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Geoelectrical Survey for Engineering Investigation

机译:工程勘察用地电勘测

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Water seepage erosion has been and remains one of the major engineering problems. However, most engineers will much depend on borehole data and soil test for designing and problem detection. By considering of the cost and destructive method, selection of geoelectrical prospecting would be appropriate. Therefore, two electrical geophysical surveys were carried out in Sekolah Menengah Kebangsaan Dato’ Haji Mohd Nor, Gelugor, Pulau Pinang to map the presence of the unknown underground water sources (saturated zones) and its movement. With the total of seven resistivity lines parallel to each other and self potential (SP) with 5 m × 5 m gridding survey were successfully done. The resistivity result from line 1 (R1) to line 6 (R6) shows the subsurface consist of saturated zones with range between 3 m up to 10 m depth, before it reaches the R7 which is believed as the accumulation zone. Meanwhile, as for SP result it shows the water flow from higher value (north-east) towards the lower value which is mostly at the south area. In conclusion, geoelectrical survey could assist in detecting and solving engineering problems as it proven by the result from each method.
机译:渗水侵蚀一直是并且仍然是主要的工程问题之一。但是,大多数工程师将在很大程度上依赖于钻孔数据和土壤测试来进行设计和问题检测。考虑到成本和破坏性方法,选择地电勘探将是适当的。因此,在槟榔屿槟榔格的Sekolah Menengah Kebangsaan Dato’s Haji Mohd Nor进行了两次电地球物理勘测,以绘制未知地下水源(饱和区)及其运动的地图。在总共7条电阻率线相互平行的情况下,成功完成了5 m×5 m网格测量的自电位(SP)。从线1(R1)到线6(R6)的电阻率结果表明,地下层在到达R7之前被认为是累积区,该饱和区的范围在3 m至10 m深度之间。同时,对于SP结果,它显示了从较高值(东北)到较低值(主要在南部地区)的水流。总而言之,地电勘测可以帮助检测和解决工程问题,正如每种方法的结果所证明的那样。

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