2006
DOI: 10.1007/s10669-006-0159-x
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Determination of groundwater potential in obiaruku and environs using surface geoelectric sounding

Abstract: The interpretation of ten resistivity curves in Obiaruku and environs indicates that the area has a great groundwater potential. Correlation of the curves with the lithologic log from a nearby borehole in Ghana quarters, reveals the lithologic succession as an extensive sandy unit between the range of 20 m and 136 m. The medium grained sand unit, which is the aquiferous zone, has a resistivity range of between 300 m and 600 m. The result of the interpreted data and the lithologic log from the borehole indicate… Show more

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Cited by 35 publications
(17 citation statements)
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“…Vertical electrical sounding (VES) is a technique which has been used in various lithological settings successfully [20][21][22]. The VES method is useful to study groundwater conditions and to evaluate the subsurface layers [23,24]. Many researchers have evaluated aquifer parameters using the resistivity method [6,9,25].…”
Section: Analysis Of Resistivity Datamentioning
confidence: 99%
“…Vertical electrical sounding (VES) is a technique which has been used in various lithological settings successfully [20][21][22]. The VES method is useful to study groundwater conditions and to evaluate the subsurface layers [23,24]. Many researchers have evaluated aquifer parameters using the resistivity method [6,9,25].…”
Section: Analysis Of Resistivity Datamentioning
confidence: 99%
“…The main objective of the investigation is to delineate the subsurface lithology and to assess the groundwater resources of the sub watershed. It's also aim to focus on the identification of fracture zone and its thickness by using VES (Vertical Electrical Sounding) method [9,10]. The exploration of buried underground resources, cannot be rely on geological information have to inevitably somehow the works of designing of these resources appear on the ground.…”
Section: Introductionmentioning
confidence: 99%
“…The VES survey technique has also been used effectively for the study of groundwater conditions, assessment of the sub-surface geoelectrical layers, thickness and depth of water bearing formation (Shankar, 1994;Lashkaripour, 2003;Oseji et al, 2006;Sahu and Sahoo 2006). The resistivity of a geological structure can vary significantly, depending on the porosity, water content and the concentration of salts in groundwater.…”
Section: Introductionmentioning
confidence: 99%