The Use of Vertical Electrical Sounding (VES) for Subsurface Geophysical Investigation around Bomo Area, Kaduna State, Nigeria

dc.contributor.authorJatau, B.S.
dc.contributor.authorPatrick, N.O.
dc.contributor.authorBaba, Adama Oleka
dc.contributor.authorFadele, S.I.
dc.date.accessioned2023-12-14T07:19:16Z
dc.date.available2023-12-14T07:19:16Z
dc.date.issued2013-01-01
dc.description.abstractElectrical resistivity investigation was carried out around Bomo area, Zaria, Kaduna state, in order to study the subsurface geologic layer with a view of determining the depth to the bedrock and thickness of the geologic layers. Vertical Electrical Sounding (VES) using Schlumberger array was carried out at fifteen (15) VES stations. ABEM terrameter (SAS 300) was used for the data acquisition. The field data obtained have been analysed using computer software (IPI2win) which gives an automatic interpretation of the apparent resistivity. The VES results revealed heterogeneous nature of the subsurface geological sequence. The geologic sequence beneath the study area is composed of hard pan top soil (clayey and sandy-lateritic), weathered layer, partly weathered or fractured basement and fresh basement. The resistivity value for the topsoil layer varies from 40Ωm to 450Ωm with thickness ranging from 1.25 to 7.5 m. The weathered basement has resistivity values ranging from 50Ωm to 593Ωm and thickness of between 1.37 to 20.1 m. The fractured basement has resistivity values ranging from 218Ωm to 520Ωm and thickness of between 12.9 to 26.3 m. The fresh basement (bedrock) has resistivity values ranging from 1215Ωm to 2150Ωm with infinite depth. However, the depth from the earth’s surface to the bedrock surface varies between 2.63 to 34.99 m. The study further stressed the importance of the findings in civil engineering structures and groundwater prospecting.en_US
dc.identifier.citation[1] DANLADI, G.G. 1985. “Appraisal of Hydrological Investigation in Shallow Basement Area of Zaria”. Unpublished M.Sc. Thesis, Department of Geology, Ahmadu Bello University, Zaria. [2] FAROUQ, A.U. 2001. “Geoelectric Investigation of the groundwater potential in the Institute for Agricultural Research farm”. Unpublished M.Sc. Thesis, Department of Physics, Ahmadu Bello University, Zaria. [3] HAROLD, E.D. 1970. “Arid Lands in Transition”. The Hornshafer Company Division of G.D.W. King Printing Co., U.S.A. [4] KLINKENBERA, K. 1970. “Soil of Zaria Area, In Zaria and its Region” (ed. M. J. Mortimore), Department of Geography, Occasional Paper No. 4, Ahmadu Bello University, Zaria, P. 223 – 238. [5] McCURRY, P. 1970. “The Geology of Zaria Sheet 21”. Unpublished M.Sc. Thesis, Department of Geology, Ahmadu Bello University, Zaria. [6] OYAWOYE, P. O. 1964. “Geology of Nigerian Basement Complex”. Journal of Mining and Geology, Vol.1, P. 110-121 [7] SAMINU, O. 1999. “Geophysical Investigation of Federal College of Education, Zaria”. Unpublished M.Sc. Thesis, Department of Physics, Ahmadu Bello University, Zaria. [8] WRIGHT, J. B. and McCURRY, P. (1970). “The geology of Nigeria Sheet 102 SW, Zaria and its regions. Edited by M. J. Mortimore. Department of Geography, Occasional paper, No. 4, Ahmadu Bello University, Zaria.en_US
dc.identifier.urihttps://keffi.nsuk.edu.ng/handle/20.500.14448/5712
dc.language.isoenen_US
dc.publisherDepartment of Geology and Mining, Nasarawa State University Keffien_US
dc.subjectElectrical Resistivity, CERT (CT), Vertical Electrical sounding (VES), Top soil (TP), Weathered basement (WB), Partly Weathered Basement (PWB) and Fresh Basement (FB).en_US
dc.titleThe Use of Vertical Electrical Sounding (VES) for Subsurface Geophysical Investigation around Bomo Area, Kaduna State, Nigeriaen_US
dc.typeArticleen_US

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