<?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%">Drias Tarek</style></author><author><style face="normal" font="default" size="100%">Toubal Ahmed Chérif</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Heterogeneous aquifer system modelization under semi-arid climate. Geophysical Research Abstracts, EGU2010-178,</style></title><secondary-title><style face="normal" font="default" size="100%">EGU General Assembly</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2010</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">ftp://ftp.gfz-potsdam.de/home/cegit/egu/pdf/EGU2010-178.pdf </style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">Vol. 12</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;span style=&quot;left:120px;top:354.469px;16.6043px;sans-serif;transform:scaleX(0.912423);&quot;&gt;The studied zone is a part of the Mellegne’s (North-East of Algeria) under pound, this zone is characterised by its&lt;/span&gt;&lt;span style=&quot;left:120px;top:374.394px;16.6043px;sans-serif;transform:scaleX(0.921716);&quot;&gt;semi-arid climate.&lt;/span&gt;&lt;span style=&quot;left:120px;top:394.319px;16.6043px;sans-serif;transform:scaleX(0.871352);&quot;&gt;The water bearing system is formed by the plio-quaternairy alluviums resting on a marley substratuim of age&lt;/span&gt;&lt;span style=&quot;left:120px;top:414.244px;16.6043px;sans-serif;transform:scaleX(0.870331);&quot;&gt;Eocene.&lt;/span&gt;&lt;span style=&quot;left:120px;top:434.171px;16.6043px;sans-serif;transform:scaleX(0.941556);&quot;&gt;The geostatiscitcs approach of the hydrodynamics parameters (Hydrolic load, transmisivity) allowed the study&lt;/span&gt;&lt;span style=&quot;left:120px;top:454.096px;16.6043px;sans-serif;transform:scaleX(0.95235);&quot;&gt;of their spatial distrubution (casting) by the method of Krigeage by blocks and the identification of zones with&lt;/span&gt;&lt;span style=&quot;left:120px;top:474.021px;16.6043px;sans-serif;transform:scaleX(0.915133);&quot;&gt;water-bearing potentialities.&lt;/span&gt;&lt;span style=&quot;left:120px;top:493.946px;16.6043px;sans-serif;transform:scaleX(0.937062);&quot;&gt;In this respect, the zone of Ain Chabro which, is situated in the South of the plain shows the best values of the&lt;/span&gt;&lt;span style=&quot;left:120px;top:513.871px;16.6043px;sans-serif;transform:scaleX(0.935078);&quot;&gt;transmisivity......&lt;/span&gt;&lt;span style=&quot;left:120px;top:533.796px;16.6043px;sans-serif;transform:scaleX(0.928924);&quot;&gt;The use of a bidimensinnel model in the differences ended in the permanent regime allowed us to establish the&lt;/span&gt;&lt;span style=&quot;left:120px;top:553.722px;16.6043px;sans-serif;transform:scaleX(0.914152);&quot;&gt;global balence sheet (overall assessment) of the tablecloth and to refine the transmisivity field. These would vary&lt;/span&gt;&lt;span style=&quot;left:120px;top:573.647px;16.6043px;sans-serif;transform:scaleX(0.903086);&quot;&gt;more exactley between 10-4 to 10-2 m&lt;/span&gt;&lt;span style=&quot;left:375.88833333333326px;top:570.9979393333333px;11.623px;sans-serif;&quot;&gt;2&lt;/span&gt;&lt;span style=&quot;left:382.53px;top:573.647px;16.6043px;sans-serif;transform:scaleX(0.868413);&quot;&gt;/s.&lt;/span&gt;&lt;span style=&quot;left:120px;top:593.572px;16.6043px;sans-serif;transform:scaleX(0.882508);&quot;&gt;The method associating the probability appraoch of Krigeage to that determining the model has facilited the&lt;/span&gt;&lt;span style=&quot;left:120px;top:613.497px;16.6043px;sans-serif;transform:scaleX(0.926475);&quot;&gt;wedging of the model and clarified the inflitration value&lt;/span&gt;</style></abstract></record></records></xml>