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

被引:17
作者
Arsene, Meying [1 ]
Elvis, BidichaelWahile Wassouo [2 ]
Daniel, Gouet [3 ]
Theophile, Ndougsa-Mbarga [2 ,4 ]
Kelian, Kuiate [1 ]
Daniel, Ngoh Jean [2 ]
机构
[1] Univ Ngaoundere, Sch Geol & Min Engn, Ngaoundere, Cameroon
[2] Univ Yaounde I, Postgrad Sch Sci Technol & Geosci, Yaounde, Cameroon
[3] Univ Maroua, Fac Mines & Petr Ind, Dept Petr Min & Groundwater Resources Explorat, Maroua, Cameroon
[4] Univ Yaounde I, Adv Teachers Training Coll, Dept Phys, Yaounde, Cameroon
关键词
D O I
10.1155/2018/2697585
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
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 Meiganga, Mbere 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-Ekele, Sabongari, Ngassiri, and Gbakoungue, 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.
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页数:14
相关论文
共 37 条
[1]   Hydrogeophysical and hydrogeological investigations of groundwater resources in Delta Central, Nigeria [J].
Anomohanran, Ochuko .
JOURNAL OF TAIBAH UNIVERSITY FOR SCIENCE, 2015, 9 (01) :57-68
[2]  
Baise D., 1995, GUIDE DESCRIPTION SO
[4]  
BELL FG, 1983, FUNDAMENTALS ENG GEO
[5]  
Betah S. S., 1976, COMPLEMENT MONOGRAPH
[6]   Resolution of 2D Wenner resistivity imaging as assessed by numerical modelling [J].
Dahlin, T ;
Loke, MH .
JOURNAL OF APPLIED GEOPHYSICS, 1998, 38 (04) :237-249
[7]  
Dedzo MG, 2017, HYDROLOGY-BASEL, V4, DOI 10.3390/hydrology4020023
[8]  
Faleye E. T., 2011, Journal of Emerging Trends in Engineering and Applied Sciences, V2, P864
[9]  
Ganwa A.A., 2011, INT J GEOSCI, V2, P138
[10]   Archean inheritances in the pyroxene-amphibole-bearing gneiss of the Meiganga area (Central North Cameroon):: Geochemical and 207Pb/206Pb age imprints [J].
Ganwa, Alembert Alexandre ;
Frisch, Wolfgang ;
Siebel, Wolfgang ;
Ekodeck, Georges Emmanuel ;
Shang, Cosmas Kongyuy ;
Ngako, Vincent .
COMPTES RENDUS GEOSCIENCE, 2008, 340 (04) :211-222