<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Boudoukha Abderrahmane</style></author><author><style face="normal" font="default" size="100%">Djenba Samir</style></author><author><style face="normal" font="default" size="100%">Jean-Sylvain Magagnosc</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation géologique et géotechnique des glissements de la ville de Bougaa. Est Algérien, ISSN 1112-3338</style></title><secondary-title><style face="normal" font="default" size="100%">courrier de savoir </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://pdfs.semanticscholar.org/6e67/266c856297aafe31a4861faea99507a79ea9.pdf</style></url></web-urls></urls><pages><style face="normal" font="default" size="100%">pp.63-67</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;span style=&quot;left:70.7998px;top:601.563px;16.8px;sans-serif;transform:scaleX(0.903164);&quot;&gt;La région de Bougaa est affectée par un glissement déplaçant un volume considérable de matériaux dé&lt;/span&gt;&lt;span style=&quot;left:763.6px;top:601.563px;16.8px;sans-serif;transform:scaleX(0.896679);&quot;&gt;tritiques formés par des &lt;/span&gt;&lt;span style=&quot;left:70.7998px;top:620.763px;16.8px;sans-serif;transform:scaleX(0.899913);&quot;&gt;colluvions, des éboulis à gros blocs et des éboulis de pente argilo&lt;/span&gt;&lt;span style=&quot;left:506.4px;top:620.763px;16.8px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:512px;top:620.763px;16.8px;sans-serif;transform:scaleX(0.933944);&quot;&gt;limoneux &lt;/span&gt;&lt;span style=&quot;left:580px;top:620.763px;16.8px;sans-serif;transform:scaleX(0.890049);&quot;&gt;rougeâtre reposant sur un substratum imperméable &lt;/span&gt;&lt;span style=&quot;left:70.7998px;top:639.963px;16.8px;sans-serif;transform:scaleX(0.893021);&quot;&gt;d’argilite schisteuse. Ce glissement est façonné dans des formations géologiques particulièrement se&lt;/span&gt;&lt;span style=&quot;left:780.4px;top:639.963px;16.8px;sans-serif;transform:scaleX(0.861645);&quot;&gt;nsibles à ce type de &lt;/span&gt;&lt;span style=&quot;left:70.7998px;top:659.163px;16.8px;sans-serif;transform:scaleX(0.922349);&quot;&gt;mouvement à cause de l'hétérogénéité de leurs faciès, de l'imperméabilité de certaines&lt;/span&gt;&lt;span style=&quot;left:663.6px;top:659.163px;16.8px;sans-serif;transform:scaleX(0.925478);&quot;&gt; couches et de l’effet de la tectonique &lt;/span&gt;&lt;span style=&quot;left:70.7998px;top:678.363px;16.8px;sans-serif;transform:scaleX(0.899453);&quot;&gt;cassante et de la karstification. Le but de cette étude est de caractériser ces glissements à l’aide&lt;/span&gt;&lt;span style=&quot;left:769.6px;top:678.363px;16.8px;sans-serif;transform:scaleX(0.903288);&quot;&gt; d’outils géologiques, &lt;/span&gt;&lt;span style=&quot;left:70.7998px;top:697.563px;16.8px;sans-serif;transform:scaleX(0.916535);&quot;&gt;géotechniques et géomorphologiques. Le rôle des eaux d’infiltration est primordial dans le dé&lt;/span&gt;&lt;span style=&quot;left:706.8px;top:697.563px;16.8px;sans-serif;transform:scaleX(0.902806);&quot;&gt;clenchement de ces glissements &lt;/span&gt;&lt;span style=&quot;left:70.7998px;top:716.763px;16.8px;sans-serif;transform:scaleX(0.964588);&quot;&gt;où la lithologi&lt;/span&gt;&lt;span style=&quot;left:169.6px;top:716.763px;16.8px;sans-serif;transform:scaleX(0.953006);&quot;&gt;e, la disposition structurale,&lt;/span&gt;&lt;span style=&quot;left:362.4px;top:716.763px;16.8px;sans-serif;transform:scaleX(0.970182);&quot;&gt;le climat&lt;/span&gt;&lt;span style=&quot;left:422.8px;top:716.763px;16.8px;sans-serif;transform:scaleX(0.932062);&quot;&gt; sont des facteurs favorables. &lt;/span&gt;&lt;span style=&quot;left:628.8px;top:716.763px;16.8px;sans-serif;transform:scaleX(0.943222);&quot;&gt;La présence de pentes &amp;gt; 20 %, de sources &lt;/span&gt;&lt;span style=&quot;left:70.7998px;top:735.963px;16.8px;sans-serif;transform:scaleX(0.906902);&quot;&gt;émergeant du réservoir karstique de Guergour, créant des zones humides qui permettent le déclenche&lt;/span&gt;&lt;span style=&quot;left:761.6px;top:735.963px;16.8px;sans-serif;transform:scaleX(0.885972);&quot;&gt;ment du mouvement du &lt;/span&gt;&lt;span style=&quot;left:70.7998px;top:755.163px;16.8px;sans-serif;transform:scaleX(0.898156);&quot;&gt;sol dans cette région.&lt;/span&gt;</style></abstract><issue><style face="normal" font="default" size="100%">N°18</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation géologique et apport de la géophysique pour la mobilisation des ressources hydriques dans le bassin de ain Djasser (Sud sétifien, Algerie NE)</style></title><secondary-title><style face="normal" font="default" size="100%">Colloque international Eau–Société–Climat’2017 (ESC-2017)  Hammamet, Tunis</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Sellam H</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation hydrochimique de l&amp;rsquo;aquifère alluvial de la plaine de Ain Djasser, Wilaya de Batna. Mémoire de Master, Université Hadj Lakhdar, Batna</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fartas FZ</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Suivi piézométrique et essais de pompage dans la plaine d&amp;rsquo;Ain Djasser, Wilaya de Batna. Mémoire de Master, Université Hadj Lakhdar, Batna - Encadreur principal.</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Mechri Ali</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Suivi piézométrique et hydrochimie dans la plaine de Ain Djasser, Wilaya de Batna. 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Eastern  Algeria </style></title><secondary-title><style face="normal" font="default" size="100%">International Multidisciplinary Academic Conference 11 to 13 May, Paris, France </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Malika</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Risque de pollution des eaux souterraines de la plaine de Zana, Est Algérien</style></title><secondary-title><style face="normal" font="default" size="100%">3émé colloque international Eau-Climat, REGARD CROISES NORD- SUD] Ressources en Eau &amp; Changement Climatique en Région Méditerranéenne 21, 22 &amp; 23 Octobre </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><pub-location><style face="normal" font="default" size="100%">Hammamet (Tunisie)</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Malika</style></author><author><style face="normal" font="default" size="100%">Marmi Ramdane</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">caractérisation géologique, hydrologique et hydrogéologique du bassin de timgad (Aurès, Algérie NE),  pour la mobilisation des ressources hydrique</style></title><secondary-title><style face="normal" font="default" size="100%">3émé colloque international Eau-Climat, REGARD CROISES NORD- SUD] Ressources en Eau &amp; Changement Climatique en Région Méditerranéenne 21, 22 &amp; 23 Octobre Hammamet (Tunisie)</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><pub-location><style face="normal" font="default" size="100%"> Hammamet (Tunisie)</style></pub-location><volume><style face="normal" font="default" size="100%">Vol. 5</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><issue><style face="normal" font="default" size="100%">No. 1</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Zouaoui Siham</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">Bouabid Abd Ennasser</style></author><author><style face="normal" font="default" size="100%">Naidji. A. N</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Conditions hydrogéologiques et hydrochimiques de l&amp;rsquo;oasis de Tolga (Nord-Est Algérien). Ressources en eau &amp;amp; changements climatiques en région méditerranéenne</style></title><secondary-title><style face="normal" font="default" size="100%"> 3ème colloque international Eau-Climat’2014 : REGARDS CROISES NORD-SUD. Hammamet (Tunisie), 21, 22 &amp; 23 Octobre</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><pub-location><style face="normal" font="default" size="100%">Hammamet, Tunisie</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude de la salinité des eaux souterraines dans les zones arides Cas de l&amp;rsquo;aquifère d&amp;rsquo;El-Outaya Région Nord ouest de Biskra  &amp;ndash; Algerie.</style></title><secondary-title><style face="normal" font="default" size="100%">The 5th International conference of Geomatics of Middle East and North Africa. The Euro-Arab Organization for Environment, Water and Desert Researches. Amman Jordan 23-27 mars</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><pub-location><style face="normal" font="default" size="100%">Amman Jordan</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Mansouri Zineb</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Evaluation of the groundwater vulnerability to pollution of the Ksar Belezma aquifer (Algeria Northeast). September 2014</style></title><secondary-title><style face="normal" font="default" size="100%">IAHS Conference, Marrakech, Morocco</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><pub-location><style face="normal" font="default" size="100%">Marrakech, Morocco</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Rihani A</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Hydrogeologic study of Bouzina watershed (Algeria Northeast). September 2014.</style></title><secondary-title><style face="normal" font="default" size="100%">IAHS Conference, Marrakech, Morocco</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><pub-location><style face="normal" font="default" size="100%">Marrakech, Morocco</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Malika</style></author><author><style face="normal" font="default" size="100%">Marmi Ramdane</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation géologique, hydrologique et hydrogéologique du bassin de timgad (Aurès, Algérie NE), pour la mobilisation des ressources hydrique</style></title><secondary-title><style face="normal" font="default" size="100%">3émé colloque international Eau-Climat, REGARD CROISES [NORD- SUD] Ressources en Eau &amp; Changement Climatique en Région Méditerranéenne Hammamet (Tunisie)</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><pub-location><style face="normal" font="default" size="100%"> Hammamet (Tunisie)</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Zouaoui Siham</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">Bouabid AN</style></author><author><style face="normal" font="default" size="100%">Nadji R</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Conditions hydrogéologiques et hydrochimiques de l&amp;rsquo;oasis de Tolga (Nord-Est Algérien). Ressources en eau &amp;amp; changements climatiques en région méditerranéenne. 21, 22 &amp;amp; 23 Octobre</style></title><secondary-title><style face="normal" font="default" size="100%">3ème colloque international Eau-Climat: REGARDS CROISES NORD-SUD. Hammamet (Tunisie)</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><pub-location><style face="normal" font="default" size="100%">Hammamet (Tunisie)</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Analysis of the risk of conflict around the transboundary water resources of the Northern Saharian Aquifer System (NSAS). 19-21 November</style></title><secondary-title><style face="normal" font="default" size="100%">GEOMATE international conference, Brisbane, Australia </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><pub-location><style face="normal" font="default" size="100%">Brisbane, Australia, </style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Les eaux transfrontalières du Système Aquifère du Sahara Septentrional (SASS) : Estimation du risque de conflit. 21-23 Octobre 2014.</style></title><secondary-title><style face="normal" font="default" size="100%">3rd International conference Eau-Climat 2014, Hammamet, Tunisie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><pub-location><style face="normal" font="default" size="100%">Hammamet, Tunisie</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Djenba Samir</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation géologique et géotechnique des glissements de la ville de Bougaa. Est algérien, Mars 2014</style></title><secondary-title><style face="normal" font="default" size="100%">Courrier du Savoir</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.google.dz/url?sa=t&amp;rct=j&amp;q=&amp;esrc=s&amp;source=web&amp;cd=1&amp;cad=rja&amp;uact=8&amp;ved=2ahUKEwi_xq7m78PgAhVGxYUKHd-NBXkQFjAAegQIABAC&amp;url=http%3A%2F%2Frevues.univ-biskra.dz%2Findex.php%2Fcds%2Farticle%2Fview%2F650%2F604&amp;usg=AOvVaw18Us5RIOfsC2lfNU6ndlpe</style></url></web-urls></urls><pages><style face="normal" font="default" size="100%">pp 63-67</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Bougaa region is affected by a shift moving a considerable amount of detritus formed by colluvial deposits, scree to boulders and scree slope reddish clay loam resting on a substratum of impermeable shale shale. This shift is shaped in geological formations particularly sensitive to this type of movement because of the heterogeneity of their facies, the impermeability of certain layers and the effect of tectonics and karstification. The purpose of this study is to characterize these shifts using tools geological, geotechnical and geomorphological features. The role of seepage is essential in triggering these shifts where lithology, structural arrangement, the climate is favorable factors. The presence of slopes&amp;gt; 20%, emerging sources of karst reservoir Guergour, creating wetlands that allow triggering of ground motion in this region.</style></abstract><issue><style face="normal" font="default" size="100%">N°18</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Malika</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Importance des ressources hydriques et leurs impacts sur le développement durable dans le bassin de Timgad (Algérie nord orientale), ISSN 2170-1318,Décembre 2014</style></title><secondary-title><style face="normal" font="default" size="100%">Journal of Arid And Environment (AJAE)</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://revues.univ-ouargla.dz/index.php/volume-4-numero-2-2014/2159-importance-des-ressources-hydriques-et-leurs-impacts-sur-le-developpement-durable-dans-le-bassin-de-timgad-algerie-nord-orientale-djaiz-fouad1-athamena-malika2-athamena-ali3-1-departemen</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">vol. 4</style></volume><pages><style face="normal" font="default" size="100%">pp 78-87</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;i&gt;&lt;span style=&quot;10pt;&quot;&gt;Located in the Aures mountains Foum Toub is characterized by an annual average rainfall of&amp;nbsp; 800mm. The hydrology subordinate to the terrain is the direct consequence of surface waters and of snow melting from the heights of Chelia Mountain. The aim of the implantation of the Foum Toub backwater is to minimize the siltation phenomenon at the upstream of the Koudiate El Mdaour dam, to regularize the Rebaa creek flow which runs from south to north and to contribute to the irrigation of the Foum Toub plain. This study puts the emphasis on the mobilization of surface water resources, a policy of the Ministry of Agriculture and Rural Development with a view to rationalize the use and planning of this vital factor, i.e. water. The site selected for the construction of this structure is characterized by a waterproof marly substratum, favourable for implanting the dike and the basin. The clay-silty-gravelly material furniture localized in the depressions as well as sandstones are used as areas for the construction materials of this structure. Stability is one of the most important parameters to take into account for the choice of the site, so as to avoid any problem linked to the withdrawal-swelling phenomena on the banks of creek. However, the sliding possibility, however weak it is, can be generated on the left bank of the creek within deposit and recent silt. The choice of the site for the implantation of this hydraulic structure remains subject to laboratory tests.&lt;/span&gt;&lt;/i&gt;</style></abstract><issue><style face="normal" font="default" size="100%">n° 2</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude de la salinité des eaux souterraines dans les zones arides Cas de l&amp;rsquo;aquifère d&amp;rsquo;El-Outaya Région Nord ouest de Biskra &amp;ndash; ALGERIE; ISSN 2052-3408,</style></title><secondary-title><style face="normal" font="default" size="100%">International Journal of Environment &amp; Water </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://ijew.ewdr.org/component/k2/item/261-case-of-aquifer-of-el-outaya-north-west-of-biskra-algeria.html</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Vol 3</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Le bassin d’El-Outaya se trouve dans la wilaya de BISKRA, une zone aride au sud algérien à environ 500 Km au sud de la capital Alger. Il constitue une ressource importante pour l'eau d'irrigation en plus d’un barrage à l’amont. La population de la plaine dépasse 11 000 habitants, leur activité principale est l'agriculture.&lt;br&gt;La plaine étudiée correspond à un bassin subsident orienté sensiblement E.NE – W.SW et situé entre deux anticlinaux. Il se trouve au nord de l’anticlinal du Dj.Bou Rhezel (Biskra) et au sud du dôme de Dj. El Melah. Il a fonctionné comme un bassin de sédimentation pendant tout le Néogène. Il est constitué à la base par un miocène laguno-marin, recouvert par du messinien (pontien) gréseux fluviatile, puis par des poudingues pliocènes. Les termes supérieurs, plus particulièrement pliocènes, sont fortement inclinés vers le centre du bassin où ils disparaissent sous une épaisseur considérable du Quaternaire.&lt;br&gt;Le dépouillement des analyses chimiques a aboutit à trois faciès chimiques: Le faciès chloruré sodique, le faciès sulfaté magnésien et le faciès sulfaté sodique.&lt;br&gt;Le suivi des variables chimiques dominant selon les axes des écoulements souterrains permet de suivre l’évolution des faciès dans aquifère ainsi que l’origine de chaque faciès.</style></abstract><issue><style face="normal" font="default" size="100%">Issue 1</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Boudjema Abderrezak</style></author><author><style face="normal" font="default" size="100%">Hacini Messaoud</style></author><author><style face="normal" font="default" size="100%">Guettaia Sabrine</style></author><author><style face="normal" font="default" size="100%">Zahrouna Abderrezak</style></author><author><style face="normal" font="default" size="100%">Baba Sy Lamine</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Modeling Groundwater Flow of the Mio-Pliocene Aquifer in the El-Outaya Plain, Biskra (Algeria) ISSN 2307-4531, (Print &amp;amp; Online).</style></title><secondary-title><style face="normal" font="default" size="100%">International Journal of Sciences: Basic and Applied Research (IJSBAR)</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.google.com/url?sa=t&amp;rct=j&amp;q=&amp;esrc=s&amp;source=web&amp;cd=1&amp;cad=rja&amp;uact=8&amp;ved=2ahUKEwjcn76xvsLgAhWB2qQKHcRnCwAQFjAAegQIBBAC&amp;url=http%3A%2F%2Fgssrr.org%2Findex.php%3Fjournal%3DJournalOfBasicAndApplied%26page%3Darticle%26op%3Ddownload%26path%255B%255D%</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Vol 17</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;
	El Outaya plain is located on the southern flank of the Aures Mountains, as part of the Saharan Atlas. It has an arid climate (less than 200 mm of rainfall / year). The Mio-Pliocene aquifer associated with this plain is an important resource for irrigation and drinking water.
&lt;/p&gt;

&lt;p&gt;
	Achieving the first hydrodynamic model of the Mio-Pliocene ground water in El Outaya plain, with different operating scenarios and using the Visual Mod-flow code, shall contribute to the development of an action plan for a rational management of water resources.&lt;br&gt;In addition, the model was calibrated to steady state conditions and then transient state conditions in order to prepare conductivity and porosity maps that characterize the spatial variability, in relation with the geological heterogeneity of the aquifer. Different operating scenarios indicated that the northern part of the plain is fairly vulnerable to feeding and exploitation conditions.
&lt;/p&gt;
</style></abstract><issue><style face="normal" font="default" size="100%">No 2 </style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderahmane</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude de la salinité des eaux souterraines dans les zones arides Cas de l&amp;rsquo;aquifère d&amp;rsquo;El-Outaya Région Nord ouest de Biskra &amp;ndash; ALGERIE, 2014. ISSN 2052-3408.</style></title><secondary-title><style face="normal" font="default" size="100%"> International Journal of Environment &amp; Water</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><volume><style face="normal" font="default" size="100%">Vol 3</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><issue><style face="normal" font="default" size="100%">Issue 1</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Azizi Yacine</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">Hemila Med Laid</style></author><author><style face="normal" font="default" size="100%">Boumezbeur Abderrahmane</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Karst Sinkholes Stability Assessment in Cheria Area, NE Algeria. Geotechnical and Geological Engineering Review, April 2014</style></title><secondary-title><style face="normal" font="default" size="100%">Springer</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://www.springerprofessional.de/karst-sinkholes-stability-assessment-in-cheria-area-ne-algeria/5004782.html </style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Volume 32</style></volume><pages><style face="normal" font="default" size="100%">pp 363-374</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">This research work deals with the problem of karst sinkhole collapse occurring in the last few years in Cheria area (NE Algeria). This newly revealed phenomenon is of a major constrain in land use planning and urbanization, it has become necessary to locate and assess the stability of these underground features before any planning operation. Several exploration methods for the localization of underground cavities have been considered. Geological survey, discontinuity analysis, resistivity survey [ground penetrating radar has not been used as most of the Mio-Plio-Quaternary filling deposit covering Eocene limestone contains clay layers which limits the applicability of the method (Roth et al. in Eng Geol 65:225–232, &lt;cite&gt;&lt;a href=&quot;https://www.springerprofessional.de/karst-sinkholes-stability-assessment-in-cheria-area-ne-algeria/5468096?redirect=1#CR25&quot;&gt;2002&lt;/a&gt;&lt;/cite&gt;)] and borehole drilling were undertaken in order to locate underground cavities and assess their depth, geometry, dimensions, etc. Laboratory testing and field work were also undertaken in order to determine both intact rock and rock mass properties. All the rock mechanics testing and measurement were undertaken according to the ISRM recommendations. It has been found that under imposed loading, the stability of the karst cavities depends on the geo-mechanical parameters (RMR, Rock Mass Rating; GSI, Geological Strength Index; E, Young modulus) of the host rock as well as the depth and dimensions of the gallery. It increases with RMR, GSI, E and depth and decreases as the cavity becomes wider. Furthermore, the calculation results show that a ratio (roof thickness to gallery width) of 0.3 and more indicate, a stable conditions. The results obtained in this work allow identifying and assessing the stability of underground karst cavities. The methodology followed in this paper can be taken as a road map in the establishment of a hazard map related to the studied phenomenon. This map will be a useful tool for the future urban extension planning in Cheria area.</style></abstract><issue><style face="normal" font="default" size="100%">Issue 2</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Drias Tarek</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Cartography of the vulnerability to pollution, Application to alluvial aquifer of Tabessa-Morsott - Eastern Algeria.</style></title><secondary-title><style face="normal" font="default" size="100%">Review of strategic and international studies</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><volume><style face="normal" font="default" size="100%">Volume VI</style></volume><pages><style face="normal" font="default" size="100%"> pp 96-107.</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><issue><style face="normal" font="default" size="100%">Number 1</style></issue></record></records></xml>