Using The Electrical Resistivity Method to Investigate Soil Resistivity at Okokpon, Okada, Edo State, Nigeria
Authors
Department of Physics Federal University Otuoke, Bayelsa State (Nigeria)
Department of Physics Federal University Otuoke, Bayelsa State (Nigeria)
Department of Physics Federal University Otuoke, Bayelsa State (Nigeria)
Article Information
DOI: 10.51584/IJRIAS.2026.11070072
Subject Category: Geophysics
Volume/Issue: 11/7 | Page No: 1115-1127
Publication Timeline
Submitted: 2026-07-17
Accepted: 2026-07-22
Published: 2026-08-03
Abstract
Electrical resistivity surveying was used to characterize the shallow subsurface at the ELPS CS2 site in Okokpon, Okada, Edo State, and to assess the implications for buried metallic infrastructure. Measurements were acquired at six vertical electrical sounding (VES) stations with an ABEM SAS 1000 Terrameter, a 12 V battery, four electrodes, connecting cables, a measuring tape, and a GPS receiver. The Schlumberger array was used to inject current and measure the resulting potential difference. Apparent resistivity values were calculated and inverted to obtain layer resistivities to an investigated depth of approximately 10 m. The interpreted resistivity values ranged from 70.1 Ωm to 9708 Ωm. The lower values are consistent with clay-rich or moisture-retaining horizons, whereas the higher values indicate relatively dry lateritic, sandy, or gravelly materials. Surface and 5 m contour maps also reveal marked lateral variation, including comparatively conductive zones around ERT1, ERT3, and ERT6 and highly resistive zones around ERT4 and ERT5. Overall, the site is not dominated by highly conductive soil; therefore, the resistivity data alone do not indicate a general requirement for cathodic protection. This conclusion should, however, be verified with seasonal measurements and complementary soil-corrosivity parameters before final pipeline design.
Keywords
electrical resistivity, soil corrosivity, vertical electrical sounding, lithology, pipeline corrosion
Downloads
References
1. Dahlin, T. (2001). The development of DC resistivity imaging techniques. Computers & Geosciences, 27(9), 1019-1029. [Google Scholar] [Crossref]
2. Samouëlian, A., Cousin, I., Tabbagh, A., Bruand, A., & Richard, G. (2005). Electrical resistivity survey in soil science: A review. Soil and Tillage Research, 83(2), 173-193. [Google Scholar] [Crossref]
3. Griffiths, D. H., & Barker, R. D. (1993). Two-dimensional resistivity imaging and modeling in areas of complex geology. Journal of Applied Geophysics, 29(3-4), 211-226. [Google Scholar] [Crossref]
4. Loke, M. H. (2004). Tutorial: 2-D and 3-D electrical imaging surveys. Geotomo Software. [Google Scholar] [Crossref]
5. Reyment, R. A. (1965). Aspects of the geology of Nigeria. Ibadan University Press. [Google Scholar] [Crossref]
6. Short, K. C., & Stauble, A. J. (1967). Outline of the geology of Onitsha, Owerri and Benue provinces. Geological Survey of Nigeria, Bulletin No. 21. [Google Scholar] [Crossref]
7. Akujieze, C. N. (2004). Effects of anthropogenic activities (sand quarrying and waste disposal) on urban groundwater system and aquifer vulnerability assessment in Benin City, Edo State, Nigeria. PhD Thesis, University of Benin, Benin City, Nigeria. [Google Scholar] [Crossref]
8. Petters, S. W., & Ekweozor, C. M. (1981). Origin of Cretaceous black shales in the Benue Trough, Nigeria. Journal of Palaeogeography, Palaeoclimatology, Palaeoecology, 40, 311-319. [Google Scholar] [Crossref]
9. Onyekuru, S. O., Iwuoha, P. O., Iwuagwu, C. J., Nwozor, K. K., & Opara, K. D. (2018). Mineralogical and geochemical properties of clay deposits in parts of Southeastern Nigeria. International Journal of Physical Sciences, 13(14), 217-229. [Google Scholar] [Crossref]
10. Obrike, S. E., Osadebe, C. C., & Onyeobi, T. U. S. (2007). Mineralogical, geochemical, physical and industrial characteristics of shale from Okada area, southwestern Nigeria. Journal of Mining and Geology, 43(2), 109-116. [Google Scholar] [Crossref]
11. Obrike, S. E. (2012). Evaluation of Imo clay-shale deposit (Paleocene) from Okada, Edo State, Southwestern Nigeria, as drilling mud clay. Journal of Applied Technology of Environmental Sanitation, 1(4), 311-316. [Google Scholar] [Crossref]
12. Nwajide, C. S. (2005). A guide to geological field trips to Anambra and related basins in Southeastern Nigeria. Great AP Express Publishers Ltd. [Google Scholar] [Crossref]
13. Okoye, I. P., & Obi, C. (2011). Synthesis and characterization of Al-pillared bentonite clay minerals. Research Journal of Applied Sciences, 6, 447-450. [Google Scholar] [Crossref]
Metrics
Views & Downloads
Similar Articles
- Geophysical Investigation for Marl Exploration Using Vertical Electrical Sounding in Akpokponke Ibii Afikpo Southeast Nigeria
- Logging Data-Driven Geomechanical Parameter Estimation Using Advanced Machine Learning Techniques
- Seismic Refraction Tomography for Engineering Site Characterization in Awka, Southeastern Nigeria
- Design of a Competency Framework for BIM-Based Collaboration among Construction Professionals in Delta State
- Aeromagnetic Investigation of the Subsurface Sturctures in Parts of Niger Delta, Nigeria