印度瓦利亚尔河流域及其周边地区地球物理电磁法地下水文调查

Rajkumar Stanly , Srinivas Yasala , Rema Vaishali Murugesan
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引用次数: 4

摘要

本研究的重点是利用电阻率斯伦贝谢阵列和磁法来确定位于印度南部尾部的瓦利亚尔河流域及其周围的隐藏线条,以确定潜在的地下水带。二维径向功率谱估计表明,磁源存在的最大深度约为700 ~ 800 m。浅埋磁性烃源岩约为40 ~ 45 m。磁资料显示,该区存在北西向东西向的主要磁线。研究区电阻率测量提供了风化带、含水层电阻率和含水层厚度等次表层信息。vs -35、vs -40、vs -47对应位置为风化裂缝层,厚度大于20 m,处于磁主线走向。对于层析的主曲线,一般在硬岩区观察到H型和HA型曲线。本研究结果的解释支持了研究区沿海地区具有良好的地下水潜力。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Hydrological subsurface investigation using geophysical electrical and magnetic methods in and around Valliyar river basin, India

The focus of the present study is to identify potential groundwater zones using resistivity Schlumberger array and magnetic method for mapping hidden lineaments in and around the Valliyar river basin situated in the tail of Southern India. Estimation by 2-D radial power spectrum indicates that the maximum depth at which the magnetic source is present is about 700 m to 800 m. In case of shallow depth magnetic source rock, it is about 40 m to 45 m. The results of magnetic data have revealed the presence of a major magnetic lineament trending in NW to SE direction. The electrical resistivity survey in our study area gives information on sub-surface layers like the weathered zone, aquifer resistivity and aquifer thickness. The locations corresponding to ves-35, ves-40, and ves-47 have weathered and fracture layers having a thickness greater than 20 m, situated in the magnetic major lineament trend. Regarding master curves for layer analysis, H and HA type curves are generally observed in the hard rock region. The interpretation of results from the present study endorses that the coastal region of the study area has good groundwater potential.

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