<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Belgaid, Nassima</style></author><author><style face="normal" font="default" size="100%">Menani, Mohamed-Redha</style></author><author><style face="normal" font="default" size="100%">Bouhidel, Kamel-Eddine</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Elaboration of Bentonite layered double hydroxide composite (LDH-bentonite) to enhance adsorption of sulfide in water</style></title><secondary-title><style face="normal" font="default" size="100%">Séminaire International sur l′Hydrogéologie et l′Environnement SIHE 2019 Ouargla</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://dspace.univ-ouargla.dz/jspui/bitstream/123456789/24561/1/Belgaid%20Nassima.pdf</style></url></web-urls></urls><pub-location><style face="normal" font="default" size="100%">Ouargla, Algeria</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	Low cost bentonite clay was chemically modified using magnesium chloride in order to enhance its sulfide removal capacity. The incorporation of Co and Al into bentonite (MB). Batch adsorption experiments were conducted to study and optimize various operational parameters such as adsorbent dose, contact time, pH, and initial sulfide concentration. It was observed that the MB works effectively over wide range of pH and showed a maximum sulfide removal capacity of 2.26mgg−1 at an initial fluoride concentration of 5mg L−1, which is much better than the unmodified bentonite. Desorption study of MB suggest that almost all the loaded fluoride was desorbed (~97%) using 1M NaOH solution however maximum sulfide removal decreases from 95.47 to 73 (%) after regeneration. From the experimental results, it may be inferred that chemical modification enhances the sulfide removal efficiency of bentonite and it works as an effective
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Boudjema,  Abderrezak</style></author><author><style face="normal" font="default" size="100%">Guettaia, Sabrine</style></author><author><style face="normal" font="default" size="100%">Brinis, Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">STATISTICAL AND HYDROCHEMICAL CLASSIFICATION OF UNDERGROUND WATERS IN A MULTI-LAYER AQUIFER SYSTEM IN AN ARID ZONE :APPLICATION TO CHOTT EL GHARBI BASIN (EXTREME WEST OF ALGERIA)</style></title><secondary-title><style face="normal" font="default" size="100%">Journal of Fundamental and Applied Sciences</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.researchgate.net/profile/Nafaa-Brinis-2/publication/344543059_Statistical_and_hydrochemical_classification_of_underground_waters_in_a_multi-layer_aquifer_system_in_an_arid_zone_application_to_chott_el_gharbi_basin_extreme_west_of_algeria/links</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p style=&quot;text-align: justify;&quot;&gt;
	The studied area, so called Chott El Gharbi shelters a multilayer aquifer system. The hydro-chemical tool shows that the results of the groundwater analyzes of the aquifer system of the Chott El Gharbi region revealed that they are sulphated-calcium and magnesian. Water infiltrated at the Bajo-Bathonian and Mio-Plio-Quaternary carbonate formations is enriched with HCO3- and SiO2 along its underground route. Also, the presence of a Triassic evaporitic formation or the Cenomano- Turonian argilo-gypsum formation enriches these waters with SO4 2- , Cl- , K+ , Mg2+, Na+ and Ca2+ . Thermodynamics has shown that these waters are under saturated evaporitic elements, which gives them a greater power of dissolution than that of carbonates which are in equilibrium or sometimes even supersaturated and tend to precipitate.
&lt;/p&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Kehiha Haifa</style></author><author><style face="normal" font="default" size="100%">Khetta Makhloufa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à l&amp;#39;étude géotechnique du viaduc de la penetrante Bir chouhada-Batnapénétrante Bir-Echouhada - Batna</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Zekiri Ahmed</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à l&amp;#39;étude géotechnique de la pénétrante  autoritière. Trançon Eleulma Djemila</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Basli Aleddine</style></author><author><style face="normal" font="default" size="100%">Aksa Nasreddine</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Cartographie de vulnérabilité de l&amp;#39;aquifère superficiel de Biska</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Mekhloufi Nadjet</style></author><author><style face="normal" font="default" size="100%">Bastal Dhaouia</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Suivi piézométrique et hydrochique de l&amp;#39;aquifère alluvionnaire de Ain Djasser</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Aichaoui Billal</style></author><author><style face="normal" font="default" size="100%">Abid Belgacem</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Le Turonien de Dj Boukezzez (ChaabetOuledChelih) : Caractérisation lithobiostratigraphique et interprétation paléoenvironnementale.</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Bessariani tahar</style></author><author><style face="normal" font="default" size="100%">Guettaoui Imed</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Coupe de Dj BouArif : Etude lithostratigraphique, sédimentologique et réflexions paléoenvironnementales à partir de l&amp;rsquo;étude de la faune et de la microfaune (Aurès, Batna).</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Slami Rafika</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Mise en Evidence de l&amp;#39;évènement anoxique océanique 2 (EAO-2) dans la région de Batna (NE, Algérie)</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://biblio.univ-annaba.dz/wp-content/uploads/2019/11/These-Slami-Rafika.pdf</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;div class=&quot;textLayer&quot; style=&quot;width:992px;height:1403px;&quot;&gt;
	&lt;span style=&quot;left:837.167px;top:63.6px;18.4px;sans-serif;transform:scaleX(0.949474);&quot;&gt;Résumé&lt;/span&gt;&lt;span style=&quot;left:141.84px;top:119.013px;20px;sans-serif;transform:scaleX(0.967493);&quot;&gt;Résumé&lt;/span&gt;&lt;span style=&quot;left:214.433px;top:119.013px;20px;sans-serif;&quot;&gt;:&lt;/span&gt;&lt;span style=&quot;left:177.433px;top:165.011px;20px;sans-serif;transform:scaleX(0.907355);&quot;&gt;La présente étude s’intéresse aux dépôts cénomano&lt;/span&gt;&lt;span style=&quot;left:591.717px;top:165.013px;20px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:598.317px;top:165.013px;20px;sans-serif;transform:scaleX(0.912758);&quot;&gt;turoniens, observables dans la région &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:188.013px;20px;sans-serif;transform:scaleX(0.916738);&quot;&gt;de Batna&lt;/span&gt;&lt;span style=&quot;left:213.033px;top:188.013px;20px;sans-serif;&quot;&gt;,&lt;/span&gt;&lt;span style=&quot;left:223.833px;top:188.011px;20px;sans-serif;transform:scaleX(0.934847);&quot;&gt;afin de définir la mise en évidence de l’évènement anoxique océanique 2 (EAO&lt;/span&gt;&lt;span style=&quot;left:869.367px;top:188.013px;20px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:875.967px;top:188.013px;20px;sans-serif;transform:scaleX(1.01227);&quot;&gt;2). &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:211.013px;20px;sans-serif;transform:scaleX(0.900573);&quot;&gt;Cette &lt;/span&gt;&lt;span style=&quot;left:192.433px;top:211.013px;20px;sans-serif;transform:scaleX(0.922909);&quot;&gt;région couvre deux domaines &lt;/span&gt;&lt;span style=&quot;left:458.483px;top:211.013px;20px;sans-serif;transform:scaleX(0.912445);&quot;&gt;paléogéographiques et structuraux : le préatlasique&lt;/span&gt;&lt;span style=&quot;left:141.84px;top:234.013px;20px;sans-serif;transform:scaleX(0.931316);&quot;&gt;(Monts de Bellezma&lt;/span&gt;&lt;span style=&quot;left:314.833px;top:234.013px;20px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:321.833px;top:234.013px;20px;sans-serif;transform:scaleX(0.911454);&quot;&gt;Batna) au N&lt;/span&gt;&lt;span style=&quot;left:426.683px;top:234.013px;20px;sans-serif;&quot;&gt;O&lt;/span&gt;&lt;span style=&quot;left:449.083px;top:234.013px;20px;sans-serif;transform:scaleX(0.910447);&quot;&gt;et l'atlasique &lt;/span&gt;&lt;span style=&quot;left:563.117px;top:234.013px;20px;sans-serif;transform:scaleX(0.907985);&quot;&gt;(Monts de l'Aurès) au SE. &lt;/span&gt;&lt;span style=&quot;left:789.167px;top:234.013px;20px;sans-serif;transform:scaleX(0.892962);&quot;&gt;Pour le faire,&lt;/span&gt;&lt;span style=&quot;left:141.84px;top:257.013px;20px;sans-serif;transform:scaleX(0.902415);&quot;&gt;une analyse sédimentologique, biostratigraphique et géochimique est réalisée sur deux coupes &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:280.013px;20px;sans-serif;transform:scaleX(0.945864);&quot;&gt;Thénièt El Manchar et Firmet Riche «&lt;/span&gt;&lt;span style=&quot;left:482.283px;top:280.013px;20px;sans-serif;transform:scaleX(1.00822);&quot;&gt;Dj Bou Arif&lt;/span&gt;&lt;span style=&quot;left:594.917px;top:280.013px;20px;sans-serif;transform:scaleX(0.918216);&quot;&gt;». Basées sur les ammonites et les &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:303.013px;20px;sans-serif;transform:scaleX(0.875237);&quot;&gt;foraminifères planctoniques, deux formations ont été définies&lt;/span&gt;&lt;span style=&quot;left:649.917px;top:303.013px;20px;sans-serif;transform:scaleX(0.893969);&quot;&gt;: (1) la Formati&lt;/span&gt;&lt;span style=&quot;left:777.567px;top:303.013px;20px;sans-serif;&quot;&gt;o&lt;/span&gt;&lt;span style=&quot;left:787.567px;top:303.013px;20px;sans-serif;transform:scaleX(0.855427);&quot;&gt;n des Marnes &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:326.013px;20px;sans-serif;transform:scaleX(0.929617);&quot;&gt;de Smail, subdivisée en quatre unités litho&lt;/span&gt;&lt;span style=&quot;left:517.883px;top:326.013px;20px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:524.483px;top:326.013px;20px;sans-serif;transform:scaleX(0.973285);&quot;&gt;stratigraphiques (IA, IB, IC, ID), datée du &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:349.011px;20px;sans-serif;transform:scaleX(0.929831);&quot;&gt;Cénomanien et (2) la base de la Formation des Dolomies de l’Oued Skhoun (unité, IIA) datée &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:372.011px;20px;sans-serif;transform:scaleX(0.948156);&quot;&gt;du Turonien inférieur. L’analyse qualitative et quantitative d&lt;/span&gt;&lt;span style=&quot;left:642.717px;top:372.013px;20px;sans-serif;&quot;&gt;e&lt;/span&gt;&lt;span style=&quot;left:651.517px;top:372.013px;20px;sans-serif;transform:scaleX(0.927028);&quot;&gt;s foraminifères (planctoniques &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:395.061px;20px;sans-serif;transform:scaleX(0.888316);&quot;&gt;et/ou benthiques), des ostracodes, l’étude du microfaciès et des marqueurs géochimiques, &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:418.061px;20px;sans-serif;transform:scaleX(0.974375);&quot;&gt;permet de reconstituer l’évolution du paléo&lt;/span&gt;&lt;span style=&quot;left:541.717px;top:418.063px;20px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:548.317px;top:418.063px;20px;sans-serif;transform:scaleX(0.91466);&quot;&gt;environnement et les variations paléo&lt;/span&gt;&lt;span style=&quot;left:890.967px;top:418.063px;20px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:141.84px;top:441.061px;20px;sans-serif;transform:scaleX(0.914609);&quot;&gt;bathymétriques au cours de l’intervalle stratigraphiq&lt;/span&gt;&lt;span style=&quot;left:562.317px;top:441.063px;20px;sans-serif;&quot;&gt;u&lt;/span&gt;&lt;span style=&quot;left:572.317px;top:441.063px;20px;sans-serif;transform:scaleX(0.951664);&quot;&gt;e concerné. Ainsi, les unités IA&lt;/span&gt;&lt;span style=&quot;left:824.767px;top:441.063px;20px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:831.567px;top:441.063px;20px;sans-serif;transform:scaleX(1.16068);&quot;&gt;IB&lt;/span&gt;&lt;span style=&quot;left:851.367px;top:441.063px;20px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:858.167px;top:441.063px;20px;sans-serif;transform:scaleX(0.973938);&quot;&gt;IC et &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:464.061px;20px;sans-serif;transform:scaleX(0.9502);&quot;&gt;la partie inférieure de l’unité ID (Cénomanien) sont dominées par des associations de fora&lt;/span&gt;&lt;span style=&quot;left:891.167px;top:464.063px;20px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:141.84px;top:487.061px;20px;sans-serif;transform:scaleX(0.907777);&quot;&gt;minifères benthiques agglutinés et des carapaces entières d’ostracodes, témoignant d’un &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:510.063px;20px;sans-serif;transform:scaleX(0.908447);&quot;&gt;milieu de plate&lt;/span&gt;&lt;span style=&quot;left:260.633px;top:510.063px;20px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:267.233px;top:510.061px;20px;sans-serif;transform:scaleX(0.916132);&quot;&gt;forme et d’un faib&lt;/span&gt;&lt;span style=&quot;left:412.483px;top:510.063px;20px;sans-serif;&quot;&gt;l&lt;/span&gt;&lt;span style=&quot;left:418.083px;top:510.061px;20px;sans-serif;transform:scaleX(0.928217);&quot;&gt;e hydrodynamisme. Les calcaires supérieurs de l’unité IC et &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:533.061px;20px;sans-serif;transform:scaleX(0.929366);&quot;&gt;inférieurs de l’unité ID sont marqués par la présence de rudistes traduisant une reduction&lt;/span&gt;&lt;span style=&quot;left:877.767px;top:533.063px;20px;sans-serif;transform:scaleX(0.880933);&quot;&gt;du &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:556.061px;20px;sans-serif;transform:scaleX(0.921854);&quot;&gt;milieu de sédimentation et une augmentation de l’hydrodynamisme. Dans ces dépôts, les &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:579.063px;20px;sans-serif;transform:scaleX(0.894683);&quot;&gt;associations m&lt;/span&gt;&lt;span style=&quot;left:262.233px;top:579.063px;20px;sans-serif;&quot;&gt;o&lt;/span&gt;&lt;span style=&quot;left:272.233px;top:579.063px;20px;sans-serif;transform:scaleX(0.883442);&quot;&gt;ntrent une diversité spécifique faible à moy&lt;/span&gt;&lt;span style=&quot;left:637.317px;top:579.063px;20px;sans-serif;transform:scaleX(0.851944);&quot;&gt;enne et une abondance plus ou &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:602.063px;20px;sans-serif;transform:scaleX(0.912045);&quot;&gt;moins élevée de foraminifères benthiques, témoignant de conditions trophiques et &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:625.061px;20px;sans-serif;transform:scaleX(0.917098);&quot;&gt;d’oxygénation considérées comme normales. Les termes sommitaux de l’unité ID (sommet du &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:648.063px;20px;sans-serif;transform:scaleX(0.917778);&quot;&gt;Cénomanien)&lt;/span&gt;&lt;span style=&quot;left:255.233px;top:648.061px;20px;sans-serif;transform:scaleX(0.930604);&quot;&gt;et l’unité IIA (base du Turonien) marquent, quant à eux, une évolution vers des &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:671.097px;20px;sans-serif;transform:scaleX(0.893131);&quot;&gt;conditions plus profondes, comme le montre la succession stan&lt;/span&gt;&lt;span style=&quot;left:679.917px;top:671.097px;20px;sans-serif;transform:scaleX(0.878418);&quot;&gt;dard des événements déjà &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:694.094px;20px;sans-serif;transform:scaleX(0.917714);&quot;&gt;reconnus en Afrique du nord, à savoir : l’abondance de foraminifères planctoniques, la &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:717.097px;20px;sans-serif;&quot;&gt;p&lt;/span&gt;&lt;span style=&quot;left:151.84px;top:717.097px;20px;sans-serif;&quot;&gt;r&lt;/span&gt;&lt;span style=&quot;left:158.44px;top:717.094px;20px;sans-serif;transform:scaleX(0.90375);&quot;&gt;ésence de ‘filaments’ et une réduction drastique de la faune d’ostracodes. &lt;/span&gt;&lt;span style=&quot;left:177.433px;top:763.094px;20px;sans-serif;transform:scaleX(0.936151);&quot;&gt;D’une manière générale, la sédimentation des deux formations dans les deux domaines &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:786.094px;20px;sans-serif;transform:scaleX(0.897595);&quot;&gt;représente une séquence qui évolue d’un environnement de plate&lt;/span&gt;&lt;span style=&quot;left:662.917px;top:786.097px;20px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:669.517px;top:786.097px;20px;sans-serif;transform:scaleX(0.918249);&quot;&gt;forme externe distale à celui &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:809.097px;20px;sans-serif;&quot;&gt;d&lt;/span&gt;&lt;span style=&quot;left:151.84px;top:809.094px;20px;sans-serif;&quot;&gt;’&lt;/span&gt;&lt;span style=&quot;left:158.44px;top:809.097px;20px;sans-serif;transform:scaleX(0.876958);&quot;&gt;une plate&lt;/span&gt;&lt;span style=&quot;left:235.633px;top:809.097px;20px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:242.233px;top:809.094px;20px;sans-serif;transform:scaleX(0.902523);&quot;&gt;forme moyenne, avec une phase régressive. Cette séquence s’achève avec le &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:832.094px;20px;sans-serif;transform:scaleX(0.898618);&quot;&gt;retour aux conditions profondes concomitantes d’une hausse eustatique et dépôt de sédiments &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:855.094px;20px;sans-serif;transform:scaleX(0.905802);&quot;&gt;pélagiques caractérisant un intervalle transgressif (IT) et s’inscrit dans le c&lt;/span&gt;&lt;span style=&quot;left:774.967px;top:855.097px;20px;sans-serif;&quot;&gt;y&lt;/span&gt;&lt;span style=&quot;left:784.567px;top:855.097px;20px;sans-serif;transform:scaleX(0.886885);&quot;&gt;cle eustatique &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:878.094px;20px;sans-serif;transform:scaleX(0.909097);&quot;&gt;majeur téthysien de troisième ordre. L’évolution séquentielle et paléogéographique des &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:900.897px;20px;sans-serif;transform:scaleX(0.860378);&quot;&gt;dépôts cénomaniens et turoniens inférieurs de la région de Batna dépendent intimement du &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:923.947px;20px;sans-serif;transform:scaleX(0.90297);&quot;&gt;contexte structural de la région.&lt;/span&gt;&lt;span style=&quot;left:167.033px;top:969.947px;20px;sans-serif;transform:scaleX(0.909695);&quot;&gt;En outre, les courbes isotop&lt;/span&gt;&lt;span style=&quot;left:389.083px;top:969.947px;20px;sans-serif;&quot;&gt;i&lt;/span&gt;&lt;span style=&quot;left:394.683px;top:969.947px;20px;sans-serif;transform:scaleX(0.897402);&quot;&gt;ques du, carbone (&lt;/span&gt;&lt;span style=&quot;left:541.517px;top:969.944px;20px;sans-serif;&quot;&gt;Δ&lt;/span&gt;&lt;span style=&quot;left:554.317px;top:968.227px;13.4px;sans-serif;transform:scaleX(0.971429);&quot;&gt;13&lt;/span&gt;&lt;span style=&quot;left:567.717px;top:969.944px;20px;sans-serif;transform:scaleX(0.94237);&quot;&gt;C) et de l’oxygène (&lt;/span&gt;&lt;span style=&quot;left:727.917px;top:969.944px;20px;sans-serif;&quot;&gt;Δ&lt;/span&gt;&lt;span style=&quot;left:740.717px;top:968.227px;13.4px;sans-serif;transform:scaleX(0.971429);&quot;&gt;18&lt;/span&gt;&lt;span style=&quot;left:754.367px;top:969.947px;20px;sans-serif;transform:scaleX(0.898125);&quot;&gt;O) des carbonates &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:992.947px;20px;sans-serif;transform:scaleX(0.922887);&quot;&gt;mettent en évidence des anomalies isotopiques relatives aux modifications paléo&lt;/span&gt;&lt;span style=&quot;left:891.167px;top:992.947px;20px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:141.84px;top:1015.95px;20px;sans-serif;transform:scaleX(0.917037);&quot;&gt;environnementales. Les données du &lt;/span&gt;&lt;span style=&quot;left:457.883px;top:1015.94px;20px;sans-serif;&quot;&gt;Δ&lt;/span&gt;&lt;span style=&quot;left:470.683px;top:1014.23px;13.4px;sans-serif;transform:scaleX(0.971429);&quot;&gt;13&lt;/span&gt;&lt;span style=&quot;left:484.283px;top:1015.95px;20px;sans-serif;transform:scaleX(0.940311);&quot;&gt;C et celles du COT indiquent une productivité &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:1038.95px;20px;sans-serif;transform:scaleX(0.87944);&quot;&gt;primaire faible. Les données d&lt;/span&gt;&lt;span style=&quot;left:393.083px;top:1038.95px;20px;sans-serif;&quot;&gt;u&lt;/span&gt;&lt;span style=&quot;left:410.283px;top:1038.94px;20px;sans-serif;&quot;&gt;Δ&lt;/span&gt;&lt;span style=&quot;left:423.083px;top:1037.23px;13.4px;sans-serif;transform:scaleX(0.971429);&quot;&gt;18&lt;/span&gt;&lt;span style=&quot;left:436.683px;top:1038.95px;20px;sans-serif;transform:scaleX(0.851647);&quot;&gt;O, quant à elles, indiquent une augmentation des paléo&lt;/span&gt;&lt;span style=&quot;left:891.167px;top:1038.95px;20px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:141.84px;top:1061.94px;20px;sans-serif;transform:scaleX(0.912284);&quot;&gt;températures, cause principale du déclenchement de l’EAO 2. Ces interprétations paléo&lt;/span&gt;&lt;span style=&quot;left:890.967px;top:1061.95px;20px;sans-serif;&quot;&gt;-&lt;/span&gt;&lt;span style=&quot;left:141.84px;top:1084.94px;20px;sans-serif;transform:scaleX(0.906523);&quot;&gt;environnementales s’accordent avec les données con&lt;/span&gt;&lt;span style=&quot;left:590.317px;top:1084.95px;20px;sans-serif;transform:scaleX(0.886902);&quot;&gt;nues du contexte paléogéographique &lt;/span&gt;&lt;span style=&quot;left:141.84px;top:1107.95px;20px;sans-serif;transform:scaleX(0.879169);&quot;&gt;régional et mettent en e&lt;/span&gt;&lt;span style=&quot;left:329.483px;top:1107.95px;20px;sans-serif;&quot;&gt;x&lt;/span&gt;&lt;span style=&quot;left:339.683px;top:1107.95px;20px;sans-serif;transform:scaleX(0.911768);&quot;&gt;ergue les spécificités téthysiennes. &lt;/span&gt;
&lt;/div&gt;
</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Bouhadeb Chamsseddine</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Evaluation du transport solide au niveau du bassin versant d&amp;#39;Oued Bounamoussa et ses incidences sur l&amp;#39;envasement du barrage de Chefia</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Djenba Samir</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caracterisation hydrochimiques des eaux du continental intercalaire et complexe terminal et les problèmes d&amp;rsquo;irrigationà la vallée d&amp;rsquo;oued Righ  </style></title><secondary-title><style face="normal" font="default" size="100%">Second International Symposium Water Resources and Environmental Impact Assessment  in North Africa (WREIANA 2019) March 25 -27 , 2019-Sousse, Tunisia</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Dekakra Mouna</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">Abdelhamid Khedidja</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Impact de la pollution agricole sur la qualité des eaux de l&amp;#39;aquifère de Teleghma</style></title><secondary-title><style face="normal" font="default" size="100%">Second International Symposium Water Resources and Environmental Impact Assessment  in North Africa (WREIANA 2019) March 25 -27 , 2019-Sousse, Tunisia</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">B. Saadali</style></author><author><style face="normal" font="default" size="100%">H. Zerouk</style></author><author><style face="normal" font="default" size="100%">Drias Tarek</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Physicochemical and organic quality assessment of Mexa and Bougous waters and its suitability for agricultural use</style></title><secondary-title><style face="normal" font="default" size="100%">Second International Symposium Water Resources and Environmental Impact Assessment  in North Africa (WREIANA 2019) March 25 -27 , 2019-Sousse, Tunisia</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Drias Tarek</style></author><author><style face="normal" font="default" size="100%">Abdelhamid Khedidja</style></author><author><style face="normal" font="default" size="100%">Belloula Moufida</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Assessment of the capacitive function of Shallow aquifer using probabilistic and deterministic approaches (geostatistics - 3D model)</style></title><secondary-title><style face="normal" font="default" size="100%">Second International Symposium Water Resources and Environmental Impact Assessment  in North Africa (WREIANA 2019) March 25 -27 , 2019-Sousse, Tunisia</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.wreiana2019.com</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Boumaiza Lamine</style></author><author><style face="normal" font="default" size="100%">Chabour Nabil</style></author><author><style face="normal" font="default" size="100%">Drias Tarek</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Reviewing the potential anthropogenic sources of groundwater contamination - Case study of the expanding urban area of Taleza in Algeria.</style></title><secondary-title><style face="normal" font="default" size="100%">the 72nd Canadian Geotechnical Conference, St-John’s, (September 29 to October 02, 2019)Newfoundland, Canada</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.iaeg.info › Congresses</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Boumaiza Lamine</style></author><author><style face="normal" font="default" size="100%">Chabour Nabil</style></author><author><style face="normal" font="default" size="100%">Drias Tarek</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">there still a chance to save the groundwater in Taleza aquifer ?</style></title><secondary-title><style face="normal" font="default" size="100%">AGC-AMC-AIH - GAC-MAC-IAH Conference | Quebec City</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://gacmac-quebec2019.ca</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Abdelhamid Khedidja</style></author><author><style face="normal" font="default" size="100%">Boudoukha Abderrahmane</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Quality assessment of shallow groundwater for irrigation purposes in Tadjenanet &amp;ndash; Chelghoum Laid area (Eastern Algeria) ISSN / e-ISSN 1571-5124 / 1814-2060</style></title><secondary-title><style face="normal" font="default" size="100%">International Journal of River Basin Management</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.researchgate.net/publication/333708795_Quality_Assessment_of_Shallow_Groundwater_for_irrigation_purposes_in_Tadjenanet_-_Chelghoum_Laid_area_Eastern_Algeria</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">The groundwater quality of Tadjenanet- Chelghoum Laid Semi-arid region was assessed for irrigation suitability; where the intensity of salinization process depends on soil characteristics, water quality, irrigation practices and in particular the inefficiency of the drainage system. The drought of the last decade has created an agricultural deficit due to high evapotranspiration, influencing the water salinity. To achieve this assessment, thirty groundwater samples were collected at identical locations from deeper wells. The physicochemical parameters such as, pH, electrical conductivity (EC), total hardness (TH), Ca²⁺, Mg²⁺, Na⁺, K⁺, HCO3⁻, SO4²⁻, Cl⁻ and NO3⁻ have been studied. Obtained results were measured and interpreted with different irrigation indexes like EC, sodium percentage (SP), sodium adsorption ratio (SAR), residual sodium carbonate (RSC), permeability index (PI) and Kelly’s ratio (KR). These parameters combined allowed to conclude that the quality of groundwater was roughly suitable for irrigation.</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Benmansour Sana</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Les carbonates marins campano-maastrichtiens dans les gorges d&amp;#39;El Kantara, Aurès occidental, Algérie : control sur la biodiversité, les types de microfaciès et l&amp;#39;architecture des dépôts</style></title><secondary-title><style face="normal" font="default" size="100%">Premier Colloque sur la géologie des Bassins Sédimentaires Maghrébins FSTGAT-USTHB 01 au 03-10-2019</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Benmansour Sana</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à l&amp;#39;étude du Crétacé supérieur- Tertiaire : cas de Dj. Arhane, bassin decGhassira (Aurès central, NE Algérien)</style></title><secondary-title><style face="normal" font="default" size="100%">Premier Colloque sur la géologie des Bassins Sédimentaires Maghrébins FSTGAT-USTHB 01 au 03-10-2019</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Benmansour Sana</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Etude lithostratigraphique et analyse séquentielle de la région de Maafa- synclinal de Béni Fedhala (Aurès, Atlas Saharien Oriental)</style></title><secondary-title><style face="normal" font="default" size="100%">Premier Colloque sur la géologie des Bassins Sédimentaires Maghrébins FSTGAT-USTHB 01 au 03-10-2019</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">Lamouri Bachir</style></author><author><style face="normal" font="default" size="100%">A. Bousahaba</style></author><author><style face="normal" font="default" size="100%">Belalite Halima</style></author><author><style face="normal" font="default" size="100%">Touansa Rachid</style></author><author><style face="normal" font="default" size="100%">Khanfer Soumia</style></author><author><style face="normal" font="default" size="100%">Marred Manal</style></author><author><style face="normal" font="default" size="100%">Chairat Imen</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation géologique et apport de la géophysique pour la mobilisation des ressources hydriques dans le  bassin de Gadaine (Ain Yagout, Algérie NE)</style></title><secondary-title><style face="normal" font="default" size="100%">1st  National Seminar on GeoSciences and Environment SGSE 19 October 23-24, Tamanrasset, </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Marred Manal</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Boushaba Abdellah</style></author><author><style face="normal" font="default" size="100%">Lamouri Bachir</style></author><author><style face="normal" font="default" size="100%">Kherchouche Adila</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Essai de caracterisation lithostratigraphiques et paléoenvironnementdes formations Eocène du bassin de Ghassira : Coupe  du Kef El-Arous (Aurès Central, NE Algérien)</style></title><secondary-title><style face="normal" font="default" size="100%">1st  National Seminar on GeoSciences and Environment SGSE 19 October 23-24, Tamanrasset</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Khanfer Soumia</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à l&amp;rsquo;étude du basin Néogène Batna-ain Touta, limite aurès-Monts de Belezma</style></title><secondary-title><style face="normal" font="default" size="100%">1st  National Seminar on GeoSciences and Environment SGSE 19 October 23-24, Tamanrasset</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Chairat Imen</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Boughdiri Mabrouk</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Reconsideration of the Cenomanian-Turonian stratigraphics units in the Tebessa region (Algero-TunisienConfines): Petroleum implications</style></title><secondary-title><style face="normal" font="default" size="100%">1st  National Seminar on GeoSciences and Environment SGSE 19 October 23-24, Tamanrasset</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">MENNANI Mohamed Redha</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Hydrochemical Characteristics under current condition exploitation usingstatistics methods : case of the Zana- Roknia plain, North east of Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">1st  National Seminar on GeoSciences and Environment SGSE 19 October 23-24, Tamanrasset</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Lamouri Bachir</style></author><author><style face="normal" font="default" size="100%">Boughdiri Mabrouk</style></author><author><style face="normal" font="default" size="100%">Touansa Rachid</style></author><author><style face="normal" font="default" size="100%">Boushaba Abdellah</style></author><author><style face="normal" font="default" size="100%">Mrred Manel</style></author><author><style face="normal" font="default" size="100%">Khaner Soumia</style></author><author><style face="normal" font="default" size="100%">Chairat Imen</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Les terrasses fluviatiles quaternaires de Oued El Gourzi et oued El Hay (Batna, NE Algérie) : Sédimentologie Caractéristiques de l&amp;rsquo;Environnement</style></title><secondary-title><style face="normal" font="default" size="100%">1st  National Seminar on GeoSciences and Environment SGSE 19 October 23-24, Tamanrasset</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Defaflia Nabil</style></author><author><style face="normal" font="default" size="100%">A. Benkhedda</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">A. Cerif</style></author><author><style face="normal" font="default" size="100%">M. Djerab-Ruault</style></author><author><style face="normal" font="default" size="100%">L. Gouadia</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Les dépots Miocène de la région de Tébessa (Nord-est Algérien) : Analyses sédimentologiques, Micropaléontologiques et Paléoenvironnement </style></title><secondary-title><style face="normal" font="default" size="100%">Premier Colloque sur la géologie des Bassins Sédimentaires Maghrébins FSTGAT-USTHB 01 au 03-10-2019</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Nadji Hocine</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">M. Hmmimed</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation géologique et apport de la géophysique pour la mobilisation des ressources hydriques dans le bassin d&amp;rsquo;El Mather.</style></title><secondary-title><style face="normal" font="default" size="100%">Premier Colloque sur la géologie des Bassins Sédimentaires Maghrébins FSTGAT-USTHB 01 au 03-10-2019</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">R. Touansa</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Boughdiri Mabrouk</style></author><author><style face="normal" font="default" size="100%">I. Cherif</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">La lithostratigraphie de l&amp;rsquo;Ammonitico Rosso de Djebel Kasserou (Monts de Batna)</style></title><secondary-title><style face="normal" font="default" size="100%">Premier Colloque sur la géologie des Bassins Sédimentaires Maghrébins FSTGAT-USTHB 01 au 03-10-2019</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">M. Marred</style></author><author><style face="normal" font="default" size="100%">A. Kherchouche</style></author><author><style face="normal" font="default" size="100%">Benmansour Sana</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Contribution à l&amp;rsquo;étude du crétacé supérieur-Tertiaire: Cas de Djebel Arhane, bassin de Ghassira (Aurès Central, NE Algérien.</style></title><secondary-title><style face="normal" font="default" size="100%">Premier Colloque sur la géologie des Bassins Sédimentaires Maghrébins FSTGAT-USTHB 01 au 03-10-2019</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">S. Khanfer</style></author><author><style face="normal" font="default" size="100%">DJAIZ Fouad</style></author><author><style face="normal" font="default" size="100%">Lamouri Bachir</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Evolution tectono-sédimentaire du bassin néogène de Batna-Ain Touta, limite Aurès-Monts de Belezma</style></title><secondary-title><style face="normal" font="default" size="100%">Premier Colloque sur la géologie des Bassins Sédimentaires Maghrébins FSTGAT-USTHB 01 au 03-10-2019</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Benmansour Sana</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">The Campanian-Maastrichtian series of Dj. Gaâga (Tebessa, NE of Algeria) : quantitative and qualitative analysis and palaeoenvironmental interpretation</style></title><secondary-title><style face="normal" font="default" size="100%">7. INTERNANATIONAL EARTH SCIENCE COLLOQUIUM ON THE AEGEAN REGION. Izmir/ Turkiye. 7-11 october 2019</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Benmansour Sana</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Lithostratigraphical and sedimentological characterization of the Aptian formation on the Northern flank of Dj Bou Arif (NE of Algeria)</style></title><secondary-title><style face="normal" font="default" size="100%">7. INTERNANATIONAL EARTH SCIENCE COLLOQUIUM ON THE AEGEAN REGION. Izmir/ Turkiye. 7-11 october 2019</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Fouad Djaiz</style></author><author><style face="normal" font="default" size="100%">Defaflia Nabil</style></author><author><style face="normal" font="default" size="100%">ATHAMENA Ali</style></author><author><style face="normal" font="default" size="100%">Bachir Lamouri</style></author><author><style face="normal" font="default" size="100%">Mabrouk Boughdiri</style></author><author><style face="normal" font="default" size="100%">Halima Belalite</style></author><author><style face="normal" font="default" size="100%">Boushaba Abdellah</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Geological Characterization and contibution of Geophysics to the mobilization of water resources in the Ain Djasser basin (South-Sétifien, Algeria NE), ISSN 2052-3408</style></title><secondary-title><style face="normal" font="default" size="100%">The Euro-arab Organization for Environment and Water  and Desert Researches, International Journal of Environment and Water </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.researchgate.net/publication/330104660_Caracterisation_geologique_et_apport_de_la_geophysique_pour_la_mobilisation_des_ressources_hydriques_dans_le_bassin_d'Ain_Djasser_Sud-Setifien_Algerie_NE_Geological_Characterization_and_contribution_o</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Vol. 8</style></volume><pages><style face="normal" font="default" size="100%">pp. 66-77</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Le bassin d'Ain Djasser fait partie de l'ensemble Sud-Sétifien. Ce dernier est représenté par une plaine inter-montagneuse appartenant au bassin des hauts plateaux constantinois. Il est caractérisé par un climat de type méditerranéen. L'hydrologie tributaire du relief est la conséquence directe des eaux de surface et de la fonte des neiges. La synthèse géologique montre un domaine allochtone résultant d'une histoire polyphasée associant les tectoniques atlasique et alpine. Ce dernier est caractérisé par des séries sédimentaires carbonatées colmaté par d'abondantes formations terrigènes. L'alimentation de l'eau souterraine des différentes nappes profondes à semi-profondes provient essentiellement de l'infiltration des eaux de pluies. Ce cortège de roche forme une nappe libre et captive, par endroit recoupée par des forages à des profondeurs de 178 à 330 m, fournissant un débit moyen de 15 l/s. L'interprétation des coupes géoélectriques du bassin montrent, (i) des formations alluvionnaires du mio-plio-quaternaire de quelques dizaines de mètres qui forment un bon aquifère superficiel, (ii) des calcaires fissurés du jurassico-crétacé dont le toit est atteint à des profondeurs variables est un aquifère captif. L'influence d'accidents entre les différents blocs rend possible une éventuelle alimentation des aquifères entres eux. L'analyse litho-stratigraphique montre que le substratum et la couverture sédimentaire ne présentent pas de grandes variations latérales. Par contre, nous observons au niveau des sondages une variation dans l'épaisseur et la lithologie des couches, essentiellement au niveau de la formation du remplissage mio-plio-quaternaire. L'objectif de cette étude réside pour l'essentiel, dans la mobilisation des ressources en eaux superficielles et souterraine pour leurs exploitations dans les domaines agricoles et l'élevage, en vue d'une utilisation rationnelle et planifiée de cet élément vital qu'est l'eau</style></abstract><issue><style face="normal" font="default" size="100%">Issue3</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Analyse statistique des paramètres hydrochimiques du continental intercalaire de la région de biskra - sud-est algérien</style></title><secondary-title><style face="normal" font="default" size="100%">1st national seminar on geosciences and environment SGSE'19, Tamanrasset, Algérie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Chafou Nasereddine</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation hydrochimique et aptitude à l&amp;#39;irrigation des eaux du (CI) dans la région de Touggourt -ouargla- Oued Righ au sud algérien</style></title><secondary-title><style face="normal" font="default" size="100%">1st national seminar on geosciences and environment SGSE'19, Tamanrasset, Algérie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Chafou Nasereddine</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Analyse statistique des paramètres hydrochimiques du continental intercalaire de la région de biskra - sud-est algérien</style></title><secondary-title><style face="normal" font="default" size="100%">1st national seminar on geosciences and environment SGSE'19, Tamanrasset, Algérie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation hydrochimique et aptitude à l&amp;#39;irrigation des eaux du (CI) dans la région de Touggourt -ouargla- Oued Righ au sud algérien</style></title><secondary-title><style face="normal" font="default" size="100%">1st national seminar on geosciences and environment SGSE'19, Tamanrasset, Algérie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Mekoussi Adel</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Identification des paramètres responsables de la minéralisation des sources d&amp;#39;eau utilisées pour l&amp;#39;irrigation dans le synclinal de BOUZINA, Nord est algérien</style></title><secondary-title><style face="normal" font="default" size="100%">Seminaire international sur l'hydrogéologie et l'environnement , Ouargla Algerie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Identification des paramètres responsables de la minéralisation des sources d&amp;#39;eau utilisées pour l&amp;#39;irrigation dans le synclinal de BOUZINA, Nord est algérien</style></title><secondary-title><style face="normal" font="default" size="100%">Seminaire international sur l'hydrogéologie et l'environnement , Ouargla Algerie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Identification des aquifères par les méthodes géophysiques. Cas du système aquifère de hammam bradaa nord-est de guelma. Algérie</style></title><secondary-title><style face="normal" font="default" size="100%">Colloque sur le géologie des bassins sédimentaires Maghrebins Alger, Algérie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Azizi Yacine</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">Boucenna Fatih</style></author><author><style face="normal" font="default" size="100%">Ag Maatallah Lamine</style></author><author><style face="normal" font="default" size="100%">Bouaam Med Lamine</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Caractérisation de potentialité aquifère du socle cristallin par les apports de la télédétection et de SIG (région de Tamanrasset)</style></title><secondary-title><style face="normal" font="default" size="100%">1er Séminaire National sur les géosciences et l'environnement SGSE'2019</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Azizi Yacine</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author><author><style face="normal" font="default" size="100%">Boumazbeur Abderrahmane</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Collapse susceptibility mapping for Karst sinkholes in Cheria area, NE Algeria</style></title><secondary-title><style face="normal" font="default" size="100%">1er Séminaire National sur les géosciences et l'environnement SGSE'2019</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Rihani Abla</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Hydrogeology of montain basin, cas of O. Labiod, North Eastern of Algreia</style></title><secondary-title><style face="normal" font="default" size="100%">15 th ICWRE - Antalya, Turkey, 25-28 Oct </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Boudjema A</style></author><author><style face="normal" font="default" size="100%">Guettaia Sabrine</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">statistical and hydrochemical classification of underground waters in a multi-layer aquifer system in an arid zone: application to chott el gharbi basin (extreme west of algeria), ISSN: 1112-9867 </style></title><secondary-title><style face="normal" font="default" size="100%">Journal of Fundamental and Applied Sciences</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><volume><style face="normal" font="default" size="100%">volume 11</style></volume><pages><style face="normal" font="default" size="100%">pp.786-803</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><issue><style face="normal" font="default" size="100%">issue 2</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Belouanas Hamza</style></author><author><style face="normal" font="default" size="100%">MENANI Mohamed redha</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Characterization on Contentinetal Intercalaire Aquifer (CI) in the Tinrhert East Area-Illizi basin on the Algerian-Libyan Border, June, ISSN / e-ISSN: 2305 - 7068 / 1674-6767 </style></title><secondary-title><style face="normal" font="default" size="100%">Journal of groundwater science and engineering. </style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://gwse.iheg.org.cn/EN/abstract/abstract367.shtml</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">vol 7</style></volume><pages><style face="normal" font="default" size="100%">pp.115-132</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">This paper addresses the characterization of the Continental Intercalaire aquifer (CI) in the Tinrhert-East area of Illizi Basin on the Algerian-Libyan border, which belongs to the SASS1 system, one of the biggest transboundary aquifers in the world. This study concerns a superficies of 4 300 km2. On the basis of Mud Logging borehole data conducted in this part of the aquifer, a realistic characterization of the aquifer was done. The thickness of the CI aquifer varies from 300 m in the south to 700 m in the north, and the depth ranges from 180 m to 320 m. The interpretation of the logs showed that the aquifer is characterized by a maximum net thickness in its southwestern part (more than 600 m), the porosity is very high, ranging from 30% in the west to 24% at the Libyan borders, the permeability is low to medium around 10-5 m/s, and the maximum transmissivity values of about 8×10-3 m2/s were recorded at the center of the study area. The depth of water varies from 235 m to 312 m, and the water flows from south to north, in accordance with the general direction observed in the CI aquifer in the Northern Sahara Aquifer System (SASS). The porosity values obtained from the interpretation of the sonic and density logs permit to estimate the water reserves of this aquifer considered fossil, at thresholds much higher than what was considered until now.</style></abstract><issue><style face="normal" font="default" size="100%">n°2</style></issue></record></records></xml>