Authors :
Taofik Olubunmi Ewumi; Taofik Titus Ogunseye; Adekunle Kazeem Bello; Godwin Babatunde Egbeyale; Kehinde Hussein Adeleke
Volume/Issue :
Volume 10 - 2025, Issue 5 - May
Google Scholar :
https://tinyurl.com/5cvs587z
DOI :
https://doi.org/10.38124/ijisrt/25may1830
Note : A published paper may take 4-5 working days from the publication date to appear in PlumX Metrics, Semantic Scholar, and ResearchGate.
Abstract :
Electrical resistivity surveying using Wenner and Schlumberger electrode array was carried out for the assessment
of groundwater potential at the Central Mosque, University of Ibadan. Nigeria. Three Constant Spacing Traverses (CST)
and ten Vertical Electrical Sounding (VES) stations were conducted at the study area. The geoelectrical imaging from this
study revealed that the lithologies consist of lateritic topsoil, sandy clay/clayey sand/clay/weathered rock and the bedrock
(fractured and fresh). The fractured and weathered basement with relatively lower resistivity is inferred to be the aquiferous
zone and could bear productive water for groundwater supply. The results revealed the study area to be a region of relatively
high groundwater potential. It was inferred that VES 1, 2, and 8 are regions associated with high groundwater yield.
References :
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Electrical resistivity surveying using Wenner and Schlumberger electrode array was carried out for the assessment
of groundwater potential at the Central Mosque, University of Ibadan. Nigeria. Three Constant Spacing Traverses (CST)
and ten Vertical Electrical Sounding (VES) stations were conducted at the study area. The geoelectrical imaging from this
study revealed that the lithologies consist of lateritic topsoil, sandy clay/clayey sand/clay/weathered rock and the bedrock
(fractured and fresh). The fractured and weathered basement with relatively lower resistivity is inferred to be the aquiferous
zone and could bear productive water for groundwater supply. The results revealed the study area to be a region of relatively
high groundwater potential. It was inferred that VES 1, 2, and 8 are regions associated with high groundwater yield.