VLF-EM and VES: an application to groundwater exploration in a Precambrian basement terrain SW Nigeria

<p>In a hard rock environment with surface or near surface expression of outcrops, the use of VES only becomes difficult due to its associated problems and limitations. However, the use of VLF-EM becomes imperative in mapping basement structures relevant to groundwater development. A total of...

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Main Authors: Adebowale Obasanmi Adelusi, Michael A. Ayuk, John Stephen Kayode
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 2014-03-01
Series:Annals of Geophysics
Subjects:
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/6291
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spelling doaj-5b272489b3c5477fa3e9076faff696732020-11-24T22:08:54ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X2014-03-0157110.4401/ag-62915927VLF-EM and VES: an application to groundwater exploration in a Precambrian basement terrain SW NigeriaAdebowale Obasanmi Adelusi0Michael A. Ayuk1John Stephen Kayode2Federal University of Technology Akure, Department of Applied Geophysics, Akure,Federal University of Technology Akure, Department of Applied Geophysics, Akure,Covenant University, Department of Physics, Canaan Land, Otta,<p>In a hard rock environment with surface or near surface expression of outcrops, the use of VES only becomes difficult due to its associated problems and limitations. However, the use of VLF-EM becomes imperative in mapping basement structures relevant to groundwater development. A total of 2100 VLF-EM data plus selected VES points were covered over 7 traverses with length varying from 3000 to 4500 m. The VLF-EM result mapped basement structures relevant in groundwater development. This is further studied using VES. Results of the investigation indicate that a HKH sounding curve is obtained with a maximum of five subsurface layers comprising: the top soil, clay/sandy clay unit, the fresh basement, fractured basement and the basement bedrock. The fractured basement layer constitutes the main aquifer unit with thickness of 20-25 m. The layer resistivity and thickness ranges are 60-100 ohm-m; 40-80 ohm-m, 1600-2100 ohm-m, 250-420 ohm-m, and 2200-7500 ohm-m; and 0.3-1.2 m, 1.9-2.5 m, 16.5-22.5 m and 22-30 m for the five layers respectively. The geoelectric results compared favorably well with drilling information to above 90%. The yield of the well is 2 L/s with good recharge capability.</p>http://www.annalsofgeophysics.eu/index.php/annals/article/view/6291Electromagnetic (VLF-EM)Hard rock environmentGroundwater developmentLayer resistivityBed thickness mappingss mapping
collection DOAJ
language English
format Article
sources DOAJ
author Adebowale Obasanmi Adelusi
Michael A. Ayuk
John Stephen Kayode
spellingShingle Adebowale Obasanmi Adelusi
Michael A. Ayuk
John Stephen Kayode
VLF-EM and VES: an application to groundwater exploration in a Precambrian basement terrain SW Nigeria
Annals of Geophysics
Electromagnetic (VLF-EM)
Hard rock environment
Groundwater development
Layer resistivity
Bed thickness mappingss mapping
author_facet Adebowale Obasanmi Adelusi
Michael A. Ayuk
John Stephen Kayode
author_sort Adebowale Obasanmi Adelusi
title VLF-EM and VES: an application to groundwater exploration in a Precambrian basement terrain SW Nigeria
title_short VLF-EM and VES: an application to groundwater exploration in a Precambrian basement terrain SW Nigeria
title_full VLF-EM and VES: an application to groundwater exploration in a Precambrian basement terrain SW Nigeria
title_fullStr VLF-EM and VES: an application to groundwater exploration in a Precambrian basement terrain SW Nigeria
title_full_unstemmed VLF-EM and VES: an application to groundwater exploration in a Precambrian basement terrain SW Nigeria
title_sort vlf-em and ves: an application to groundwater exploration in a precambrian basement terrain sw nigeria
publisher Istituto Nazionale di Geofisica e Vulcanologia (INGV)
series Annals of Geophysics
issn 1593-5213
2037-416X
publishDate 2014-03-01
description <p>In a hard rock environment with surface or near surface expression of outcrops, the use of VES only becomes difficult due to its associated problems and limitations. However, the use of VLF-EM becomes imperative in mapping basement structures relevant to groundwater development. A total of 2100 VLF-EM data plus selected VES points were covered over 7 traverses with length varying from 3000 to 4500 m. The VLF-EM result mapped basement structures relevant in groundwater development. This is further studied using VES. Results of the investigation indicate that a HKH sounding curve is obtained with a maximum of five subsurface layers comprising: the top soil, clay/sandy clay unit, the fresh basement, fractured basement and the basement bedrock. The fractured basement layer constitutes the main aquifer unit with thickness of 20-25 m. The layer resistivity and thickness ranges are 60-100 ohm-m; 40-80 ohm-m, 1600-2100 ohm-m, 250-420 ohm-m, and 2200-7500 ohm-m; and 0.3-1.2 m, 1.9-2.5 m, 16.5-22.5 m and 22-30 m for the five layers respectively. The geoelectric results compared favorably well with drilling information to above 90%. The yield of the well is 2 L/s with good recharge capability.</p>
topic Electromagnetic (VLF-EM)
Hard rock environment
Groundwater development
Layer resistivity
Bed thickness mappingss mapping
url http://www.annalsofgeophysics.eu/index.php/annals/article/view/6291
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