Hydrogeophysical Delineation and Hydrogeochemical Characterization of the Aquifer Systems in Umuahia-South Area, Southern Nigeria

C. Amos-Uhegbu *

Department of Physics (Geophysics),College of Natural and Applied Sciences, Michael Okpara University of Agriculture, Umudike, P.M.B 7267 Umuahia, Abia-State, Nigeria

M. U. Igboekwe

Department of Physics (Geophysics),College of Natural and Applied Sciences, Michael Okpara University of Agriculture, Umudike, P.M.B 7267 Umuahia, Abia-State, Nigeria

G. U. Chukwu

Department of Physics (Geophysics),College of Natural and Applied Sciences, Michael Okpara University of Agriculture, Umudike, P.M.B 7267 Umuahia, Abia-State, Nigeria.

K. O. Okengwu

Department of Geology, University of Port Harcourt, P.M.B 5323 Port Harcourt, Nigeria

T. K. Eke

Department of Physics/Electronics, Abia State Polytechnic, P.M.B 7166 Aba, Abia-State, Nigeria

*Author to whom correspondence should be addressed.


Abstract

In Umuahia-South Local Government Area of Abia State Nigeria, some cases of boreholes failure and groundwater discolouration have been observed. An investigation in order to determine the hydrogeological conditions of the area was carried out using geoelectrical, drill-hole and hydrogeochemical data. Using the Schlumberger electrode configuration, ten vertical electrical sounding data were acquired and the computer-aided Resist software method was used for further processing and interpretation. The interpretation of the VES data obtained from the study area shows that the vicinity of VES station 1 is likely to record failure in bore-hole exploration. A high variation in aquifer thicknesses is observed with the least as 27m at VES Station 5, and the highest 226m at VES Station 3. A new approach was used in the estimation of aquifer hydraulic parameters such as hydraulic conductivity and transmissivity. Some geoelectric sections generated from VES stations were compared with some lithologs which gave a good geological description of the study area; thereby revealing a multi-aquifer hydrogeologic system. Water samples were taken from ten boreholes for hydrogeochemical investigation which reveals the occurrence of same geochemical process; but slightly varying water quality which is associated to the multi-aquifer status of the area. The discolouration of water observed in some boreholes owes its origin from the silty-sand aquiferous units with slightly high iron content. A further analysis of the samples when plotted on Gibb’s Diagram reveals that recharge occurs through precipitation, but the local geology of the area is the source of major ion concentrations in the samples.

Keywords: Benin formation, Umuahia-South, aquifer characteristics, parameter estimation, groundwater quality, hydrogeochemical facies


How to Cite

Amos-Uhegbu, C., M. U. Igboekwe, G. U. Chukwu, K. O. Okengwu, and T. K. Eke. 2012. “Hydrogeophysical Delineation and Hydrogeochemical Characterization of the Aquifer Systems in Umuahia-South Area, Southern Nigeria”. Current Journal of Applied Science and Technology 2 (4):406-32. https://doi.org/10.9734/BJAST/2012/1645.

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