A Hydrogeophysical Appraisals for Surficial Aquifer Potentials of Sedimentary Basin of SW Nigeria

dc.contributor.authorOke, S.A.
dc.date.accessioned2021-01-03T10:50:13Z
dc.date.available2021-01-03T10:50:13Z
dc.date.issued2019
dc.descriptionPublished Articleen_US
dc.description.abstractThis study presents the use of geoelectrical method in assessing the surficial aquifer potentials of the multi-layered sedimentary basin of South Western Nigeria. The 18 Vertical Electrical Sounding (VES) covering the sedimentary basin was conducted using the schlumberger electrode array. Methodology and data evaluation includes zoning the basin according to their geological formations and rock types. Field resistivity data were inverted into one and two dimensions with IPI2Win Software. The inversion were done to obtain both lateral and vertical layer distribution of beds in the vadose zone, depth to water levels, identification of lithological types and thicknesses and presence of aquifers. Four to six lithological layers were delineated general for the basin from the interpretation of the data inversions. Results showed that vadose sediment compositions include porous sandstones, limestones, shales and topsoils. Transverse conductance from the study correlated with the aquifer transmissivity which suggest possibility of good yield. This study has shown the importance of surface resistivity in aquifer parameters and potentials estimations.en_US
dc.identifier.issn1816-949X
dc.identifier.urihttp://hdl.handle.net/11462/2102
dc.language.isoenen_US
dc.publisherJournal of Engineering and Applied Sciencesen_US
dc.relation.ispartofseriesJournal of Engineering and Applied Sciences;14 (11): 3575-3582, 2019
dc.subjectElectrical Resistivityen_US
dc.subjectAquifer Transmissivityen_US
dc.subjectVertical Electrical Soundingen_US
dc.subjectTransverse Conductanceen_US
dc.subjectHydrogeophysicsen_US
dc.subjectLimestonesen_US
dc.titleA Hydrogeophysical Appraisals for Surficial Aquifer Potentials of Sedimentary Basin of SW Nigeriaen_US
dc.typeArticleen_US

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