Abstract

Hydraulic and layer parameters of groundwater aquifer have been evaluated in parts of Buruku and Gboko local government area councils, for the primary purpose of assessing quality and potential of groundwater in the areas. A total of 18 Vertical Electrical Sounding (VES) stations were occupied along traverse lines using the Schlumberger electrode configuration. The results revealed a characteristic QQA, QHH and QH type curves, with 6 - 7 geoelectric subsurface layers. The geoelectric layers are dominantly sandy with intercalations of shale at shallow depths in most stations. The aquiferous layers were delineated at the fourth and fifth geoelectric layers with average aquifer resistivity and depth of 420.56 Ω·m and 69.1 m, respectively. Groundwater flow is generally from the northeast to the southwest in line with the tectonics of the Benue trough. Two potential groundwater zones were delineated. These are the zone of poor quality water to the north (central) and east of the area of high potential and the zone of quality groundwater to the northeast, west and southwest of low potential. The study revealed that productive boreholes for excellent and sustainable yields were more viable in the northern (central) and eastern parts of the study area than in the northeast, west and southwest parts.

Highlights

  • IntroductionGroundwater is one of the most valuable resources and main source of potable drinking

  • Hydraulic and layer parameters of groundwater aquifer have been evaluated in parts of Buruku and Gboko local government area councils, for the primary purpose of assessing quality and potential of groundwater in the areas

  • The present study aims at assessing groundwater quality and evaluating aquifer hydraulic parameters to possibly delineate areas with quality groundwater and high aquifer potential using geoelectric method

Read more

Summary

Introduction

Groundwater is one of the most valuable resources and main source of potable drinking. It supplies fresh drinking water for over 95% of the world population. This is especially important in parts of the world that do not have ample surface water sources. Groundwater is stored in a geologic formation called aquifer. Aquifer is a water bearing layer which produces economically useful amount of water to springs and well. They are typically made up of gravel, sand, sandstone or fractured rock. The regional distribution on earth, varies and depends mainly on climatic conditions as well as the geology of the subsurface (Sophocleous, 2000; Alley and Leake, 2004) [1] [2]

Methods
Findings
Discussion
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call