2010
DOI: 10.4314/swj.v4i2.51845
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Assessment of the aquifers in some selected villages in Chikun local government area, Kaduna state, Nigeria.

Abstract: The Vertical Electrical Sounding (VES) technique was used to investigate the sub-surface layering in some selected villages in Chikun LGA of Kaduna State with the aim of determining the configuration of the aquifer underlying the region. The result of the interpreted VES data suggests that the area is underlain by three to five layers. The geologic sections derived from the analyzed geoelectric section suggest that the alluvial deposits of sand, silt and sandy clay as well as the weathered and fractured baseme… Show more

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Cited by 11 publications
(12 citation statements)
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“…Also, the presence of laterites and quartzites in the study area beneath the clayey topsoil which extends beyond 2.5m are filter factors which could reduce the degree of aquifer vulnerability from the surface contamination. Figures 6 and 7 show the resistivity and thickness maps of the weathered layer respectively which closely agrees with the work of [11]. The deeper aquifer is found mostly in southwest (VES points D1, D2, E1, E2 and E3), and some parts of north (VES points A2, B2 and B3), and east (VES points B6 and C6), of the map which denoted by deep blue colour.…”
Section: Resultssupporting
confidence: 83%
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“…Also, the presence of laterites and quartzites in the study area beneath the clayey topsoil which extends beyond 2.5m are filter factors which could reduce the degree of aquifer vulnerability from the surface contamination. Figures 6 and 7 show the resistivity and thickness maps of the weathered layer respectively which closely agrees with the work of [11]. The deeper aquifer is found mostly in southwest (VES points D1, D2, E1, E2 and E3), and some parts of north (VES points A2, B2 and B3), and east (VES points B6 and C6), of the map which denoted by deep blue colour.…”
Section: Resultssupporting
confidence: 83%
“…This information is vital in evaluating the aquifer protective capacity which is the interest of this research work. [11], held that the sections where the aquifer appears thickest with an averagely low resistivity value are the best areas for the exploitation of underground water or siting boreholes. With the aquifer thickness ranging from about 11.0 m to 42.0 m, the study area appears largely good enough for siting of boreholes except some parts of south-south (VES points C5 and D5), aquifer thickness is relatively low.…”
Section: Resultsmentioning
confidence: 99%
“…In addition, a remarkable study noted that to ensure adequate water security and sustainability, there is a need to install multiple boreholes in geophysical identi ed groundwater promising zones where the aquifer occurs in deeper zones and fractured [3]. This is because most remarkable studies conducted in the complex basement rock noted that the weathered/fractured units are largely responsible for the regional groundwater-bearing capacity [3,11,17,18]These situations therefore make this type of investigation a prima facie for the precise location of fractured zones for productive borehole sites. This study therefore evaluated the VES station parameters for groundwater development in a study area that falls within the Basement Complex terrain of Kaduna State, Nigeria.…”
Section: Introductionmentioning
confidence: 99%
“…To overcome this disadvantage Exam Hall seating arrangement System was developed. Details in modules such as Students Details, Examination Timing Details, and Hall Details with the proper descriptions will be monitored (Ibrahim, Yaro and Adebola, 2017).…”
Section: Introductionmentioning
confidence: 99%