The Investigation of Mass Transfer in the Karasu Karstic Aquifer, Konya, Turkey

被引:0
|
作者
Adnan Ozdemir
Tahir M. Nalbantcilar
机构
[1] Department of Geological Engineering,
[2] University of Selcuk,undefined
[3] Konya,undefined
[4] Turkey,undefined
来源
Hydrogeology Journal | 2002年 / 10卷
关键词
Mass transfer Hydrogeology Karstic aquifer Konya Turkey;
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摘要
In this study, the changes in the chemical composition of the groundwater along a flow path were examined by using the water samples collected from unconfined, semi-confined and confined parts of the Karasu karstic aquifer. It was determined that transport of bicarbonate, calcium, and magnesium was dominant in unconfined and semi-confined parts of the aquifer, whereas calcite and dolomite precipitate in the confined parts. On the other hand, gypsum dissolution is present in all parts of the aquifer. In addition, the computed saturation indices explain the occurrences and precipitation of travertines in the Goksu Valley, which is the discharge area for the aquifer.
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页码:656 / 661
页数:5
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