INTEGRATED GEO-ELECTRICAL AND ELECTROMAGNETIC INVESTIGATION OF GRID PART OF FELELE CAMPUS, FEDERAL UNIVERSITY LOKOJA, NIGERIA

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INTEGRATED GEO-ELECTRICAL AND ELECTROMAGNETIC INVESTIGATION OF GRID PART OF FELELE CAMPUS, FEDERAL UNIVERSITY LOKOJA, NIGERIA

Isaac O. Agbane1*, Ogbadu R. Omeje2, Dayo J. Olutokun3 and Esther A. Yahaya3

1Department of Geology, Federal University Lokoja, Nigeria

2Department of Geology, Kogi State University, Anyigba, Nigeria

3Department of Physics, Kogi State University, Anyigba, Nigeria

*Email:agbaneisaac@gmail.com

ABSTRACT

Geophysical investigation involving the use of vertical electrical sounding (VES) on  grid-A part of Felele campus, Federal University Lokoja, Nigeria with  objectives  to delineating depth to fresh basement, fractured zones in the study area for potential groundwater exploration within the crystalline basement rocks. The area is underlain by the Crystalline Basement rocks composed of granite gneiss, quartzite and intrusions.  PASI Terrameter was used and the symmetrical Schlumberger configuration adopted. A total of four (4) Vertical Electrical Sounding (VES) stations were established. Preliminary input data from the field were inputed into the WINRESIST software to generate real resistivities and depths to geoelectric layers. Three (3) geoelectric layers were interpreted, the first layer is the top soil made up of resistivity values ranging from 141 Ωm – 486.1 Ωm and depth to weathered basement of 1.2-2.5m. It is inferred that this layer does not consist of the same material across the entire length of the profile. The second layer is made up of resistivity values ranging from 37.9Ωm to 85.6Ωm and depth to fresh basement of 11.2 – 16.1m. Its inferred to composed mostly of fractured and unconsolidated rocks, loose gravel, sandy soil and clayey. The resistivity value within this layer indicates that is it good for groundwater exploration and the third layer has the highest resistivity values ranging from 821.2 Ωm – 2695Ωm with an infinite depth. It’s entirely composed of fresh basement rock which is possibly of the gneissic suite.

Keywords: Basement rocks, Fractures, Geoelctric layers, ground water, lokoja, schlumberger