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Assessment of groundwater potential based on aquifer properties of hard rock terrain in the Chittar–Uppodai watershed, Tamil Nadu, India

机译:根据印度泰米尔纳德邦奇塔尔-乌波代代流域硬岩地形的含水层特性评估地下水潜力

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摘要

Aquifer performance was tested in 24 locations to assess the groundwater potential of the hard rock terrain in the Chittar–Uppodai watershed of the Tambaraparani River basin. Geologically, the area consists of biotite gneiss, charnockite, and quartzite. The aquifer characteristics, such as transmissivity (T), the storage coefficient, specific capacity, optimum yield, and the recovery rate were calculated. The drawdown transmissivity was determined using Jacob’s straight-line method, while the recovery transmissivity was determined by the Theis method. The drawdown transmissivity was low in the western areas, particularly at Kadayanallur, and was higher in the other areas. The recovery transmissivity was high in the western area, and, with the exception of Gangaikondan, was low at other locations. The assessment indicates that there is groundwater potential in the western part of the study area because of favorable results for recovery drawdown, aquifer thickness, and specific capacity.
机译:在24个位置测试了含水层的性能,以评估坦巴拉巴拉尼河流域奇塔尔-乌波代代流域硬岩地形的地下水潜力。从地质学上讲,该地区由黑云母片麻岩,夏诺克岩和石英岩组成。计算了水层特征,如透射率(T),储水系数,比容,最佳产量和回收率。垂降透射率使用雅各布的直线法确定,恢复透射率通过Theis方法确定。在西部地区,尤其是在Kadayanallur,回落率较低,而在其他地区则较高。西部地区的恢复透射率较高,而Gangaikondan除外,其他地区的恢复透射率较低。评估表明,由于采收量下降,含水层厚度和比容的有利结果,研究区域的西部存在地下水潜力。

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