Delineation of Groundwater Potential Zones of Girei and Environs, Adamawa State, North Eastern Nigeria

Zainab Haliru Ali, Buba Apagu Ankidawa, Jackson M. Ishaku, Ahmed Buba Seli
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Abstract

Evaluation of groundwater resources of Girei and environs is necessary in order to develop appropriate water supply scheme to the community. Cases of borehole failures have been on increase in the area due to a lack of knowledge of the aquifer geometry. The study is aimed at delineating the groundwater potential zones of Girei and environs with the objectives of delineating the different aquifer systems, estimating the aquifer characteristics such as transmissivity and hydraulic conductivity using the Dar Zarrouk parameter, determining groundwater flow direction, and identifying the recharged and discharged areas. Geological investigation indicates that the area underlain by Bima sandstone. Thirty profiles of Vertical Electrical Sounding using Schlunberger array method with the aid of ABEM signal averaging system (SAS 1000) was used to determine aquifer types and groundwater potential zones. Correlation between borehole lithological section and geoelectric section within the study area revealed a confineded aquifer type. The aquifer characteristics indicate that the transverse resistance ranged between 29.796 to 238000 ?m2, longitudinal conductance ranged between 0.0148 ?-1 to 9.34 ?-1, hydraulic conductivity values range from 0.0014 to 5.865 m/s with an average value of 0.0355 m/s. Transmissivity values obtained from the various layers range from 237.6 m2/day to 6324 m2/day. Aquifer rating based on transmissivity values reveals that the aquifers in the study area have moderate to high potential.
尼日利亚东北部阿达马瓦州Girei及其周边地区地下水潜力区圈定
为了制定适当的社区供水方案,有必要对吉雷及其周边地区的地下水资源进行评价。由于缺乏对含水层几何形状的了解,该地区的钻孔失败案例有所增加。该研究旨在圈定吉雷及其周边地区的地下水潜力带,目的是圈定不同的含水层系统,利用Dar Zarrouk参数估算含水层特征,如透水性和导电性,确定地下水流动方向,并确定补给和排放区域。地质调查表明,该地区下部为毕玛砂岩。利用30条Schlunberger阵列垂直电测深剖面,借助于ABEM信号平均系统(SAS 1000),确定了含水层类型和地下水潜力带。研究区内钻孔岩性剖面与地电剖面对比显示为封闭含水层类型。含水层特征表明:横向阻力为29.796 ~ 238000 μ m2,纵向电导为0.0148 μ m -1 ~ 9.34 μ m -1,水力电导值为0.0014 ~ 5.865 μ m/s,平均值为0.0355 μ m/s。不同层的透射率值从237.6 m2/天到6324 m2/天不等。基于透光率值的含水层等级表明研究区含水层具有中高潜力。
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