研究地下水和地下土壤污染的地球物理方法——一个案例研究

C. Nwankwo, G. Emujakporue
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引用次数: 16

摘要

地球物理方法有助于绘制受污染土壤和地下水的分布区。在尼日利亚南南Ahoada的一个浅层烃污染现场进行了电阻率调查。其目的是在溢油后清理工作进行三年后,评估该地区的底土条件和地下水质量。地球物理调查包括垂直电测深(VES)技术,采用斯伦贝谢配置和水平剖面方法。来自两种不同方法的数据相互关联良好,所获得数据的生成剖面有助于绘制污染物羽流,该区域被描绘为高解释电阻率区域。探测结果表明,研究区49 m以下的次表层具有中~高电阻率值(>200 Ώm),可能影响作物和地下水的发育。然而,在30米及以上的深度仍然可以获得良好的含水层。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Geophysical Method of Investigating Groundwater and Sub-Soil Contamination – A Case Study
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 three 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 Ώm) 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.
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