot;&gt;Maastrichtian&lt;/a&gt;, but rather characterize a range covering the Campanian–Maastrichtian. As regards the paleobiogeography, the presence of species in common between Algeria and other countries or regions enables us to compile four maps showing the distribution of two provinces that developed during the Santonian-Paleocene, i) the South-West and South Tethyan Margins Province, including North Africa, the Middle East and Arabian Peninsula, and ii) the East Atlantic Margin Province, bordering West and Central-West Africa. We can also recognize relationships between the different regions making up these provinces, which remained under more or less arid, subtropical to tropical climates, with ostracods migrating according to the directions of ocean currents during the&amp;nbsp;&lt;a href=&quot;https://www.sciencedirect.com/topics/earth-and-planetary-sciences/late-cretaceous&quot; title=&quot;Learn more about Late Cretaceous from ScienceDirect's AI-generated Topic Pages&quot;&gt;Late Cretaceous&lt;/a&gt;. The&amp;nbsp;&lt;a href=&quot;https://www.sciencedirect.com/topics/earth-and-planetary-sciences/dispersal&quot; title=&quot;Learn more about Dispersal from ScienceDirect's AI-generated Topic Pages&quot;&gt;dispersal&lt;/a&gt;&amp;nbsp;of the ostracods reflects marine communication between these provinces and India, the southern USA and Jamaica, Brazil and Europe.</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Naji Hossein</style></author><author><style face="normal" font="default" size="100%">Meddour Taib</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Étude géologique de la plaine d&amp;rsquo;El Mather par une approche géophysique.</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Derdakhe Mohamed</style></author><author><style face="normal" font="default" size="100%">Baci Maamer</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Étude géologique de la plaine d&amp;rsquo;Ain Djasser par une approche géophysique.</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Beldjani I</style></author><author><style face="normal" font="default" size="100%">Henni Y</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Traitement des eaux salées -par osmose inverse- pour la production d&amp;#39;eau potable dans le sud algérien / Unité de déminéralisation de Touggourt</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Dif H</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à une étude Comparative entre    la qualité des eaux du Complexe Terminal et du Continental Intercalaire dans la région D&amp;rsquo;EL-OUED.</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Djenba Samir</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">water resources in a semi-arid country case aïn djasser northeast Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">Desalination for Environment : Clean Water and Energy May22–26, Rome-Italy</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><pub-location><style face="normal" font="default" size="100%"> Rome-Italy</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Djenba Samir</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">les problèmes de mouvement de sols nord de wilaya de Sétif</style></title><secondary-title><style face="normal" font="default" size="100%">1er colloque international sur la géologie de la chaine maghrébides et des régions limitrophes Sétif </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">khadidja A</style></author><author><style face="normal" font="default" size="100%">Djenba Samir</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">hydrodynamic caracreization of ground of the region of Tadjnenet- Chelghoum aid (eastern algeria)</style></title><secondary-title><style face="normal" font="default" size="100%">International conference on Applied Geology and Environment May19–21, Mahdia-  Tunisia</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><pub-location><style face="normal" font="default" size="100%">Mahdia-  Tunisia</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Djenba Samir</style></author><author><style face="normal" font="default" size="100%">khadidja A</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Study of the instability of the land : typology and mapping cases of the wilaya of setif (eastern algeria)</style></title><secondary-title><style face="normal" font="default" size="100%">International conference on Applied Geology and Environment May19–21 Mahdia-  Tunisia</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><pub-location><style face="normal" font="default" size="100%">Mahdia-  Tunisia</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Belloula Moufida</style></author><author><style face="normal" font="default" size="100%">Drias Tarek</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Assessment of groundwater quality in the plain of ichemoul using the geomatics approach</style></title><secondary-title><style face="normal" font="default" size="100%">ISER-78th International Conference on Chemical and Environmental Science (ICCES) Zurich, Switzerland November 22nd -23rd</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><pub-location><style face="normal" font="default" size="100%">Zurich, Switzerland </style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Drias Tarek</style></author><author><style face="normal" font="default" size="100%">Belloula Moufida</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Hydrogeochemical assessment of an alluvial aquifer under semi-arid climat. Eastern Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">ISER-78th International Conference on Chemical and Environmental Science (ICCES) Zurich, Switzerland November 22nd -23rd </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><pub-location><style face="normal" font="default" size="100%">Zurich, Switzerland </style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Djenba Samir</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Les problèmes de mouvements de sols au nord de la wilaya de Setif</style></title><secondary-title><style face="normal" font="default" size="100%">1er colloque international sur la géologie de la chaine des maghrébides et des régions voisines (CIGCM 2016), université Ferhat Abbas Setif1 Setif, Alger</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><pub-location><style face="normal" font="default" size="100%">Setif, Alger</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Cheriet Manel</style></author><author><style face="normal" font="default" size="100%">Benzagouta Mohamed Said</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">CONTROLE DES CARACTERISTIQUES PETROPHYSIQUES DES RESERVOIR CARBONATES: CAS DU CONIACIEN &amp;ndash;SANTONIEN(SUD EST CONSTANTINOIS)</style></title><secondary-title><style face="normal" font="default" size="100%">Sciences &amp; Technologie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://revue.umc.edu.dz/index.php/d/article/view/2148/2291</style></url></web-urls></urls><pages><style face="normal" font="default" size="100%">pp 27-40</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Investigation on oil reservoirs is up to several approaches under different aspects. oilreservoir is dependent on several approaches in different aspects. Distinct settings may be considered for the qualitative and quantitative reservoir evaluation. Control on potential reservoir accumulation is related to permeability and poroslty, in addition to diagenetic and petrographic effects. ln the case study, the considered reservoir is dealing with Cretaceous Carbonate series of ConiacianSantonian age located in the South East of Constantine area (Sud-Est Constontinois). From exploration and evaluation point of view, the oil potential, in the cited area levels, remains almost unexplored. Based on logging and drilling collected data indicates that the approached level of Coniancian -Santonian age can be a tight type. Evidences is from the permeability which is ranging from 0.1 md to 50 md and porosity stretching from lYo up to 16%o. Thus, contribution of tectonic effect is minimized. In the same harmony is the diagenetic and petrographic attitude which is responsible for the compaction and lesser dissolution with occlusion mostly of the intergranular.</style></abstract><issue><style face="normal" font="default" size="100%">N°43</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Aoun Mounira</style></author><author><style face="normal" font="default" size="100%">Benzagouta Mohamed Said</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Expansive And Aggressive Soil Characteristics And Their Impact On Building Construction: Case Of El Kouif City (tebessa, Algeria)</style></title><secondary-title><style face="normal" font="default" size="100%">Bulletin du Service Géologique de l'Algérie </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://asga.dz/wp-content/uploads/2019/01/Bulletin-vol-27-2016.pdf</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Volume 27</style></volume><pages><style face="normal" font="default" size="100%">pp 105-121 </style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Prediction of soil swelling characteristics and accurate quality estimation can be of a great consideration and contribution regarding the site stability. Any concerned investigation is correspondingly an advanced priority for the project realization. Related inquiries allow potential reduction concerning financial and technical charges damage prior to any urban development. The determination of soil characteristics lead for a better recognition, and allow to make the best choice of foundation type adopted for each site. Thus, in any urban case study, much gain can be made by team work recording and surveying the related data. In the considered city of El Kouif, located in Tebessa (Algeria), several buildings have been mainly built on expansive soils. Observations indicate different severe damages which were caused mostly in the nearby structures. These damages are characterized by deflection and failure of walls. Lateral and vertical displacements evidences support the presence of shear movements and subsidence. The scale up of these movements occurrence can reach millimetric shifting dimension. Ground and subsurface risk activity affecting El Kouif city site are also related to the presence of destructive chemical components such as sulfates. The sulfate occurrence is illustrated through generally gypsum minerals concentration present in the concerned soil. During building projects, these soils, in meeting concrete and in presence of water, are source of new mineral generation such as ettringite. It consists on the assemblage of water and sulfate in addition to calcium. Source for these chemical products expansion might be associated to historical event: the city of El Kouif was the field of phosphates mining area in addition to established phosphate extraction plant. Thus, determination of soil characteristics and involvement of chemical components turn out to be the main objectives in this investigation.</style></abstract><issue><style face="normal" font="default" size="100%">Numéro 1</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Aptitude a l&amp;#39;irrigation par les eaux uses epurees cas de la STEP de Sidi Merouane, willaya de Mila, Est Algerien</style></title><secondary-title><style face="normal" font="default" size="100%">10th international conference for water ressources and water security in the middle East and North Africa, held in Istanbul, Turkey on th 14th-16th November</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><pub-location><style face="normal" font="default" size="100%">Istanbul, Turkey </style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">les impacts climatiques sur les eaux souterraines, cas de la plaine de Zana-Chott saboun, Est Algerien</style></title><secondary-title><style face="normal" font="default" size="100%">10th international conference for water ressources and water security in the middle East and North Africa, held in Istanbul, Turkey on th 14th-16th November</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><pub-location><style face="normal" font="default" size="100%">Istanbul, Turkey</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Defaflia Nabil</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">Marmi Ramdane</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">L&amp;#39;intéret de l&amp;#39;etude géologique et hydrogéologique pour la mobilisation des ressources hydriques dans le bassin de Timgad (Aures, Algerie Nord oriental)</style></title><secondary-title><style face="normal" font="default" size="100%">1er Séminaire National sur l'eau et l'environnement (SNEE 2016), Centre universitaire Abdelhafid Boussouf, Milla, Alger 28-29 novembre</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><pub-location><style face="normal" font="default" size="100%">Milla, Alger</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">Lehchili Nouh</style></author><author><style face="normal" font="default" size="100%">Benchaoui Amine</style></author><author><style face="normal" font="default" size="100%">Benabdelaziz Noureddine</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Aptitude à l&amp;#39;irrigation par les eaux usées épurées, cas de la STEPde Sidi Merouane, willaya de Mila, Est Algerien</style></title><secondary-title><style face="normal" font="default" size="100%">1er Séminaire National sur l'eau et l'environnement (SNEE 2016), Centre universitaire Abdelhafid Boussouf, Milla, Alger 28-29 novembre</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><pub-location><style face="normal" font="default" size="100%">Milla, Alger</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">Bilalite Halima</style></author><author><style face="normal" font="default" size="100%">Bechar Salah-Eddine</style></author><author><style face="normal" font="default" size="100%">Guesmi Hayat</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Fluctuation du niveau piézométrique des eaux souterraines cas de la plaine de Zana-Chott Saboun, Batna Est Algerien</style></title><secondary-title><style face="normal" font="default" size="100%">1er Séminaire National sur l'eau et l'environnement (SNEE 2016), Centre universitaire Abdelhafid Boussouf, Milla, Alger 28-29 novembre</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><pub-location><style face="normal" font="default" size="100%">Milla, Alger</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Anthropogenic pressures on groundwater resources. Case of the Northern plains of Batna region (North-East Algeria)</style></title><secondary-title><style face="normal" font="default" size="100%">43rd IAH  Congress, 25-29 September, Montpellier, France, </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language><issue><style face="normal" font="default" size="100%">Abstract n° 2701. </style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Defaflia N</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">Marmi R</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Geological, Hydrological and Hydrogeological Characterization of the Timgad&amp;rsquo;s Basin (Aures, Algeriane) for the Mobilization of Water Resources</style></title><secondary-title><style face="normal" font="default" size="100%">International Journal of Environment and Water ISSN 2052-3408</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.researchgate.net/publication/330038879_Geological_Hydrological_and_Hydrogeological_Characterization_of_the_Timgad's_Basin_Aures_Algeria_ne_for_the_Mobilization_of_Water_Resources</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Vol 5</style></volume><pages><style face="normal" font="default" size="100%">pp 143</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">The basin of Timgad is located in the Aures. It is characterized by an average annual precipitation which reaches 800 mm. Hydrology tributary of the relief is the direct result of surface water and snowmelt from the heights of the Massif of Chélia. The origin of groundwater: semi-deep to deep aquifer is mainly from the infiltration of precipitation in the geological layers. This rock forms a water table that is intersected by drilling to a depth of 137-400 m giving a flow rate of 6 l / s. and white fractured sandstone forming a confined aquifer 190 m with a flow rate of 28 l / s. The check of geo-electric results of the basin show that the Miocene and Cretaceous layers have important thickness, they are heterogeneous and may contain large aquifer at different levels. The influence of vertical normal faults makes possible an exchange of waters between theses aquifers. The implementation of dam project in the basin will minimize the silting, regulate the flow rate, and contribute to the irrigation of the plain, it can be used for industry too. The objective of this approach is the mobilization of surface water resources decided by the government for a rational and planned of this vital factor which is water. Caractérisation géologique, hydrologique et hydrogéologique du bassin de Timgad (Aurès, Algérie NE), pour la mobilisation des ressources hydriques Résumé : Le bassin de Timgad est située dans les Aurès. Il est caractérisé par une moyenne annuelle des précipitations de l'ordre de 800 mm. L'hydrologie tributaire du relief est la conséquence directe des eaux de surface et de la fonte des neiges provenant des hauteurs du massif de Chélia. L'alimentation de l'eau souterraine des différentes nappes phréatiques profondes à semi-profonde provient essentiellement de l'infiltration des eaux de pluies dans les couches géologiques. Ce cortège de roche forme une nappe libre qui est recoupée par des forages sur une profondeur de 137-400 m fournissant un débit de 6 l/s. et des grés blancs grossiers fracturés formant une nappe captive à 190 m avec un débit de 28 l/s. L'examen des coupes géoélectriques du bassin montrent que les formations du miocène et du crétacé sont dont l'ensemble, épais, hétérogène et susceptible de contenir de grandes potentialités d'aquifères à des niveaux différents. L'influence de failles normales verticales rend possible une éventuelle alimentation des aquifères entres eux. L'importance de l'implantation d'ouvrage de retenue dans le bassin est de minimiser le phénomène d'envasement, de réguler le débit d'écoulement et de contribuer à l'irrigation de la plaine ainsi que l'alimentation des briqueteries. L'objectif de cette approche, est la mobilisation des ressources en eaux superficielles décidée par l'état en vue d'une utilisation rationnelle et planifiée de ce facteur vital qui et l'eau.</style></abstract><issue><style face="normal" font="default" size="100%">Issue 3</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Mensouri Z</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">L&amp;rsquo;étude des caractéristiques hydrodynamiques et la vulnérabilité de la plaine alluvionnaire de Ksar Belezma (Batna - nord-est Algérien), ISSN 1112-3680,Juin 2016</style></title><secondary-title><style face="normal" font="default" size="100%">Larhyss Journal</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.asjp.cerist.dz/en/article/55339</style></url></web-urls></urls><pages><style face="normal" font="default" size="100%">pp. 237-247</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;span style=&quot;left:82.64px;top:914.206px;18.4px;sans-serif;transform:scaleX(0.900078);&quot;&gt;The cartography of the vulnerability in the pollution of subterranean waters &lt;/span&gt;&lt;span style=&quot;left:82.64px;top:935.406px;18.4px;sans-serif;transform:scaleX(0.925887);&quot;&gt;allows identifying zones with high risk of contamination who takes into account &lt;/span&gt;&lt;span style=&quot;left:82.64px;top:956.406px;18.4px;sans-serif;transform:scaleX(0.887344);&quot;&gt;the major part of th&lt;/span&gt;&lt;span style=&quot;left:237.833px;top:956.406px;18.4px;sans-serif;transform:scaleX(0.891738);&quot;&gt;e hydrogeological factors which allocate and control the &lt;/span&gt; &lt;span style=&quot;left:82.64px;top:61.6094px;16.6px;sans-serif;transform:scaleX(0.983122);&quot;&gt;Mansouri Z.&lt;/span&gt;&lt;span style=&quot;left:174.033px;top:61.6094px;16.6px;sans-serif;transform:scaleX(0.944038);&quot;&gt;&amp;amp; al. / Larhyss Journal, 2&lt;/span&gt;&lt;span style=&quot;left:346.6833333333333px;top:61.609399999999866px;16.6px;sans-serif;&quot;&gt;6&lt;/span&gt;&lt;span style=&quot;left:359.283px;top:61.6094px;16.6px;sans-serif;transform:scaleX(0.920009);&quot;&gt;(2016), &lt;/span&gt;&lt;span style=&quot;left:412.117px;top:61.6094px;16.6px;sans-serif;transform:scaleX(0.888087);&quot;&gt;23&lt;/span&gt;&lt;span style=&quot;left:428.71666666666664px;top:61.609399999999866px;16.6px;sans-serif;&quot;&gt;7&lt;/span&gt;&lt;span style=&quot;left:437.1166666666666px;top:61.609399999999866px;16.6px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:442.517px;top:61.6094px;16.6px;sans-serif;transform:scaleX(0.909747);&quot;&gt;24&lt;/span&gt;&lt;span style=&quot;left:459.3166666666666px;top:61.609399999999866px;16.6px;sans-serif;&quot;&gt;7&lt;/span&gt;&lt;span style=&quot;left:82.64px;top:1052.01px;18.4px;sans-serif;transform:scaleX(0.899023);&quot;&gt;238&lt;/span&gt;&lt;span style=&quot;left:82.64px;top:142.039px;18.4px;sans-serif;transform:scaleX(0.929441);&quot;&gt;flow of subterranean waters: the depth of the water, the refill.&lt;/span&gt;&lt;span style=&quot;left:546.717px;top:142.039px;18.4px;sans-serif;transform:scaleX(0.88392);&quot;&gt;These factors are &lt;/span&gt;&lt;span style=&quot;left:82.64px;top:163.039px;18.4px;sans-serif;transform:scaleX(0.908482);&quot;&gt;represented by weights and quotations which depend respectively on their &lt;/span&gt;&lt;span style=&quot;left:82.64px;top:184.239px;18.4px;sans-serif;transform:scaleX(0.925057);&quot;&gt;relative importance and on local hydrogeolo&lt;/span&gt;&lt;span style=&quot;left:412.317px;top:184.239px;18.4px;sans-serif;transform:scaleX(0.932673);&quot;&gt;gical conditions.&lt;/span&gt;&lt;span style=&quot;left:539.717px;top:184.239px;18.4px;sans-serif;transform:scaleX(0.937613);&quot;&gt;The overall of the &lt;/span&gt;&lt;span style=&quot;left:82.64px;top:205.239px;18.4px;sans-serif;transform:scaleX(0.848433);&quot;&gt;weights and the quotations of the diverse parameters &lt;/span&gt;&lt;span style=&quot;left:486.31666666666666px;top:205.23893333333322px;18.4px;sans-serif;&quot;&gt;a&lt;/span&gt;&lt;span style=&quot;left:494.517px;top:205.239px;18.4px;sans-serif;transform:scaleX(0.853118);&quot;&gt;nd in a numerical value &lt;/span&gt;&lt;span style=&quot;left:82.64px;top:226.239px;18.4px;sans-serif;transform:scaleX(0.918584);&quot;&gt;which is the indication Drastic. The cartography of the indication of &lt;/span&gt;&lt;span style=&quot;left:82.64px;top:247.439px;18.4px;sans-serif;transform:scaleX(0.90494);&quot;&gt;vulnerability bases on the overlapping of 7 indexed cards. &lt;/span&gt;</style></abstract><issue><style face="normal" font="default" size="100%">n°26</style></issue></record></records></xml>