Aquifer Delineation using Electrical Resistivity Method, a Case Study of Opolo Community in Yenagoa Local Government Area of Bayelsa State; Nigeria

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Ovuru and Eteh

Greener Journal of Science, Engineering and Technological Research

Vol. 10(1), pp. 1-8, 2021

ISSN: 2276-7835

Copyright ©2021, the copyright of this article is retained by the author(s)

https://gjournals.org/GJSETR

 

 

 

 

 

 

Aquifer Delineation using Electrical Resistivity Method, a Case Study of Opolo Community in Yenagoa Local Government Area of Bayelsa State; Nigeria

 

 

*Ovuru Cyril; Eteh Desmond Rowland

 

 

Department of Geology, Niger Delta University, Wilberforce Island, Amassoma, Bayelsa State

 

 

 

ARTICLE INFO ABSTRACT
 

Article No.: 032221026

TypeResearch

 

 

Nine vertical electrical soundings (VES) were carried out in Opolo community in Yenagoa local government area of Bayelsa State, the aim is to delineate aquifer in the area for the drilling of productive wells, using Abem Terrameter, SAS 1000. The interpreted geo-electric sections from the VES data and computer modeling curves revealed five (5) geo-electric layers. The first geo-electric layer has a resistivity value of 31Ωm with a thickness of 2.2m and a depth of 2.2m. This layer is interpreted as topsoil. The second geo-electric layer has a resistivity value of 33.87Ωm with a thickness of 1.6m and a depth of 4.0m. This layer is interpreted as clay. The third geo-electric layer has a resistivity value of 44.33Ωm with a thickness of 12.02m and a depth of 15m. This layer is interpreted as silty clay. The fourth geo-electric layer has a resistivity value of 684.2Ωm with a thickness of 16m and a depth of 17m. This layer is interpreted as fine to medium coarse sand and is aquiferous. The fifth layer has a resistivity value of 1442Ωm with a depth of 11.86m and a thickness of 7m. This layer is interpreted as coarse sand and is aquiferous. The third and the fourth layers with high resistivity values should be considered for drilling. The geo electric sections were compared with strata log of a nearby borehole in Opolo Community and these were correlatable. From this study, a benchmark of 26m depth has been recommended to represent subsurface horizon saturated with freshwater in the study area.

 

Accepted:  25/03/2021

Published: 18/05/2021

 

*Corresponding Author

Ovuru Cyril

E-mail: Cebimtakuu@ gmail.com

 

Keywords:

Resistivity; Depth; Aquifer; Delineation.

   

 

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REFERENCES

 

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Ovuru, C., Udom, G.J and Oborie, E (2010). Electrical resistivity survey for groundwater in parts of Yenagoa and Ogbia local government area, Bayelsa state, Nigeria. International journal of physical science, 5 (3), 2006-1064.

 

Ovuru, C., & Udom, G.J. (2018). Geo- Electric Characterization of Recent Hydrocarbon Contaminated Soil and Groundwater in Parts of Ogale Community, Eleme Local Government Area of Rivers State Nigeria. International Journal of Research, 5, 505-514.

 

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Cite this Article: Ovuru C; Eteh DR (2021). Aquifer Delineation using Electrical Resistivity Method, a Case Study of Opolo Community in Yenagoa Local Government Area of Bayelsa State; NigeriaGreener Journal of Science, Engineering and Technological Research, 10(1): 1-8.

Journal Name : citation_journal : Greener Journal of Science, Engineering and Technological Research 

Publication Status/Date : usp_status_date : 18/05/2021

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