Hydro-Geophysical Assessment of Groundwater Resources Within Parts of Omu Aran, South Western Nigeria

K. O. Iheme, A. Usman, R. I. Obaro, C. I. Aganigbo, A. Gbadebo
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引用次数: 3

Abstract

Hydro-geophysical assessment of groundwater resources in part of Omu Aran South Western Nigeria has been evaluated and analyzed with a view of delineating the groundwater potentials and aquifer characteristics within the study area. Eleven-(11) vertical electrical soundings (VES) were acquired with a maximum half current electrode spacing of 75 metres using ABEM 3000 SAS Tetrameter and the sounding data were processed and interpreted using partial curve matching method by the computer iteration techniques. Results from the geo-electric sections revealed the presence of three to five geo-electric layers. The depth to water table ranges between 2.59m and 71.9m and a resistivity of 89.9 to 3072 Ωm. The depth to Watertable is deepest around Omu area with depth of 71.9m. The result of the geophysical analysis correlates positively with themselves showing similarity in geology. The result shows that the weathered basement is a primary target for ground water exploration in the studied area, as the area is void of prominent fracture which is a target for ground water exploration. It is recommended that an average depth of 7.0m should be drilled for borehole within the northern part of the studied area and a depth of about 10.0m in the southern part of the study area. All these deductions were reached after qualitative and quantitative interpretation of the geophysical data, and considering geology of the area.
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尼日利亚西南部Omu Aran部分地区地下水资源的水文地球物理评价
对尼日利亚西南部Omu Aran部分地区地下水资源的水文地球物理评价进行了评价和分析,以期圈定研究区内的地下水潜力和含水层特征。利用ABEM 3000 SAS Tetrameter在最大半电流电极间距为75 m的条件下获得了11个垂直电测深(VES),并用计算机迭代技术对测深数据进行了部分曲线匹配处理和解释。地电剖面结果显示存在3 ~ 5个地电层。地下水位深度2.59 ~ 71.9m,电阻率89.9 ~ 3072 Ωm。至地下水位最深的是欧木一带,深度为71.9m。地球物理分析的结果与它们本身正相关,显示出地质上的相似性。结果表明,风化基底是研究区地下水勘探的首要目标,因为该区域没有明显的裂缝,是地下水勘探的目标。建议研究区北部钻孔平均深度为7.0m,研究区南部钻孔平均深度为10.0m左右。所有这些推论都是在对地球物理资料进行定性和定量解释后,结合该地区的地质情况得出的。
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