<?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%">Brahmia Ali</style></author><author><style face="normal" font="default" size="100%">Brinis Nafaa</style></author><author><style face="normal" font="default" size="100%">Nouar Tahar</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Statistical and hydro-geochemical characteristics of the M&amp;rsquo;daourouch-Drea plain&amp;rsquo;s groundwater; North-east of Algeria, ISSN / e-ISSN 1429-7426 / 2083-4535</style></title><secondary-title><style face="normal" font="default" size="100%">Journal of Water and Land Development</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.degruyter.com/downloadpdf/j/jwld.2018.38.issue-1/jwld-2018-0038/jwld-2018-0038.pdf</style></url></web-urls></urls><pages><style face="normal" font="default" size="100%"> pp 19–26. (VII-IX) 2018 (promesse de publication).</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:146.5px;top:687.918px;16.7px;serif;transform:scaleX(1.01679);&quot;&gt;This work was conducted on 23 samples distributed between sprin&lt;/span&gt;&lt;span style=&quot;left:597.798px;top:687.918px;16.7px;serif;transform:scaleX(1.01856);&quot;&gt;gs, wells and boreholes tapping the shal-&lt;/span&gt;&lt;span style=&quot;left:118.2px;top:707.118px;16.7px;serif;transform:scaleX(1.03235);&quot;&gt;low and deep aquifer in the M'Daourouch-Drea area located in ex&lt;/span&gt;&lt;span style=&quot;left:570.299px;top:707.118px;16.7px;serif;transform:scaleX(1.02727);&quot;&gt;treme northeast of Algeria. Ca&lt;/span&gt;&lt;span style=&quot;left:778.5px;top:704.876px;10.8px;serif;transform:scaleX(1.00066);&quot;&gt;2+&lt;/span&gt;&lt;span style=&quot;left:790px;top:707.118px;16.7px;serif;transform:scaleX(1.04393);&quot;&gt;, Mg&lt;/span&gt;&lt;span style=&quot;left:823px;top:704.876px;10.8px;serif;transform:scaleX(1.00066);&quot;&gt;2+&lt;/span&gt;&lt;span style=&quot;left:834.5px;top:707.118px;16.7px;serif;transform:scaleX(1.05444);&quot;&gt;, Na&lt;/span&gt;&lt;span style=&quot;left:863.7999999999998px;top:704.8754765625px;10.799999999999999px;serif;&quot;&gt;+&lt;/span&gt;&lt;span style=&quot;left:869.9px;top:707.118px;16.7px;serif;transform:scaleX(1.006);&quot;&gt;, &lt;/span&gt;&lt;span style=&quot;left:118.20237199999988px;top:726.217698203125px;16.7px;serif;&quot;&gt;K&lt;/span&gt;&lt;span style=&quot;left:130.3px;top:723.9754765624999px;10.799999999999999px;serif;&quot;&gt;+&lt;/span&gt;&lt;span style=&quot;left:136.4px;top:726.218px;16.7px;serif;transform:scaleX(1.01316);&quot;&gt;, Cl&lt;/span&gt;&lt;span style=&quot;left:160.79999999999998px;top:723.9754765624999px;10.799999999999999px;serif;&quot;&gt;–&lt;/span&gt;&lt;span style=&quot;left:166.2px;top:726.218px;16.7px;serif;transform:scaleX(1.00919);&quot;&gt;, SO&lt;/span&gt;&lt;span style=&quot;left:196.2px;top:733.9754765624999px;10.799999999999999px;serif;&quot;&gt;4&lt;/span&gt;&lt;span style=&quot;left:201.6px;top:723.976px;10.8px;serif;transform:scaleX(0.999999);&quot;&gt;2–&lt;/span&gt;&lt;span style=&quot;left:212.4px;top:726.218px;16.7px;serif;transform:scaleX(1.00141);&quot;&gt;, HCO&lt;/span&gt;&lt;span style=&quot;left:256.2px;top:733.9754765624999px;10.799999999999999px;serif;&quot;&gt;3&lt;/span&gt;&lt;span style=&quot;left:261.59999246666666px;top:723.9757565624999px;10.799999999999999px;serif;&quot;&gt;–&lt;/span&gt;&lt;span style=&quot;left:267px;top:726.218px;16.7px;serif;transform:scaleX(1.01348);&quot;&gt; and NO&lt;/span&gt;&lt;span style=&quot;left:324.09999999999997px;top:733.9754765624999px;10.799999999999999px;serif;&quot;&gt;3&lt;/span&gt;&lt;span style=&quot;left:329.49999246666664px;top:723.9757565624999px;10.799999999999999px;serif;&quot;&gt;–&lt;/span&gt;&lt;span style=&quot;left:334.9px;top:726.218px;16.7px;serif;transform:scaleX(1.00336);&quot;&gt; were analysed. The interpreta&lt;/span&gt;&lt;span style=&quot;left:537.399px;top:726.218px;16.7px;serif;transform:scaleX(1.00219);&quot;&gt;tion of the geological-geophysica&lt;/span&gt;&lt;span style=&quot;left:760.897px;top:726.218px;16.7px;serif;transform:scaleX(1.00361);&quot;&gt;l data allowed us &lt;/span&gt;&lt;span style=&quot;left:118.201px;top:745.418px;16.7px;serif;transform:scaleX(1.02106);&quot;&gt;to highlight two aquifers. The first consists of conglomerates,&lt;/span&gt;&lt;span style=&quot;left:537.799px;top:745.418px;16.7px;serif;transform:scaleX(1.02005);&quot;&gt; sandstones, gravels, sands, marls, limestones, la-&lt;/span&gt;&lt;span style=&quot;left:118.201px;top:764.618px;16.7px;serif;transform:scaleX(1.02594);&quot;&gt;custrine and alluvial deposits varying in thickness from a few &lt;/span&gt;&lt;span style=&quot;left:544.899px;top:764.618px;16.7px;serif;transform:scaleX(1.02638);&quot;&gt;tens to a few hundred meters, representing Neo-&lt;/span&gt;&lt;span style=&quot;left:118.201px;top:783.718px;16.7px;serif;transform:scaleX(0.998009);&quot;&gt;gene-Quaternary filling of the st&lt;/span&gt;&lt;span style=&quot;left:333px;top:783.718px;16.7px;serif;transform:scaleX(0.996796);&quot;&gt;udied basin. The second is mor&lt;/span&gt;&lt;span style=&quot;left:540.3px;top:783.718px;16.7px;serif;transform:scaleX(0.998671);&quot;&gt;e important localized in the cracked and karstified &lt;/span&gt;&lt;span style=&quot;left:118.202px;top:802.918px;16.7px;serif;transform:scaleX(1.01933);&quot;&gt;limestones of upper Cretaceous age; these limestones are outcro&lt;/span&gt;&lt;span style=&quot;left:554.1px;top:802.918px;16.7px;serif;transform:scaleX(1.03264);&quot;&gt;pped on the flanks of the syncline and the bor-&lt;/span&gt;&lt;span style=&quot;left:118.202px;top:822.118px;16.7px;serif;transform:scaleX(0.999164);&quot;&gt;ders of the basin. The first aqui&lt;/span&gt;&lt;span style=&quot;left:326.301px;top:822.118px;16.7px;serif;transform:scaleX(0.999189);&quot;&gt;fer sometimes rests directly o&lt;/span&gt;&lt;span style=&quot;left:522.8px;top:822.118px;16.7px;serif;transform:scaleX(0.999564);&quot;&gt;n the second which allows hydraulic communication &lt;/span&gt;&lt;span style=&quot;left:118.202px;top:841.217px;16.7px;serif;transform:scaleX(1.00093);&quot;&gt;between them. The hydogeochemical and statistical study, with t&lt;/span&gt;&lt;span style=&quot;left:549.8px;top:841.217px;16.7px;serif;transform:scaleX(0.997864);&quot;&gt;he combination of numerous tools, indicates that &lt;/span&gt;&lt;span style=&quot;left:118.202px;top:860.417px;16.7px;serif;transform:scaleX(1.01258);&quot;&gt;the chemistry of groundwater in t&lt;/span&gt;&lt;span style=&quot;left:344.101px;top:860.417px;16.7px;serif;transform:scaleX(1.00969);&quot;&gt;he M'Daourouch-Drea Plain is c&lt;/span&gt;&lt;span style=&quot;left:561.6px;top:860.417px;16.7px;serif;transform:scaleX(1.0143);&quot;&gt;ontrolled both by the dissolution of the miner-&lt;/span&gt;&lt;span style=&quot;left:118.202px;top:879.617px;16.7px;serif;transform:scaleX(0.998243);&quot;&gt;als of the evaporite formations and those of the carbonate form&lt;/span&gt;&lt;span style=&quot;left:537.4px;top:879.617px;16.7px;serif;transform:scaleX(0.999627);&quot;&gt;ations.&lt;/span&gt;</style></abstract><issue><style face="normal" font="default" size="100%">N°38</style></issue></record></records></xml>