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Subsurface Investigation using 2D Resistivity and Ground Penetrating Radar at Teluk Kumbar, Penang

机译:使用 2D 电阻率和探地雷达在槟城 Teluk Kumbar 进行地下勘探

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The objective of this study is to determine the structure and condition of the subsurface by using 2D resistivity and Ground Penetrating Radar (GPR) methods. The study was conducted at SK Sungai Batu, Teluk Kumbar, Penang Island. For 2D resistivity method, Wenner-Schlumberger array was used while for GPR, 250 MHz antenna was used at the site. The survey consists of 200m length survey line. GPR result shows that there is high intensity of EM. 2D resistivity result shows that the low resistivity region (200 Ωm to 340 Ωm) appears to be at the centre of the survey line from depth 7 m to 13 m. Meanwhile, the higher resistivity region (4000 Ωm to 6000 Ωm) may indicate the bedrock structure of the subsurface, which is the granitic rock. This region is bedrock which rested at depth 14 m and below. In conclusion, data obtained from GPR and 2D resistivity methods can be easily correlated to determine the features of the subsurface.
机译:本研究的目的是使用 2D 电阻率和探地雷达 (GPR) 方法确定地下的结构和状况。该研究是在槟城岛 Teluk Kumbar 的 SK Sungai Batu 进行的。对于 2D 电阻率方法,使用 Wenner-Schlumberger 阵列,而对于 GPR,现场使用 250 MHz 天线。该测量由 200m 长的测量线组成。GPR 结果表明 EM 强度高。2D 电阻率结果表明,低电阻率区域(200 Ωm 至 340 Ωm)似乎位于深度 7 m 至 13 m 的测量线的中心。同时,较高的电阻率区域(4000 Ωm 至 6000 Ωm)可能表明地下的基岩结构,即花岗岩。这个区域是基岩,位于 14 m 及以下的深度。总之,从 GPR 和 2D 电阻率方法获得的数据可以很容易地关联起来,以确定地下的特征。

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