The Application of Vertical Electrical Sounding (VES) for Groundwater Exploration in Tudun Wada Kano State, Nigeria

Musa Garba Abdullahi, M. Toriman, M. B. Gasim
{"title":"The Application of Vertical Electrical Sounding (VES) for Groundwater Exploration in Tudun Wada Kano State, Nigeria","authors":"Musa Garba Abdullahi, M. Toriman, M. B. Gasim","doi":"10.4172/2329-6755.1000186","DOIUrl":null,"url":null,"abstract":"A new simple and quick geophysical method for groundwater exploration in the crystalline rocks of Tudun Wada Kano State, Nigeria has been developed. A geophysical evaluation using Electrical Resistivity method for groundwater exploration at the study area was carried out which involved the utilization of Vertical Electrical Sounding (VES) technique with schlumberger array system. The study area is located within the sedimentary rocks, igneous, and metamorphic with alluvial as common types of rocks. The data acquired from six (6) VES stations using ABEM terrameter (SAS 300) was tabulated in a table which shows the resistivity, the thicknesses and the number of layers for each VES station. The data was analyzed using computer software called IPI2win, which yield an automatic interpretation of the apparent resistivity. The VES results revealed heterogeneous nature of the subsurface geological sequence. The geological profile sequence in the study area include the topsoil, weathered layer, fractured basement and fresh basement. The value for topsoil ranges from 16 Ωm to 550 Ωm with thickness varies from 1.45 m to 6.05 m. The weathered layer resistivity ranges from 14 Ωm to 541 Ωm and thickness of 5.70 m to 33.00 m. The fractured basement ranges in value from 189 Ωm to 785 Ωm with thickness ranges from 11 m to 20 m. The fresh or bedrock basement has a resistivity of 1011 Ωm to 3006 Ωm which move down infinitely. Therefore the depth of the bedrock from the topsoil or earth’s surface ranges from 2 m to 45 m.","PeriodicalId":344421,"journal":{"name":"Journal of Geology and Geosciences","volume":"35 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"28","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Geology and Geosciences","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.4172/2329-6755.1000186","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 28

Abstract

A new simple and quick geophysical method for groundwater exploration in the crystalline rocks of Tudun Wada Kano State, Nigeria has been developed. A geophysical evaluation using Electrical Resistivity method for groundwater exploration at the study area was carried out which involved the utilization of Vertical Electrical Sounding (VES) technique with schlumberger array system. The study area is located within the sedimentary rocks, igneous, and metamorphic with alluvial as common types of rocks. The data acquired from six (6) VES stations using ABEM terrameter (SAS 300) was tabulated in a table which shows the resistivity, the thicknesses and the number of layers for each VES station. The data was analyzed using computer software called IPI2win, which yield an automatic interpretation of the apparent resistivity. The VES results revealed heterogeneous nature of the subsurface geological sequence. The geological profile sequence in the study area include the topsoil, weathered layer, fractured basement and fresh basement. The value for topsoil ranges from 16 Ωm to 550 Ωm with thickness varies from 1.45 m to 6.05 m. The weathered layer resistivity ranges from 14 Ωm to 541 Ωm and thickness of 5.70 m to 33.00 m. The fractured basement ranges in value from 189 Ωm to 785 Ωm with thickness ranges from 11 m to 20 m. The fresh or bedrock basement has a resistivity of 1011 Ωm to 3006 Ωm which move down infinitely. Therefore the depth of the bedrock from the topsoil or earth’s surface ranges from 2 m to 45 m.
查看原文
分享 分享
微信好友 朋友圈 QQ好友 复制链接
本刊更多论文
垂直电测深(VES)在尼日利亚Tudun Wada Kano州地下水勘探中的应用
提出了一种简便、快速的在尼日利亚图顿瓦达卡诺州结晶岩中勘探地下水的物探新方法。利用斯伦贝谢阵列垂直电测深(VES)技术对研究区地下水进行了电阻率法地球物理评价。研究区位于沉积岩、火成岩和变质岩中,以冲积岩为常见的岩石类型。利用ABEM测深仪(SAS 300)对6个测深站采集的数据进行了整理,得到了各测深站的电阻率、厚度和层数。这些数据是用名为IPI2win的计算机软件进行分析的,该软件可以自动解释视电阻率。探测结果揭示了地下地质层序的非均质性。研究区地质剖面序列为表土-风化层-断裂基底-新鲜基底。表层土取值范围为16 Ωm ~ 550 Ωm,厚度范围为1.45 m ~ 6.05 m。风化层电阻率范围为14 Ωm ~ 541 Ωm,厚度为5.70 ~ 33.00 m。裂缝基底值为189 Ωm ~ 785 Ωm,厚度为11 ~ 20 m。新鲜基岩基底的电阻率为1011 Ωm ~ 3006 Ωm,并无限下移。因此基岩离表层土壤或地表的深度在2米到45米之间。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 去求助
来源期刊
自引率
0.00%
发文量
0
期刊最新文献
Stratigraphic Status of the Bama Beach Ridge and the Chad Formation in the Bornu Sub-Basin, Nigeria Seismic Hazard Analysis of Pakistan Petrology and Geochemistry of Granitoids of the Northern Part of Adamawa Massif, N.E Nigeria Characterisation of Eluvial Corundum (Ruby) from Kermunda, Kalahandi District, Odisha, India Satellite Datasets and there Scaling Factor for Land Surface Temperature
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
已复制链接
已复制链接
快去分享给好友吧!
我知道了
×
扫码分享
扫码分享
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1