The geophysical investigation for groundwater was carried out at Oda town,Akure south local government area of Ondo State.Fourteen(14)points were sounded using a Schlumberger array with AB/2 of 80 m and the resulting ...The geophysical investigation for groundwater was carried out at Oda town,Akure south local government area of Ondo State.Fourteen(14)points were sounded using a Schlumberger array with AB/2 of 80 m and the resulting geoelectric parameters were used in the estimation of the aquifer layer parameters of the subsurface.The first layer resistivity value ranges from 29 to 164Ωm and thickness ranges from 0.6 to 2.5 m.The second layer has a resistivity value ranging from 21-1361Ωm with a thickness ranging from 1.5 m to 14.6 m.The third layer resistivity value is from 68 to 297Ωm with thickness ranging from 4 m to 12.4 m.The fourth layer which is the deepest layer has a resistivity value ranging from 180 to 4364Ωm with depth ranging from 4 m to 19.5 m.The parameters interpreted from the geoelectric data were used to generate the aquifer thickness and resistivity maps,with bedrock relief which were combined to produce the groundwater potential map of the area.These maps were used to characterise the study area into low to high groundwater potential zones.The southwestern and eastern parts were identified as productive groundwater potential zones.The result was validated by taking water column depth from eight existing hand-dug wells.A significant correlation was obtained between the groundwater potential model and the well water column.The surveyed area is generally suitable for hand-dug well aside from the north-eastern part where groundwater potential is low and water volume is observed.展开更多
文摘The geophysical investigation for groundwater was carried out at Oda town,Akure south local government area of Ondo State.Fourteen(14)points were sounded using a Schlumberger array with AB/2 of 80 m and the resulting geoelectric parameters were used in the estimation of the aquifer layer parameters of the subsurface.The first layer resistivity value ranges from 29 to 164Ωm and thickness ranges from 0.6 to 2.5 m.The second layer has a resistivity value ranging from 21-1361Ωm with a thickness ranging from 1.5 m to 14.6 m.The third layer resistivity value is from 68 to 297Ωm with thickness ranging from 4 m to 12.4 m.The fourth layer which is the deepest layer has a resistivity value ranging from 180 to 4364Ωm with depth ranging from 4 m to 19.5 m.The parameters interpreted from the geoelectric data were used to generate the aquifer thickness and resistivity maps,with bedrock relief which were combined to produce the groundwater potential map of the area.These maps were used to characterise the study area into low to high groundwater potential zones.The southwestern and eastern parts were identified as productive groundwater potential zones.The result was validated by taking water column depth from eight existing hand-dug wells.A significant correlation was obtained between the groundwater potential model and the well water column.The surveyed area is generally suitable for hand-dug well aside from the north-eastern part where groundwater potential is low and water volume is observed.
