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...
Main Authors: | , , |
---|---|
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 |
id |
doaj-5b272489b3c5477fa3e9076faff69673 |
---|---|
record_format |
Article |
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 |
work_keys_str_mv |
AT adebowaleobasanmiadelusi vlfemandvesanapplicationtogroundwaterexplorationinaprecambrianbasementterrainswnigeria AT michaelaayuk vlfemandvesanapplicationtogroundwaterexplorationinaprecambrianbasementterrainswnigeria AT johnstephenkayode vlfemandvesanapplicationtogroundwaterexplorationinaprecambrianbasementterrainswnigeria |
_version_ |
1725814008579096576 |