Groundwater Pathway Mapping Using Electrical Resistivity Tomography (ERT) Method

Syazwan Aiman Sufiyanussuari, S. A. AHMAD TAJUDIN, Mohammad Izzat Shaffiq Azmi, M. N. H. Zahari, Nordiana MOHD MUZTAZA
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Abstract

Geophysical electrical resistivity method has been one of the more popular non-destructive method to explore the subsurface. Geophysical electrical resistivity tomography (ERT) subsurface profiling was conducted to map the groundwater path along the embankment. The groundwater path able to decrease the slope stability, thus its need to locate the position for conduct the slope remediation via subsoil drainage. In this study, Terrameter LS2 model, electrodes, cables, battery, and cable connectors were the equipment used for measurement. This study uses cable spread line at 200m with 2.5m spacing between electrodes by using gradient protocol. The resistivity data was analyzed using RES2DINV software. The interpretation of groundwater path is based on the resistivity values less than 100 ohm.m, which is interpreted as saturated materials. This study demonstrates the efficiency of application of electrical resistivity tomography (ERT) in detecting the groundwater pathways. This investigation will help in sustaining the slope stability via indicating the position of groundwater pathways, and thus implementing the slope remediation work.
利用电阻率层析成像(ERT)方法绘制地下水通道
地球物理电阻率法是目前较为流行的地下勘探非破坏性方法之一。采用地球物理电阻率层析成像(ERT)地下剖面法绘制了路基地下水路径图。地下水通道会降低边坡的稳定性,因此需要确定通过底土排水进行边坡修复的位置。在本研究中,用于测量的设备为Terrameter LS2模型、电极、电缆、电池和电缆连接器。本研究采用梯度协议,在200m处采用电缆展线,电极间距2.5m。利用RES2DINV软件对电阻率数据进行分析。地下水路径的解释是基于小于100欧姆的电阻率值。M,被解释为饱和材料。本研究证明了电阻率层析成像(ERT)在地下水通道探测中的有效性。这项调查将有助于通过指示地下水通道的位置来维持边坡的稳定性,从而实施边坡修复工作。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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