Characterization of Subsurface Lithology and Aquifer Parameters Using Vertical Electrical Sounding (VES) for Groundwater Development in Igbo-Imabana, Southern Nigeria

Authors

  • Philip Obasi Department of Geology, Faculty of Science, Ebonyi State University, Abakaliki, Nigeria
  • Awara Ekinya Department of Geology, Faculty of Science, Ebonyi State University, Abakaliki, Nigeria
  • Chibuike Akpa Department of Geology, Faculty of Science, Ebonyi State University, Abakaliki, Nigeria
  • Emmanuel Edene Department of Geology, Faculty of Science, Ebonyi State University, Abakaliki, Nigeria

DOI:

https://doi.org/10.30564/agger.v4i3.4939

Abstract

Vertical Electrical Soundings (VES) using Schlumberger array was carried out at fifteen (15) different points to evaluate aquifer characteristics within Igbo-Imabana, Abi L.G.A of Cross River State. Resistivity meter and its accessories were used for data acquisition. The maximum current and potential electrode distance were 400 m and 20 m respectively. The field data were interpreted using Interpex software and three to five geo-electric layers encountered within the study area. The dominant curve type was H followed by K. From the result, geo-electric layers delineated were sandstone, clay, saturated sandstone, sandy shale, clayey shale, and shale with average apparent resistivity values of 2249.94 Ωm, 2.86 Ωm, 365.28 Ωm, 222.69 Ωm, 14.60 Ωm and 59.02 Ωm respectively. The top geoelectric layer was dominantly lateritic topsoil, with variation in degrees of compaction and having an average resistivity of 876.33 Ωm with depth and thickness generally less than 5 m. The calculated aquifer parameters hydraulic conductivity (Kc), transmissivity, longitudinal conductance, and transverse resistance from the VES results show ranges values; 3.86×10–4  to 4.69×10–2 m/day, 2.95×10–3 to 2.82 m2 /day, 2.95×10–3 to 2.81 Ωm and 484.33 to 19444.83 Ω2 m respectively. The aquifer thickness and depth values range from 3.60 m to 68.05 m and 5.20 m to 76 m respectively. The study reviewed that the area is made of heterolithic/heterogenou lithofacies, confined aquifer(s), shallow and deep aquifer. Also, from the models and aquifer parameters, the area is characterized by semipervious materials. This integrally explains why the area have have low transmissivity and majority of boreholes drilled in the area failed.

Keywords:

Groundwater; Aquifer parameters; Vertical electrical sounding (VES); Igbo-Imabana

References

[1] Obasi, P.N., Eyankware, M.O., Akudinobi, B.E.B., 2021. Characterization and evaluation of the effects of mine discharges on surface water resources for irrigation: a case study of the Enyigba Mining District, Southeast Nigeria. Applied Water Science. 11, 112. DOI: https://doi.org/10.1007/s13201-021-01400-w

[2] Igwe, O., Una, C.O., Abu, E., et al., 2017. Environmental risk assessment of lead–zinc mining: a case study of Adudu metallogenic province, middle Benue Trough, Nigeria. Environmental Monitoring Assess-ment. 189(10), 492.

[3] Obiora, S.C., Chukwu, A., Toteu, S.F., et al., 2018. Contamination of the potable water supply sources in the lead–zinc mining communities of Enyigba, Southeastern Nigeria. Mine Water & the Environment. DOI: https://doi.org/10.1007/s10230-018-0550-0

[4] Laxman, K.D., Ratnakar, D., Sakram, G., et al., 2021. Hydrochemical appraisal of groundwater quality for drinking and agricultural utility in a granitic terrain of Maheshwaram area of Ranga Reddy district, Telnagana State, India. Hydro Research. DOI: https://doi.org/10.1016/j.hydres.2021.02.002

[5] Azadeh, G., Mehrdad, C., Soheil, S., et al., 2020. Hydrogeochemical characteristics, temporal, and spatial variations for evaluation of groundwater quality of Hamedan–Bahar Plain as a major agricultural region, West of Iran. Environmental Earth Sciences. 79, 428. DOI: https://doi.org/10.1007/s12665-020-09177-y

[6] Bouderbal, A., 2017. Assessment of water quality index for the groundwater in the upper Chelif plain, Algeria. Journal of Geological Society India. 90, 347. DOI: https://doi.org/10.1007/s12594-017-0723-7

[7] Eyankware, M.O., Obasi, P.N., OmoIrabor, O.O., et al., 2020. Hydrochemical characterization of abandoned quarry and mine water for domestic and irrigation uses in Abakaliki, southeast Nigeria. Modeling Earth Systems and Environment. DOI: https://doi.org/10.1007/s40808-020-00827-5

[8] Obianwu, V.I., Atan, O.E., Okiwelu, A.A., 2015. Determination of Aquifer Position Using Electric Geophysical Method. Applied Physics Research. 7, 2.

[9] Ebong, G.A., ETUK, H.S., Johnson, A.S., 2007. Heavy metal Accumulation by Talinum Triangulare grown on Waste Dumpsite in Uyo Metropolis, Akwa Ibom state, Nigeria. Journal of Applied Sciences. 7(10), 1404-1409.

[10] Alile, O.M, Ujuanbi, O., Evbuomwan, I.A., 2011. Geoelectric Investigation of Groundwater in Obaretin- Iyanornon Locality, Edo State, Nigeria. Journal of Geology and Mining Research. 3(1), 13-20.

[11] Obasi, P.N., Ani, C.C., Akakuru, O.C., et al., 2020. Determination of Aquifer Depth Using Vertical Electrical Sounding in Ihechiowa Area, Arochukwu Southeast Nigeria. EBSU Science Journal. 1(1), 111-126.

[12] Riwayat, A.I., Nazri, M.A.A., Abidin, M.H.Z., 2018. Application of Electrical Resistivity Method (ERM) in Groundwater Exploration. Journal of Physics Conference. Series 995. DOI: https://doi.org/10.1088/1742-6596/995/1/012094

[13] Okwueze, E.E., 1996. Preliminary Findings of the Groundwater Resource Potentials from a Regional Geo-electric Survey of the Obudu Basement area. Global Journal of Pure and Applied Sciences. 2(2), 201-211.

[14] Keary, P., Brooks, M., 1991. An Introduction to geophysical Exploration. 2nd ed. London; Cambridge University Press. New York. pp. 254.

[15] Lowrie, W., 2007. Fundamentals of Geophysics; 2nd ed. Cambridge University Press. New York. pp. 384.

[16] Raghunath, H.M., 2007. Groundwater; 3rd ed. New Age International Pvt Limited publishers. pp. 500.

[17] Tammaneni, K.R., Hanuman, D.S., Malisethy, J.G., 2006. Site investigations for the identification of a groundwater source for Sullurupeta, Andrha Pradesh, India, IAEG Publication, No. 36.

[18] Batayneh, A.T., 2009. A hydrogeophysical model of the relationship between geoelectric and hydraulic parameters, Central Jordan. Journal of Water Resource and Protection. 1(6), 400-407.

[19] Batayneh, A.T., Elawadi, E.A., Al-Arifi, N.S., 2010. Use of geoelectrical technique for detecting subsurface fresh and saline water: A case study of the eastern Gulf of Aqaba coastal aquifer. Journal of Coastal Research. 26(6), 1079-1084.

[20] Atakpo, E.A., Akpoborie, A.I., Okolie, E.C., 2008. Geoelectric mapping of Amukpe area of Delta State, Nigeria. Nigerian Journal of Basic & Applied Sciences. 7, 73-82.

[21] Okolie, E.C., 2010. Geoelectric investigation of treasured formation strata and groundwater potential in Ogume, Delta State, Nigeria. International Journal of Physical Sciences. 6(5), 1152-1160.

[22] Okolie, E.C., Egbai, J.C., Oseji, J.O., 2008. Comparative investigation of formation strata and groundwater distributions in Orerokpe and Ovu using Schlumberger Array, Nigeria. Journal of Science Environment. 7, 91-98.

[23] Anomohanran, O., 2011. Determination of groundwater potential in Asaba, Nigeria using surface geoelectric sounding. International Journal of the Physical Sciences. 6(33), 7651-7656.

[24] Arong, T.O., Avwenagha, E., 2013. Evaluation of ground water resource in Akamkpa area, Cross river state, Nigeria. Advances in Applied Science Research. 4(5), 10-24.

[25] Iserhien-Emekeme, R.E., 2014. Electrical Resistivity Survey for Predicting Aquifer at Onicha-Ugbo, Delta State, Nigeria. Journal of Applied Mathematics and Physics. 2, 520-527.

[26] Reyment, R.A., 1965. Aspect of Geology of Nigeria. Ibadan University press. pp. 145.

[27] Nwajide, C.S., 2013. Geology of Nigeria’s Sedimentary Basin. CSS Bookshops Ltd Lagos. pp. 56-98.

[28] Eseme, E., Agyingi, C.M., Foba-Tendo, J., 2002. Geochemistry and genesis of brime emanation fromcretaceous strata of the Mamfe Basin, Cameroun. Journal of African Earth Sciences. 35, 467-476.

[29] Burke, K.C., Dessauvagie, R.F., Whiteman, A.W., 1972. Geological History of the Benue Valley and Adjacent Areas. African Geology, University of Ibadan Press. 187-206.

[30] Nweke, O.M., Okogbue, C.O., 2021. Mechanical and performance-related properties of bitumen-beneficiated indurated shale aggregates for use in road construction in southeastern Nigeria. Bulletin of Engineering Geology and the Environment. 80, 9141-9156. DOI: https://doi.org/10.1007/s10064-021-02379-z

[31] Kogbe, C.A., 1989. The cretaceous and paleogene sediments of southern Nigeria. In Kogbe, C.A. (ed) Geology of Nigeria. 2nd Edition.Rock View (Nig) Limited, Jos. 325-334.

[32] Benkhelil, J., 1987. Cretaceous deformation, magmatism and metamorphism in the lower Benue Trough, Nigeria. Geological Journal. 22, 467-493.

[33] Petters, S.W., 1978. Mid-cretaceous paleoenvironments and biostratigraphy of the Benue trough, Nigeria. Bulletin Geological Society of America. 151-155.

[34] Chukwu, A., Obiora, S.C., 2018. Geochemical constraints on the petrogenesis of the pyroclastic rocks in Abakaliki basin (Lower Benue Rift), Southeastern Nigeria, Journal of African Earth Sciences. 141, 207-220.

[35] Nigeria Geological Survey Agency (NGSA), 2006. Geological and mineral resources map of Cross River State, Nigeria.

[36] Odigi, M.I., Amajor, L.C., 2009. Geochemical characterization of cretaceous sandstones from the southern Benue Trough, Nigeria. Chinese Journal of Geochemistry. 28, 044-054.

[37] Akpan, E.A., Ebong, D.E., Chimezie, N.E., 2015. Exploratory assessment of groundwater vulnerability to pollution in Abi, southeastern Nigeria, using geophysical and geological techniques. Environmental Monitoring & Assessment. 187, 156.

[38] Loke, M.H., Barker, R.D., 1996. Practical Techniques for 3D Resistivity surveys and data Inversion. Geophysics Prospect. 44, 499-523.

[39] Todd, D.K., 2004. Groundwater Hydrology, 2nd Edition, John Wiley & Sons, New York, pp. 897.

[40] Singh, K.P., 2005. Non-linear Estimation of Aquifer Parameters from Surficial Resistivity Measurements: Hydrogeology and Earth system Sciences Discussions (HESSD). 2, 919-938.

[41] Corriols, M., Dahlin, T., 2007. Geophysical Characterization of the Leon-Chinandega Aquifer. Hydrogeology Journal. 16(2), 355.

[42] Soupios, P.M., Kouli, M., Vallianatos, F., et al., 2006. Hydraulic parameters from surface geophysical methods: Keritis basin in chania-crete.

[43] Kelly, W.E., 1977. Geoelectrical sounding for estimating aquifer hydraulic conductivity. Groundwater.50(6), 420-425.

[44] Mazac, O., Cislerova, M., Vogel, T., 1988. Application of geophysical methods in describing spatial variability of saturated hydraulic conductivity in the zone of aeration. Journal of Hydrology. 103, 117-126.

[45] Huntley, D., 1986. Relations between permeability and electrical resistivity in granular aquifers. Groundwater. 24(4), 466-474.

[46] Ekwe, A.C., Onu, N.N., Onuoha, K.M., 2006. Estimation of Aquifer Hydraulic Characteristics from Electrical Soundings data, The case of Middle Imo River basin aquifer, Southeastern Nig. Journal of Spartial Hydrogeology. 6(2), 121-132.

[47] Niwas, S., Singhal, D.C., 1981. Estimation of aquifer transmissivity from Dar Zarrouk parameters in porous media. Hydrology. 50, 393-399.

[48] Telford, W.M., Geldart, L.P., Sheriff, R.E., 1998. Applied geophysics 2nd ed; Cambridge University Press, New York. pp. 770.

[49] Odoh, B.I., 2010. Surface-outcrop characterization for fracture flow of groundwater: case study of ABakaliki Basin, Ebonyi State, Nigeria. International Archive of Applied Sciences & Technology. 1(1), 45-53.

[50] Edet, A.E., Nganje, T.N., Ukpong, A.J., et al., 2011. Groundwater chemistry and quality of Nigeria: A Status Review. African Journal of Environmental Science and Technology. 5(13), 1152-1169. DOI: https://doi.org/10.5897/AJESTX11.011

[51] Akpan, A.E., Ugbaja, A.N., George, N.J., 2013. Integrated Geophysical, Geochemical and hydrogeological investigation of shallow ground water resources in parts of the Ikom-Mamfe Embayment and the adjourning in Cross River State, Nigeria. Environmental Earth Sciences. DOI: https://doi.org/10.1007/s12665-013-2232-3

[52] Bear, J., 1972. Dynamics of Fluids in Porous Media. Dover publication, Mineola, New York.

[53] Frohlich, R.K., Parke, C.D., 1989. The Electrical Resistivity of the Vadose Zone Field Study. Groundwater. 25, 525-530.

[54] Iduma, R.E.O., Abam, T.K.S., Uko, E.D., 2016. Dar Zarrouk Parameter as a Tool for Evaluation of Well Locations in Afikpo and Ohaozara, Southeastern Nigeria. Journal of Water Resource and Protection. 8, 505-521.

[55] Krasny, J., 1993. Classification of transmissivity magnitude and variation. Groundwater. Classification of Transmissivity Magnitude and Variation. 31, 230-236.

[56] Gheorghe, A., 1978. Processing and Synthesis of Hydrogeological Data. Abacus Press, Tumbridge wells, Kent.

[57] Henriet, J., 1976. Direct applications of the dar zarrouk parameters in groundwater surveys. Geophys Prospect. 24(2), 344-353.

[58] Oladapo, M.I., Mohammed, M.Z., Adeoye, O.O., et al., 2004. Geoelectric investigation of the Ondo State Housing Corporation Estate Ijapo Akure, southwestern Nigeria. Journal of Mining and Geology. 40(1), 41-48.

[59] Oladapo, M.I., Akintorinwa, O.J., 2007. Hydrogeophysical study of Ogbese, southwestern. Niger Global Journal of Pure and Applied Science. 13(1), 55-56.

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How to Cite

Obasi, P., Ekinya, A., Akpa, C., & Edene, E. (2022). Characterization of Subsurface Lithology and Aquifer Parameters Using Vertical Electrical Sounding (VES) for Groundwater Development in Igbo-Imabana, Southern Nigeria. Advances in Geological and Geotechnical Engineering Research, 4(3), 12–31. https://doi.org/10.30564/agger.v4i3.4939

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