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利用水力参数对尼日利亚东北部贡贝及其周边地区的含水层潜在区域进行 delineation。(注:“delineation” 这个词在中文里可能没有完全对应的准确词汇,这里保留英文以便准确传达原文信息)

Delineation of aquifer potential zones using hydraulic parameters in Gombe and environs, North-Eastern, Nigeria.

作者信息

Kwami I A, Ishaku J M, Mukkafa S, Haruna A I, Ankidawa B A

机构信息

Department of Geology, Gombe State University, P.M.B.0127, Gombe, Nigeria.

Department of Geology, School of Physical Sciences, Modibbo Adama University of Technology, PMB 2076, Yola, Nigeria.

出版信息

Heliyon. 2019 Jul 3;5(7):e01927. doi: 10.1016/j.heliyon.2019.e01927. eCollection 2019 Jul.

DOI:10.1016/j.heliyon.2019.e01927
PMID:31317078
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC6611938/
Abstract

This research is aimed at delineating the groundwater potential zones in Gombe and environs using Dar Zarrouk parameters. The study area is located within longitudes 11°7'0″E to 11°14'0″E, and latitudes 10°15'0″N to 10°21'0″N, it is basically underlain by basement Complex rocks represented by Diorite and Granites, and Cretaceous sedimentary rocks represented by Bima, Yolde, Fika and Gombe Formations. Thirty two (32) vertical electric soundings (VES) using Schlumberger array method with the aid of ABEM Signal Averaging System (SAS) Terrameter was used for the data acquisition. The result of the interpretation shows four to six geo-electric layers. The geo-electric section revealed the major aquifers to be confined and semi confined and consist of Medium grain sandstones, with varying thicknesses. The aquifer hydraulic characteristics indicated that the transverse resistance, ranges from 235.2Ωm to 6317.87Ωm with an average value of 1789.50Ωm. The Longitudinal conductance, S, ranges from 0.1415Ωm to 31.933Ωm with an average of 2.002Ωm. The Hydraulic conductivity value range from 2.62m/day to 138.66 m/day with a mean value of 20.662 m/day. The transmissivity values obtained for the various layers range from 78.34 m/day to 13284.02m/day, with the average value been 893.57 m/day. Four groundwater potential zones were delineated including medium grain sandstones, Sandstones, clayey sand and shaly sand.

摘要

本研究旨在利用达扎鲁克参数描绘贡贝及其周边地区的地下水潜力区。研究区域位于东经11°7′0″至11°14′0″,北纬10°15′0″至10°21′0″之间,其基底主要由闪长岩和花岗岩代表的基底杂岩以及由比马组、约尔德组、菲卡组和贡贝组代表的白垩纪沉积岩构成。借助ABEM信号平均系统(SAS)地电仪,采用施伦贝格阵列法进行了32次垂直电测深(VES)以获取数据。解释结果显示有四至六个地电层。地电剖面表明主要含水层为承压含水层和半承压含水层,由中粒砂岩组成,厚度各异。含水层的水力特征表明,横向电阻范围为235.2Ωm至6317.87Ωm,平均值为1789.

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/18e3/6611938/d84ed39c2234/gr9.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/18e3/6611938/630f13c0116b/gr1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/18e3/6611938/752595c9520d/gr2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/18e3/6611938/12798d10fc64/gr3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/18e3/6611938/faefb9f2caf7/gr4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/18e3/6611938/3931758a7a40/gr5.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/18e3/6611938/578ed5961a7a/gr6.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/18e3/6611938/7e273a22e6b9/gr7.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/18e3/6611938/3f09ce2a4119/gr8.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/18e3/6611938/d84ed39c2234/gr9.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/18e3/6611938/630f13c0116b/gr1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/18e3/6611938/752595c9520d/gr2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/18e3/6611938/12798d10fc64/gr3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/18e3/6611938/faefb9f2caf7/gr4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/18e3/6611938/3931758a7a40/gr5.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/18e3/6611938/578ed5961a7a/gr6.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/18e3/6611938/7e273a22e6b9/gr7.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/18e3/6611938/3f09ce2a4119/gr8.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/18e3/6611938/d84ed39c2234/gr9.jpg

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