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Geophysical Method of Investigating Groundwater and Sub-Soil Contamination: A Case Study

机译:调查地下水和地下土壤污染的地球物理方法:一个案例研究

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Geophysical methods can be helpful in mapping areas of contaminated soil and groundwater. Electrical resistivity surveys were carried out at a site of shallow hydrocarbon contamination in Ahoada, South South Nigeria. This was aimed at evaluating the subsoil conditions and groundwater quality of the area 3 years after the post-spill clean-up exercise. The geophysical investigation involved the Vertical Electrical Sounding (VES) technique using the Schlumberger configuration and the horizontal profiling method. The data from the two different approaches correlate well and the generated profiles of the acquired data helped to map the contaminant plume which was delineated as an area of high interpreted resistivities. The VES result shows that the subsurface layers up to a depth of 49 m is of moderate to high resistivity values (>200 Ωm) that may affect crops and groundwater development in the study area. However, good aquifer can still be obtained from the depth of 30 m and above.
机译:物探方法可有助于绘制受污染的土壤和地下水区域的图。电阻率调查是在尼日利亚南部南部Ahoada的一个浅层碳氢化合物污染现场进行的。这项工作旨在评估泄漏后清理工作三年后该地区的地下土壤状况和地下水质量。地球物理研究涉及使用斯伦贝谢构造和水平剖面法的垂直电测深(VES)技术。来自两种不同方法的数据具有良好的相关性,并且所获取数据的生成轮廓有助于绘制污染物羽流图,该污染物羽流被描绘为高解释电阻率区域。 VES结果表明,深度达49 m的地下层具有中等至较高的电阻率值(> 200Ωm),可能会影响研究区域的作物和地下水发育。但是,从30 m及以上的深度仍可获得良好的含水层。

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