Evaluation of Topsoil Competence, Aquifer Types, Groundwater Prospect and Flow Pattern using Geoelectric Characterization for Part of Ogbomoso, Nigeria

O. Bayowa
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Abstract

Part of Ogbomoso Southwestern Nigeria was assessed using electrical resistivity method with a view to obtaining the subsurface geoelectric parameters (resistivities and thicknesses), categorizes the topsoil into different competence zones and evaluates the aquifer types, groundwater prospect and flow pattern. Fifty-four Vertical Electrical Sounding (VES) data were quantitatively interpreted using the partial curve matching technique to obtain the preliminary layer parameters which were further refined through 1-D forward modelling WinResist software package. The resulting final layer parameters were used to generate 2D geoelectric sections, isopach and isoresistivity maps and subsequently used to categorize the study area into different topsoil Competence, Aquifer types and Groundwater Potential zones. Static water levels of hand-dug wells in the area were used to generate the groundwater flow pattern. Four subsurface geoelectric layers were delineated. These were the topsoil, laterite, weathered/partly weathered layer (main aquifer) and fractured/fresh bedrock. The resistivities and thicknesses of the layers were 76-1858, 649-2021, 17-880 and 260-33385 Ωm and 0.4-4, 0.7-1.9 and 1.9-25.2 m respectively. The groundwater flow pattern in the area was NE-SW. The study concluded that incompetent to highly competent topsoil, weathered bedrock (main) aquifer unit/partly weathered/fractured bedrock aquifer and generally low groundwater potential with NE-SW flow direction underlay the study area.
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利用地电特征评价尼日利亚Ogbomoso部分地区表土能力、含水层类型、地下水远景和流型
采用电阻率法对尼日利亚西南部Ogbomoso部分地区进行了评价,获得了地下电参数(电阻率和厚度),将表土划分为不同的功能区,并对含水层类型、地下水远景和流型进行了评价。利用部分曲线拟合技术对54份垂直电测深(VES)数据进行定量解释,获得初步层位参数,并通过WinResist软件包进行一维正演模拟,进一步细化。得到的最终层参数用于生成二维地电剖面、等电阻率和等电阻率图,并随后用于将研究区域划分为不同的表土能力、含水层类型和地下水潜力带。利用该地区手挖井的静态水位生成地下水流型。圈定了4个地下地电层。表层土、红土、风化/部分风化层(主要含水层)和断裂/新鲜基岩。层的电阻率和厚度分别为76-1858、649-2021、17-880和260-33385 Ωm和0.4-4、0.7-1.9和1.9-25.2 m。该地区地下水流型为东北—西南。研究认为,研究区下部为不饱和-强饱和表土、风化基岩(主要)含水层单元/部分风化/裂隙基岩含水层,地下水潜力普遍较低,流向NE-SW。
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