Application of vertical electrical sounding (VES) for groundwater exploration in Onitsha and environs, Nigeria

Surface geo-electrical survey using vertical electrical sounding (VES) method has been carried out in Onitsha and environs in southwestern part of Anambra state in order to determine the aquifer characteristics and groundwater potential of the area. Eleven vertical electrical soundings were carried out within the area of study using schlumberger array configuration. The interpretation of the vertical electrical sounding (VES) data revealed three to five geoelectric units with depth to the aquiferous layers ranging from 21 to 78m and resistivity of the saturated layers varying between 20 and 5600 ohm-m. Aquifer characteristics such as transmissivity and hydraulic conductivity calculated from interpretated VES result ranged from 2.55m2/day to 29.01m2/day and 0.03m/day to 1.37m/day respectively. This result shows that the water saturated sandstone units of the study area is hydrological good and capable of producing optimum groundwater yield. Furthermore, borehole could be drilled at depth between 40 and 110m in the area for sustainable water supply and hydrochemical study carried out to determine the water quality for domestics and municipal purposes.

[1]  E. Chukwuma,et al.  Determination of Aquifer Characteristics from Geo-electrical Sounding data in parts of Anambra State, Nigeria , 2015 .

[2]  E. Anakwuba,et al.  Hydrogeophysical assessment of some parts of Anambra basin, Nigeria , 2014 .

[3]  B. Egboka,et al.  Evaluation of the aquifer characteristic of Nanka Sands using hydrogeological method in combination with Vertical Electrical Sounding (VES) , 2010 .

[4]  Filippos Vallianatos,et al.  Estimation of aquifer hydraulic parameters from surficial geophysical methods: A case study of Keritis Basin in Chania (Crete - Greece) , 2007 .

[5]  A. Ekwe,et al.  Estimation of aquifer hydraulic characteristics from electrical sounding data: the case of middle Imo River basin aquifers, south- eastern Nigeria. , 2006 .

[6]  K. Singh,et al.  Nonlinear estimation of aquifer parameters from surficial resistivity measurements , 2005 .

[7]  O. Falode,et al.  Hydrocarbon Potential and Thermal Maturity of Nkporo Shale from Lower Benue Trough, Nigeria , 2005 .

[8]  C. S. Nwajide,et al.  Evolution of the Enugu Cuesta: a tectonically driven erosional process , 2001 .

[9]  Fletcher G. Driscoll,et al.  Groundwater and Wells , 1986 .

[10]  J. B. Wright South Atlantic continental drift and the Benue Trough , 1968 .

[11]  Chukwudi C. Ezeh,et al.  Geoelectrical studies for estimating aquifer hydraulic properties in Enugu State, Nigeria , 2011 .

[12]  O. Ujuanbi,et al.  Hydrogeophysical investigation of groundwater potential in Emu kingdom, Ndokwa land of Delta State, Nigeria , 2009 .

[13]  E. Emenike Geographysical Exploration For Groundwater In A Sedimentary Environment: A Case Study From Nanka Formation In Anambra Basin, Southeastern Nigeria , 2001 .

[14]  K. Onuoha,et al.  Aquifer Transmissivity from Electrical Sounding Data: The case of Ajali Sandstone Aquifers, Southeast of Enugu, Nigeria , 1988 .

[15]  D. C. Singhal,et al.  Estimation of aquifer transmissivity from Dar-Zarrouk parameters in porous media , 1981 .

[16]  R. Reyment Aspects of the geology of Nigeria : the stratigraphy of the Cretaceous and Cenozoic deposits , 1965 .