Hydrogeophysical Investigation for Groundwater Resources from Electrical Resistivity Tomography and Self-Potential Data in the Méiganga Area, Adamawa, Cameroon

IF 1 Q3 GEOCHEMISTRY & GEOPHYSICS
Meying Arsène, Bidichael Wahile Wassouo Elvis, G. Daniel, N. Theophile, Kuiate Kelian, Ngoh Jean Daniel
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引用次数: 21

Abstract

Exploration and production of groundwater, a vital and precious resource, is a challenging task in hard rock, which exhibits inherent heterogeneity. A geophysical survey was conducted in Méiganga, Mbéré department, in the Adamawa region, Cameroon. High-resolution electrical resistivity tomography (ERT) and self-potential (SP) dataset were collected in a gneissic terrain to solve the groundwater problem as people are facing acute shortage of drinking water in the study area. The analysis and interpretations based on resistivity models revealed substantial resistivity contrast between the altered gneiss that might contain water and massive gneiss and delineated five deeper groundwater prospects zones located at Yelwa, Ngoa-Ekélé, Sabongari, Ngassiri, and Gbakoungué, respectively. Nevertheless shallow groundwater zones (<13 m) are located in the northern part of the study area at high elevation while best prospect and productive groundwater zones lying between 20 and 25 m depth are at low elevation in the southern part. On the other hand, analysis of SP negative peaks along with groundwater head and groundwater vector maps revealed areas of recharge and discharge across the study area. The discharge areas serve as groundwater collection center and are good groundwater potential zones. In addition these maps revealed that groundwater flow pattern shows inward flow from the flanks to center and south central parts of the study area.
喀麦隆阿达马瓦Méiganga地区地下水资源的电阻率层析成像和自电位数据水文地质调查
地下水是一种重要而珍贵的资源,在具有内在非均质性的坚硬岩石中,地下水的勘探和开采是一项具有挑战性的任务。在喀麦隆阿达马瓦地区姆贝雷省的梅甘加进行了地球物理调查。高分辨率电阻率层析成像(ERT)和自电位(SP)数据集是在片麻岩地形中收集的,以解决研究区域内人们面临饮用水严重短缺的地下水问题。基于电阻率模型的分析和解释揭示了可能含有水的蚀变片麻岩和块状片麻岩之间的电阻率对比,并分别位于Yelwa、Ngoa Ekélé、Sabongari、Ngassiri和Gbakoungué的五个更深的地下水勘探区。然而,浅层地下水带(<13m)位于研究区北部的高海拔地区,而20至25m深度的最佳勘探和生产地下水带位于南部的低海拔地区。另一方面,对SP负峰以及地下水水头和地下水矢量图的分析揭示了整个研究区域的补给和排泄区域。排放区是地下水收集中心,是良好的地下水潜力区。此外,这些地图显示,地下水流动模式显示从研究区域的侧翼向中心和中南部向内流动。
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来源期刊
International Journal of Geophysics
International Journal of Geophysics GEOCHEMISTRY & GEOPHYSICS-
CiteScore
1.50
自引率
0.00%
发文量
12
审稿时长
21 weeks
期刊介绍: International Journal of Geophysics is a peer-reviewed, Open Access journal that publishes original research articles as well as review articles in all areas of theoretical, observational, applied, and computational geophysics.
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