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Studies of groundwater exploration in Chamarajanagar taluk, using electrical resistivity techniques, Chamarajanagar district, karnataka, south India

机译:印度南部卡纳塔克邦Chamarajanagar区,使用电阻率技术研究Chamarajanagar taluk的地下水勘探

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摘要

The geophysical methods has been used for a number of applications particularly groundwater potentialudzone. There are four important techniques like gravity, magnetic, seismic, and geoelectrical prospectingudmethods are available. Electrical resistivity (Geoelectrical) methods are the most popular among them andudits highest resolving power and economical viability. Electrical resistivity techniques to investigate theuddifferent lithological formations, bed rock dispositions, the depth to water table or zone of saturatedudformations, thickness of weathered zones, detection of fissures, fractures, fault zones, establishment ofudtheir depths, thickness and lateral extent of aquifers, groundwater flow directions, valley fills, depth toudbasement in hard rocks, fresh and salt water intrusions, groundwater prospective zones, for locating oreuddeposits and archaeological studies. In this area, electrical resistivity method has been worked to analyseudgeoelectrical parameter identification.
机译:地球物理方法已经用于许多应用,尤其是地下水潜力 udzone。有四种重要的技术,例如重力,磁力,地震和地电勘探 udmethods可用。电阻率(地电)方法是其中最受欢迎的方法,具有最高的分辨能力和经济可行性。电阻率技术,用于研究不同的岩性地层,基岩布置,到地下水位或饱和变形区域的深度,风化带的厚度,裂缝,裂缝,断层带的检测,其深度,厚度和侧向的确定含水层的范围,地下水的流动方向,河谷的填充,硬岩中至地下的深度,淡水和咸水的侵入,地下水的潜在区域,用于定位矿石沉积物和考古研究。在这个领域,电阻率法已经被用来分析预算电参数的识别。

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