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首页> 外文期刊>Journal of applied science & environmental management: JASEM >2D Geo-Electrical Imaging for Groundwater Exploration in Shika, along Zaria-Funtua Road North of Ahmadu Bello University Main Campus, Samaru, Zaria
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2D Geo-Electrical Imaging for Groundwater Exploration in Shika, along Zaria-Funtua Road North of Ahmadu Bello University Main Campus, Samaru, Zaria

机译:位于Zaria Samaru Ahmadu Bello大学主校区以北的Zaria-Funtua路沿Shika进行地下水勘探的2D地电成像

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A two dimensional (2D) geoelectrical tomography of Ahmadu Bello University Teaching HospitalPremises was carried out with the aim of identifying a suitable location for siting a borehole. This was sequel to the factthat a borehole drilled without proper geophysical investigation in the quarters for resident doctors did not produce water.State-of-the-art equipment was employed and 2D surveying proved a powerful geological mapping tool, for use inhydrogeological mapping including engineering and environmental applications. The 2D inversion results of the surveywere correlated with the lithology information obtained from the boreholes in Jama’a village, and the hostels and theresidential quarters of ABUTH. The stratigraphic structure of the study area is very complex and is a product of volcanicand magmatic activities of various ages. Based on the geo-electrical images obtained in the study area, three distinct layerswere revealed, the overburden with an average thickness of about 16 m – 26 m. The overburden is immediately underlainby the weathered basement, 5 m – 14 m thick which consists of disintegrated schistose rock materials, sand and gravel.This layer has a relatively low resistivity due to the presence of water and clay, which reduces the permeability, so thislayer is thus regarded as the aquifer. The fresh basement rock was encountered at a variable depth of between 21 m and30 m with resistivity 1223 Ωm up to 11918 Ωm. These results agree with the borehole logs. The complete set of boreholelogs used in this research were obtained from the original hydro-geologic assessment report of the groundwater researchdepartment of the National Water Resources Institute (NWRI), Mando, Kaduna; Kaduna State, Nigeria.
机译:进行了Ahmadu Bello大学教学医院校舍的二维(2D)地电层析成像,目的是确定合适的钻孔位置。这是以下事实的结果:在驻地医生的宿舍中未经适当的地球物理调查而钻出的钻孔不会产生水。采用了最先进的设备,二维勘测证明了强大的地质测绘工具,可用于包括工程在内的水文地质测绘和环境应用。勘测的二维反演结果与从贾马村的钻孔以及ABUTH的旅馆和住宅区获得的岩性信息相关。研究区域的地层结构非常复杂,是不同年龄火山和岩浆活动的产物。根据研究区域获得的地电图像,揭示了三个不同的层,覆盖层的平均厚度约为16 m – 26 m。覆盖层立即被风化的地下层覆盖,地下层厚5 m – 14 m,由崩解的片状岩石材料,沙子和砾石组成。该层由于存在水和粘土而具有较低的电阻率,从而降低了渗透率,因此该层因此被视为含水层。在21 m至> 30 m的可变深度处遇到了新鲜的基底岩石,电阻率从1223Ωm到11918Ωm。这些结果与钻孔测井结果一致。本研究中使用的完整的井眼测井数据是从卡杜纳州曼多市国家水资源研究所(NWRI)地下水研究部门的原始水文地质评估报告中获得的。尼日利亚卡杜纳州。

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