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Deciphering transmissivity and hydraulic conductivity of the aquifer by vertical electrical sounding (VES) experiments in Northwest Bangladesh

机译:孟加拉国西北部垂直电探(VES)实验破译含水层的透射率和水导率

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摘要

The vertical electrical soundings (VESs) are carried out in 24 selective locations of Chapai-Nawabganj area of northwest Bangladesh to determine the transmissivity and hydraulic conductivity of the aquifer. Initially, the transmissivity and hydraulic conductivity are determined from the pumping data of nearby available production wells. Afterwards, the T and K are correlated with geoelectrical resistance and the total resistivity of the aquifer. The present study deciphers the functional analogous relations of the geoelectrical resistance with the transmissivity and the total resistivity with the hydraulic conductivity of the aquifer in northwest Bangladesh. It has been shown that the given equations provide reasonable values of transmissivity and hydraulic conductivity where pumping test information is unavailable. It can be expected that the aquifer properties viz. transmissivity and hydraulic conductivity of geologically similar area can be determined with the help of the obtained equations by conducting VES experiments.
机译:在孟加拉国西北部Chapai-Nawabganj地区的24个选择性位置进行垂直电测深(VES),以确定含水层的透射率和水力传导率。最初,传输率和水力传导率是根据附近可用生产井的抽水数据确定的。然后,将T和K与地电阻和含水层的总电阻率关联起来。本研究对孟加拉西北部含水层的地电阻与透射率以及总电阻率与水力传导率之间的功能类比关系进行了解释。已经表明,在没有泵送测试信息的情况下,给定的方程式提供了合理的透射率和水力传导率值。可以预期,含水层的性质也就是。可以通过进行VES实验,借助所获得的方程式来确定地质相似区域的透射率和水力传导率。

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