Demirel Zeynel
Department of Geological Engineering, Faculty of Engineering, Mersin University, Turkey.
J Environ Manage. 2004 Mar;70(3):275-82. doi: 10.1016/j.jenvman.2003.12.007.
The Mersin-Kazanli 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.
梅尔辛-卡赞勒地区是一个工业化密集的地区。工厂和城镇的用水需求依靠地下水来满足。随着用水需求的增加，海水入侵现象出现了。自这些水井钻探以来，已定期对一些水井的水样中的氯化物浓度进行分析。这些分析结果和电导率测量结果被用于展示直至2000年海水入侵的历史和发展情况。1999年，冲积含水层内水体的Cl(-)浓度增加到超过3000毫克/升，这些水井被完全关闭。2001年，在距离大海和旧井场1公里多的地方钻了新的水井。根据2001年进行的分析结果，确定了当前的地下水水质。该地下水属于镁-钙-重碳酸盐类型，这种成分受水与冲积沉积物之间相互作用的控制。
