Geo-Electrical Exploration for Groundwater in Eiyenkorin, Ajelanwa and Owa-Otun Communities in Kwara State, Nigeria

Schlumberger Vertical Electrical Soundings (VES) for groundwater exploration in Eiyenkorin, Ajelanwa and Owa-Otun communities in the Basement Complex terrain of the southwestern Nigeria were carried out with a view to establishing the different subsurface geoelectric layers and the aquifer units. Data were collected from 4, 5 and 15 VES stations at Ajelanwa, Owa-Otun and Eiyenkorin communities respectively. From the quantitative interpretations of the data collected, using the usual method of curve matching with the Orellana-Mooney Master curves and 1-D forward modeling with WinResist 1.0 version software, between four and five lithologic units were identified in these Communities. These include: the topsoil, the lateritic layer, the weathered layer, the partly weathered/fractured basement and the fresh basement. The weathered layer and the partly weathered/fractured basement constitute the main aquifer units. The depth to bedrock at the chosen VES locations vary from 3.7 to 23.8 m at Eiyenkorin, 6 to 30 m at Ajelanwa, and 7 to 13 m at Owa Otun communities. Some lobes or areas of low resistivity which constitute the prospective zones for water exploration in these areas have been delineated.

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Publication Details

Journal
Zenodo (CERN European Organization for Nuclear Research)
Published
2024-12-30
DOI
https://doi.org/10.5281/zenodo.14565424
Primary Topic
Geophysical and Geoelectrical Methods
Type
article
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article

Geo-Electrical Exploration for Groundwater in Eiyenkorin, Ajelanwa and Owa-Otun Communities in Kwara State, Nigeria

Zenodo (CERN European Organization for Nuclear Research)
Geophysical and Geoelectrical Methods
article

Geo-Electrical Exploration for Groundwater in Eiyenkorin, Ajelanwa and Owa-Otun Communities in Kwara State, Nigeria

article en

Abstract

Schlumberger Vertical Electrical Soundings (VES) for groundwater exploration in Eiyenkorin, Ajelanwa and Owa-Otun communities in the Basement Complex terrain of the southwestern Nigeria were carried out with a view to establishing the different subsurface geoelectric layers and the aquifer units. Data were collected from 4, 5 and 15 VES stations at Ajelanwa, Owa-Otun and Eiyenkorin communities respectively. From the quantitative interpretations of the data collected, using the usual method of curve matching with the Orellana-Mooney Master curves and 1-D forward modeling with WinResist 1.0 version software, between four and five lithologic units were identified in these Communities. These include: the topsoil, the lateritic layer, the weathered layer, the partly weathered/fractured basement and the fresh basement. The weathered layer and the partly weathered/fractured basement constitute the main aquifer units. The depth to bedrock at the chosen VES locations vary from 3.7 to 23.8 m at Eiyenkorin, 6 to 30 m at Ajelanwa, and 7 to 13 m at Owa Otun communities. Some lobes or areas of low resistivity which constitute the prospective zones for water exploration in these areas have been delineated.

Zenodo (CERN European Organization for Nuclear Research)
University of Ilorin (NG)
Clean water and sanitation
Openalex Percentile: Top 58%
Geophysical and Geoelectrical Methods
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