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Direct determination of aquifer configuration using geoelectrical techniques in a piedmont zone, Himalayan foothills region, India

机译:在印度喜马拉雅山麓地区的皮埃蒙特地区,使用地电技术直接确定含水层的构造

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Geoelectrical techniques have been used to define the geometry of aquifer systems in the Pathri-Rao watershed situated in the piedmont zone of the Himalayan foothill region, Uttarakhand, India. This has been done by integrating the results of dc resistivity and electromagnetic data recorded in the area. Two-dimensional resistivity imaging was carried out to define the horizontal and vertical geometry of the aquifer system and to infer the local groundwater flow condition. On the basis of resistivity values it was found that shallow and deep aquifers have different degrees of interaction in the area. The study demonstrates the versatility of geoelectrical techniques.
机译:地电技术已被用于定义位于印度北阿坎德邦喜马拉雅山麓地区前山带的Pathri-Rao流域中含水层系统的几何形状。这是通过将直流电阻率和记录在该区域中的电磁数据的结果进行积分来完成的。进行了二维电阻率成像,以定义含水层系统的水平和垂直几何形状,并推断局部地下水流动状况。根据电阻率值,发现该区域的浅层和深层含水层具有不同程度的相互作用。该研究证明了地电技术的多功能性。

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