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Slope Monitoring by Using 2-D Resistivity Method at Sungai Batu, Pulau Pinang, Malaysia

机译:在马来西亚槟城的Sungai Batu使用2-D电阻率法

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Slope is a dynamic system of geo-environmental phenomena that related to the movement of the soil and rock masses. In Pulau Pinang, the occurrence of slope related phenomena such as landslide and rock fall has become a huge issue especially during rainy season as the government would have to invest more for the people safety. 2-D resistivity method is one of the geophysical methods that can be applied to overcome this issue thus prepare countermeasure actions. Monitoring is one of the common acquisition technique that has been used in solving such issue. This technique was applied to identify and monitor changes at the suspected area and thus, countermeasure steps can be taken accordingly and not blindfolded. Starting from August until November 2016, a 200 m survey line of 2-D resistivity survey had been conducted monthly at Sungai Batu, Pulau Pinang slope for monitoring purpose. Three resistivity ranges were able to detect within the subsurface. Resistivity value of 250 - 400 Ωm indicated the low resistivity value and interpreted as the weak zone located at distance of 90 - 120 m with depth of 10 m. Intermediate resistivity value was interpreted as weathered granite zone with resistivity value of 400 - 1500 Ωm was found at almost along survey line. High resistivity value was > 5000 Ωm and interpreted as granitic bedrock located at depth of > 20 m. Aside from weathered granite zone and weak zone, a fracture was found develop over time at distance of 130 - 140 m. The features found have the potential to be the cause for slope failure phenomena to occur. As a conclusion, monitoring slope using 2-D resistivity method is a success and indeed helpful in overcome landslide and rock fall issue as a pre-countermeasure action.
机译:坡是一种与土壤和岩石的运动有关的地质环境现象的动态系统。在Pulau Pinang,坡度相关现象如滑坡和岩石跌倒的发生,尤其是在雨季,因为政府必须为人民的安全投资更多。 2-D电阻率方法是可以应用于克服这一问题的地球物理方法之一,从而准备对策行动。监控是解决此类问题的常见收购技术之一。应用该技术以识别和监测疑似区域的变化,因此,可以相应地采取对策步骤而不蒙上蒙上。从8月到2016年11月开始,每月在Pulau Pinang Spacope的Sungai Batu进行2-D电阻率调查的200米测量线,用于监测目的。三种电阻率范围能够检测到地下。电阻率值为250-400Ωm表示低电阻率值,并以距离为90-20米的距离,深度为10米的弱区。中间电阻率值被解释为具有电阻率值400-1500Ωm的风化花岗岩区域,几乎沿着调查线发现。高电阻率值>5000Ωm,并以距离>20μm的深度位于较深的花岗岩基岩。除了风化花岗岩区和弱区外,在130-140米的距离下发现骨折随时间发育。发现的特征有可能成为斜坡故障现象的原因。作为一种结论,使用2-D电阻率法监测坡度是成功,并且确实有助于克服滑坡和岩石坠落问题作为对策前行动。

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