Electrical Resistivity Sounding for Groundwater Investigation around Enugu Metropolis and the Environs, Southeast Nigeria

Claris C. Nwachukwu, C. C. Ugbor, Osim Jethro Ogboke
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引用次数: 1

Abstract

This report evaluates the use of electrical method and borehole data to investigate the subsurface to delineate the groundwater potential in Enugu metropolis and the environs, south-eastern Nigeria other than rely only on resistivity method which could lead to interpretation error. Integrating these 2 data sets is key in this study. The study area is located in the Anambra Basin and is underlain by Nkporo/Enugu Shale which is overlain by the Mamu Formation. It is bounded by Latitudes 6 ̊2 0'00"N to 6 ̊30'00"N and Longitudes 7 ̊25'00"E to 7 ̊35'00"E and covers surface area of about 342 m2. Thirty-one vertical electrical soundings (VES) were carried out across the area using the Schlumberger electrode array with current electrode separation from 2 to 500 m to identify the depths and resistivity values of the identified geo-electric layers. Through data analysis using WinResist software, the apparent resistivity, thicknesses and depths and the thicknesses of the aquifers were generated. The resistivity and depths were modelled to generate resistivity map and depth map. The resistivity of the aquiferous zone within the study area varied from 20.55 427.8 ohm-m at depths of between 10.7 40.05 m. Depth to the water table appears to be shallow at the south western part of the map. The interpreted geo-electric layers show a sequence of lateritic top soil, shale, sand and shale. The frequency distribution of the VES curves generated shows the presence of 3 to 5 layers with HK type as the highest. Also, a 2D model was generated using the correlation of VES to VES data and borehole data to VES data to show the underlying stratigraphy beneath the study area as well as the direction of ground water flow. Result of the VES curve analysis reveals that the sub-surface is underlain by three lithological layers namely: lateritic top soil, shale, sand and shales with NW direction of groundwater flow from the 2D model. Groundwater prospective zones can be seen along NW, SW and How to cite this paper: Nwachukwu, C.C., Ugbor, C.C. and Ogboke, O.J. (2022) Electrical Resistivity Sounding for Groundwater Investigation around Enugu Metropolis and the Environs, Southeast Nigeria. International Journal of Geosciences, 13, 54-70. https://doi.org/10.4236/ijg.2022.131004 Received: September 26, 2021 Accepted: January 26, 2022 Published: January 29, 2022 Copyright © 2022 by author(s) and Scientific Research Publishing Inc. This work is licensed under the Creative Commons Attribution International License (CC BY 4.0). http://creativecommons.org/licenses/by/4.0/ Open Access C. C. Nwachukwu et al. DOI: 10.4236/ijg.2022.131004 55 International Journal of Geosciences central parts of the study area which have low resistivity values.
尼日利亚东南部埃努古大都市及其周边地区地下水电阻率测深研究
本报告评估了在尼日利亚东南部埃努古市及其周边地区,利用电法和钻孔数据调查地下以划定地下水潜力,而不是仅仅依靠可能导致解释误差的电阻率法。整合这两个数据集是本研究的关键。研究区位于Anambra盆地,下覆Nkporo/Enugu页岩,上覆Mamu组。它以北纬6纬20′00”~ 6纬30′00”,东经7纬25′00”~ 7纬35′00”为界,面积约342平方米。使用斯伦贝谢电极阵列,在整个区域内进行了31次垂直电测深(VES),电流电极间距为2至500 m,以确定已识别的地电层的深度和电阻率值。利用WinResist软件对数据进行分析,得到视电阻率、厚度、深度及含水层厚度。对电阻率和深度进行建模,生成电阻率图和深度图。研究区内含水层电阻率变化范围为20.55 ~ 27.8 ω -m,深度为10.7 ~ 0.05 m。在地图的西南部分,地下水位的深度似乎很浅。解释的地电层为红土表土-页岩-砂-页岩序列。生成的电磁测深曲线的频率分布显示存在3 ~ 5层,以HK型最高。利用VES数据与VES数据、钻孔数据与VES数据的相关性,生成二维模型,显示研究区下伏地层及地下水流动方向。VES曲线分析结果表明,地下发育红土、页岩、砂、页岩3个岩性层,2D模型地下水流向为NW方向。Nwachukwu, C.C., Ugbor, C.C.和Ogboke, O.J.(2022)尼日利亚东南部埃努古大都市及其周边地区地下水电阻率测深调查。地球科学进展,26(3):544 - 544。https://doi.org/10.4236/ijg.2022.131004收稿日期:2021年9月26日收稿日期:2022年1月26日出版日期:2022年1月29日版权所有©2022 by作者和Scientific Research Publishing Inc。本作品采用知识共享署名国际许可协议(CC BY 4.0)。http://creativecommons.org/licenses/by/4.0/ Open Access C. C. Nwachukwu等。研究区中部低电阻率值区域。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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