首页> 外文会议>Kovacs Colloquium on Hydrological Sciences and Water Security: Past, Present and Future >Using geochemical investigations for determining the interaction between groundwater and saline water in arid areas: case of the Wadi Ouazzi basin (Morocco)
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Using geochemical investigations for determining the interaction between groundwater and saline water in arid areas: case of the Wadi Ouazzi basin (Morocco)

机译:利用地球化学研究确定干旱地区地下水和盐水之间的相互作用:WADI OUAZZI盆地(摩洛哥)的情况

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The characteristics of the Essaouira basin water resources are a semi-arid climate, which is severely impacted by the climate (quantity and quality). Considering the importance of the Essaouira aquifer in the groundwater supply of the region, a study was conducted in order to understand groundwater evolution in this aquifer. The Essaouira aquifer is a coastal aquifer located on the Atlantic coastline of southern Morocco, corresponding to a sedimentary basin with an area of nearly 200 km~2. The control of the fluid exchange and the influence of mixing zones between the groundwater and saline water was investigated by sampling from 20 wells, drillings and sources belonging to the Plio-Quaternary and Turonian aquifers.
机译:Essaouira盆地水资源的特点是半干旱气候,受到气候(数量和质量)的严重影响。考虑到Essaouira含水层在该地区地下水供应中的重要性,进行了一项研究,以了解这种含水层的地下水进化。 Essaouira Aquifer是一家位于摩洛哥南部大西洋海岸线的沿海含水层,对应沉积盆地,面积近200公里〜2。通过从20个孔,钻孔和所属的地板 - 四元和接合含水层采样来研究流体交换和混合区的影响。

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