Evaluation of Groundwater Potential in Bakarare Village Using Electrical Method

This study assesses the groundwater potential of Bakarare village in Minjibir Local Government Area (LGA), Kano State, Nigeria, using electrical resistivity methods. Geographically, the village lies between latitudes 12°10′0″N to 12°13′30″N and longitudes 8°32′30″E to 8°36′0″E. A total of 46 Vertical Electrical Soundings (VES) were conducted using the Schlumberger array configuration. The collected data were processed, modeled, and interpreted to delineate subsurface layers, evaluate aquifer thicknesses, and identify recharge zones. The findings revealed promising groundwater potential zones at depths ranging from 60.7 m to 72 m, with aquifer thicknesses between 56 m and 67.54 m. Laterite layers with thicknesses ranging from 1.54 m to 2.1 m (thin) and 2.25 m to 2.98 m (moderate) were identified as suitable for water infiltration and recharge to deeper aquifers. These results underscore the effectiveness of electrical resistivity methods for groundwater exploration and provide a scientific basis for addressing the village’s critical water scarcity challenges.

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Publication Details

Journal
BIMA JOURNAL OF SCIENCE AND TECHNOLOGY GOMBE
Published
2025-06-30
DOI
https://doi.org/10.64290/bima.v9i2a.1060
Primary Topic
Geophysical and Geoelectrical Methods
Type
article
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article

Evaluation of Groundwater Potential in Bakarare Village Using Electrical Method

BIMA JOURNAL OF SCIENCE AND TECHNOLOGY GOMBE
Geophysical and Geoelectrical Methods
article

Evaluation of Groundwater Potential in Bakarare Village Using Electrical Method

article en

Abstract

This study assesses the groundwater potential of Bakarare village in Minjibir Local Government Area (LGA), Kano State, Nigeria, using electrical resistivity methods. Geographically, the village lies between latitudes 12°10′0″N to 12°13′30″N and longitudes 8°32′30″E to 8°36′0″E. A total of 46 Vertical Electrical Soundings (VES) were conducted using the Schlumberger array configuration. The collected data were processed, modeled, and interpreted to delineate subsurface layers, evaluate aquifer thicknesses, and identify recharge zones. The findings revealed promising groundwater potential zones at depths ranging from 60.7 m to 72 m, with aquifer thicknesses between 56 m and 67.54 m. Laterite layers with thicknesses ranging from 1.54 m to 2.1 m (thin) and 2.25 m to 2.98 m (moderate) were identified as suitable for water infiltration and recharge to deeper aquifers. These results underscore the effectiveness of electrical resistivity methods for groundwater exploration and provide a scientific basis for addressing the village’s critical water scarcity challenges.

BIMA JOURNAL OF SCIENCE AND TECHNOLOGY GOMBE
Bayero University Kano (NG)
Openalex Percentile: Top 80%
Geophysical and Geoelectrical Methods
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