Exploring groundwater resources in southwestern Nigeria: An integrated geophysical approach

I.O. Idowu , A.O. Ojo
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引用次数: 0

Abstract

Groundwater potential regions were delineated using Very-Low Frequency Electromagnetic (VLF-EM) and Vertical Electrical Sounding (VES) geophysical techniques. The VLF-EM measurements were taken as fast reconnaissance to delineate shallow conductive features along seven traverses with 10 m station intervals. The data were qualitatively analyzed and indicated zones of hydrogeological relevance, pointing to regions for VES investigations. Thirteen VESs were mapped with 100 m intervals between current electrodes, and the data were processed manually and using WinResist software to generate sounding curves and geo-electric sections that revealed 3 (84.6%) and 4 (15.4%) layers of earth models. The aquifer units were found in the weathered and fractured layers. The subsurface was classified into high, medium, and low groundwater potential regions, with a larger area indicating low prospects. Regions with high potentials had overburden thicknesses above 18 m, while medium and low yields had overburden thicknesses of 13–18 m and below 13 m, respectively.

尼日利亚西南部地下水资源勘探:综合地球物理方法
利用甚低频电磁(VLF-EM)和垂直电探测(VES)地球物理技术划定了地下水潜势区。甚低频电磁(VLF-EM)测量是作为快速勘测进行的,目的是沿 7 条 10 米站间距的横断面划定浅层传导特征。对数据进行了定性分析,指出了与水文地质相关的区域,并指出了进行 VES 调查的区域。绘制了 13 个电流电极间距为 100 米的 VES 图,并通过人工和 WinResist 软件对数据进行了处理,生成了探测曲线和地电剖面图,显示了 3 层(84.6%)和 4 层(15.4%)的地层模型。含水层单元位于风化层和断裂层中。地下分为高、中、低地下水潜势区,面积越大,地下水潜势越低。高地下水潜力区的覆土厚度在 18 米以上,而中等和低地下水产 量区的覆土厚度分别为 13-18 米和 13 米以下。
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CiteScore
9.20
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