Please use this identifier to cite or link to this item: http://localhost:8080/xmlui/handle/123456789/820
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dc.contributor.authorBadmus, B. S-
dc.contributor.authorAyolabi, E. A-
dc.contributor.authorOlowofela, J. A-
dc.contributor.authorAdisa, S. A-
dc.contributor.authorOyekunle, T. O-
dc.date.accessioned2022-07-21T09:39:31Z-
dc.date.available2022-07-21T09:39:31Z-
dc.date.issued2005-
dc.identifier.citationBadmus, B. S , Ayolabi, E. A , Olowofela, J. A , Adisa, S. A and Oyekunle, T. O (2005). Current variation in electrical resistivity probing using Wenner and Schlumberger arrays in a basement terrain. JOURNAL OF GEOPHYSICS AND ENGINEERING. 2 (2005) 118–125en_US
dc.identifier.urihttp://localhost:8080/xmlui/handle/123456789/820-
dc.description.abstractSchlumberger and Wenner vertical electrical soundings (VES) were carried out at five locations each within the campus of University of Agriculture, Abeokuta, Nigeria, with the aim of imaging the subsurface using different current values varying from 0.2 A to 20.0 A at each location as it appears on an ABEM SAS300B terrameter. The results of the interpretation for both electrode arrangements revealed six geo-electric layers: topsoil, sandy clay, clayey sand, sandstone, shale/clay and fresh basement. The work revealed that a current range of 0.2–1.0 A is ideal for both Schlumberger and Wenner arrays in a basement terrain.en_US
dc.language.isoenen_US
dc.publisherNANJING INSTITUTE OF GEOPHYSICAL PROSPECTING AND INSTITUTE OF PHYSICS PUBLISHINGen_US
dc.relation.ispartofseries2;-
dc.subjectGeo-electrical resistivityen_US
dc.subjectcurrent variationen_US
dc.subjectgeo-electric layersen_US
dc.subjectSchlumbergeren_US
dc.subjectWenner arraysen_US
dc.subjectcurve typesen_US
dc.titleCurrent variation in electrical resistivity probing using Wenner and Schlumberger arrays in a basement terrainen_US
dc.typeArticleen_US
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