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Electrical resistivity imaging and bedrock elevation in UPM, Serdang, Malaysia

机译:芬欧汇川(UPM)的电阻率成像和基岩标高

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Electrical resistivity imaging surveys have been conducted in order to locate, delineate subsurface water resource and estimate its reserve. The resistivity imaging surveys carried out basically measures and maps the resistivity of subsurface materials. A 2-D geoelectrical resistivity technique was used. Resistivity measurement was carried out using an ABEM SAS 4000 terrameter with electrode selector system. A Wenner electrode configuration was employed. The field survey was conducted along four profiles providing continuous coverage. Colour-modulated sections of resistivity versus depth were plotted for all lines, giving an approximate image of the subsurface structure. The results showed that the layers associated with the resistivities between 30 ¿.m and 1000 ¿.m and are located at a depth varying from 8 to 36 m.
机译:为了定位,划定地下水资源并估算其储量,已经进行了电阻率成像调查。进行的电阻率成像调查基本上测量并绘制了地下材料的电阻率。使用了二维地电阻率技术。使用带有电极选择器系统的ABEM SAS 4000测斜仪进行电阻率测量。使用了温纳电极构造。实地调查是沿着四个提供连续覆盖的概况进行的。绘制了所有线的电阻率对深度的颜色调制截面,从而给出了地下结构的近似图像。结果表明,与电阻率在30°C.m和1000°C.m之间的各层,位于从8到36 m不等的深度。

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