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The history and evaluation of saltwater intrusion into a coastal aquifer in Mersin, Turkey

机译:土耳其梅尔辛市咸水入侵沿海含水层的历史和评估

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The Mersin-Kazanh region is a densely industrialized region. The factories and towns cover their water demand from groundwater. With the increased water demand, saltwater intrusion has occurred. The chloride concentration of the water samples from some wells has been analysed periodically since these wells were drilled. The results of these analyses and electrical conductivity measurements were used to show the history and development of saltwater intrusion up to the year 2000. The Cl~- concentration of the water within the alluvial aquifer increased to over 3000 mg/l in 1999 and the wells were closed completely. In 2001 new wells were drilled more than 1 km away from the sea and old well field. With the results of the analyses conducted in 2001, the current groundwater quality was determined. The ground water is of the magnesium-calcium-bicarbonate type and this composition is controlled by the interaction of the water with the sediments of alluvial deposits.
机译:Mersin-Kazanh地区是一个工业密集区。工厂和城镇满足了地下水的用水需求。随着需水量的增加,发生了盐水入侵。自从钻探这些井以来,已经定期分析了一些井中水样的氯离子浓度。这些分析和电导率测量的结果用于显示直到2000年咸水入侵的历史和发展。1999年,冲积层中水的Cl〜-浓度增加到3000 mg / l以上。被完全关闭。 2001年,在距海洋和老井场1公里以上的地方钻了新井。根据2001年的分析结果,确定了当前的地下水水质。地下水是镁-碳酸氢钙类型的,并且该成分通过水与冲积物沉积物的相互作用来控制。

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