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2D Resistivity Method in Delineating Subsurface Problems in Urban Area

机译:划定城市地区地下问题的2D电阻率法

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2D resistivity is carried out to detect spread saturated zone and subsurface problems cause by the presence of underground river, which resulted from selected urban area at Selangor, Malaysia. Six 2D resistivity survey lines with minimum 5 m electrode spacing were executed using Pole-dipole array. Borehole was carried out at multiple locations in the study area. Subsequently, the borehole was used to verify the 2D resistivity results. Interpretation of 2D resistivity data showed a low resistivity value (< 40 ohm-m), which appears to be a zone that is fully saturated with sandy silt and this could be an influence factor the increasing water level because sandy silt is highly permeable in nature. The borehole, support the results of 2D resistivity method relating a saturated zone in the survey area. There is a good correlation between the 2D resistivity investigations and the results of borehole records.
机译:通过地下河流的存在,进行了2D电阻率以检测扩散饱和区和地下问题,导致来自马来西亚雪兰莪的选定城区。使用极点偶极阵列执行具有最小5 M电极间距的六个2D电阻率测量线。在研究区域的多个位置进行钻孔。随后,使用钻孔来验证2D电阻率结果。对2D电阻率数据的解释显示了低电阻率值(<40欧姆-M),这似乎是与桑迪淤泥完全饱和的区域,这可能是水平增加的影响因素,因为沙质淤泥在自然界中高度渗透。钻孔,支持调查区域中饱和区的2D电阻率法的结果。 2D电阻率研究与钻孔记录结果之间存在良好的相关性。

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