Evaluation of groundwater potential in Kabirwala area, Pakistan: A case study by using geophysical, geochemical and pump data

doi:10.1111/1365-2478.12679

CORC > 地质与地球物理研究所 > 中国科学院地质与地球物理研究所 > 中国科学院页岩气与地质工程重点实验室

	Evaluation of groundwater potential in Kabirwala area, Pakistan: A case study by using geophysical, geochemical and pump data
	Hasan, Muhammad 1,2,3; Shang, Yanjun 1,2,3; Akhter, Gulraiz 4; Jin, Weijun1,2,3
刊名	GEOPHYSICAL PROSPECTING
	2018-11-01
卷号	66 期号:9 页码:1737-1750
关键词	Dar Zarrouk parameters Electrical resistivity Groundwater Hydraulic conductivity Pump test Transmissivity Vertical electrical soundings (VES)
ISSN号	0016-8025
DOI	10.1111/1365-2478.12679
英文摘要	Knowledge of hydraulic parameters (hydraulic conductivity and transmissivity) is essential for the delineation of groundwater potential zones. Conventionally, these parameters are measured using pumping tests carried out on boreholes. However, pumping tests are costly, labour intensive and require a considerable amount of equipment. The integration of geophysical methods with pumping tests provides efficient and cost-effective alternative to calculate hydraulic parameters. Fifty electrical resistivity soundings were carried out in the study area using Schlumberger inter-electrode configuration to obtain hydraulic characteristics that are estimated through the pumping tests. To apply this approach successfully, sufficient number of boreholes are used. Part of the boreholes, in which pumping tests were carried out, is used for both to constrain resistivity inversions and to establish the empirical relationship between the interpreted geophysical and hydraulic parameters. The rest of the boreholes without pumping tests are still used for constraining the inversions. Initially, aquifer parameters were measured using pumping tests at 12 water wells. Afterwards, transmissivity (T) and hydraulic conductivity (K) were correlated with transverse resistance (T-r) and the bulk resistivity ((o)) of the aquifer at other sites where pumping tests had not been conducted. In this way, the entire study area was covered to assess the groundwater reserves. The hydraulic properties obtained by the geophysical method fit pretty well to both the pumping and physicochemical data of the investigated area. The integrated study reveals five layers (i.e. topsoil, clay, clay sand, sand and gravel sand) and three potential zones (i.e. high, medium and low potential aquifer zones) with specific ranges of T, K, T-r and (o). The results suggest that, in case of sparse well data, the aquifer parameters can be estimated using the relations depending on the specifications of the area.
资助项目	CAS-TWAS President's Fellowship for International PhD Students ; National Natural Science Foundation of China[41372324] ; National Natural Science Foundation of China[41772320] ; Xinjiang Uygur Autonomous Region International Science and Technology Cooperation Program[20166017] ; Key Laboratory of Shale Gas and Geoengineering, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing China ; Pakistan Council of Research in Water Resources (PCRWR), Islamabad Pakistan
WOS关键词	HYDRAULIC CONDUCTIVITY ; ELECTRICAL-RESISTIVITY ; AQUIFER ; TRANSMISSIVITY ; POROSITY ; PARAMETERS ; RESERVOIR ; NIGERIA ; SURFACE ; SANDS
WOS研究方向	Geochemistry & Geophysics
语种	英语
出版者	WILEY
WOS记录号	WOS:000448076000008
资助机构	CAS-TWAS President's Fellowship for International PhD Students ; CAS-TWAS President's Fellowship for International PhD Students ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Xinjiang Uygur Autonomous Region International Science and Technology Cooperation Program ; Xinjiang Uygur Autonomous Region International Science and Technology Cooperation Program ; Key Laboratory of Shale Gas and Geoengineering, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing China ; Key Laboratory of Shale Gas and Geoengineering, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing China ; Pakistan Council of Research in Water Resources (PCRWR), Islamabad Pakistan ; Pakistan Council of Research in Water Resources (PCRWR), Islamabad Pakistan ; CAS-TWAS President's Fellowship for International PhD Students ; CAS-TWAS President's Fellowship for International PhD Students ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Xinjiang Uygur Autonomous Region International Science and Technology Cooperation Program ; Xinjiang Uygur Autonomous Region International Science and Technology Cooperation Program ; Key Laboratory of Shale Gas and Geoengineering, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing China ; Key Laboratory of Shale Gas and Geoengineering, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing China ; Pakistan Council of Research in Water Resources (PCRWR), Islamabad Pakistan ; Pakistan Council of Research in Water Resources (PCRWR), Islamabad Pakistan ; CAS-TWAS President's Fellowship for International PhD Students ; CAS-TWAS President's Fellowship for International PhD Students ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Xinjiang Uygur Autonomous Region International Science and Technology Cooperation Program ; Xinjiang Uygur Autonomous Region International Science and Technology Cooperation Program ; Key Laboratory of Shale Gas and Geoengineering, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing China ; Key Laboratory of Shale Gas and Geoengineering, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing China ; Pakistan Council of Research in Water Resources (PCRWR), Islamabad Pakistan ; Pakistan Council of Research in Water Resources (PCRWR), Islamabad Pakistan ; CAS-TWAS President's Fellowship for International PhD Students ; CAS-TWAS President's Fellowship for International PhD Students ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Xinjiang Uygur Autonomous Region International Science and Technology Cooperation Program ; Xinjiang Uygur Autonomous Region International Science and Technology Cooperation Program ; Key Laboratory of Shale Gas and Geoengineering, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing China ; Key Laboratory of Shale Gas and Geoengineering, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing China ; Pakistan Council of Research in Water Resources (PCRWR), Islamabad Pakistan ; Pakistan Council of Research in Water Resources (PCRWR), Islamabad Pakistan
内容类型	期刊论文
源URL	[http://ir.iggcas.ac.cn/handle/132A11/89172]
专题	地质与地球物理研究所_中国科学院页岩气与地质工程重点实验室
通讯作者	Hasan, Muhammad
作者单位	1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Shale Gas & Geoengn, Beijing 100029, Peoples R China 2.Chinese Acad Sci, Inst Earth Sci, Beijing 100029, Peoples R China 3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 4.Quaid I Azam Univ, Dept Earth Sci, Islamabad 45320, Pakistan
推荐引用方式 GB/T 7714	Hasan, Muhammad,Shang, Yanjun,Akhter, Gulraiz,et al. Evaluation of groundwater potential in Kabirwala area, Pakistan: A case study by using geophysical, geochemical and pump data[J]. GEOPHYSICAL PROSPECTING,2018,66(9):1737-1750.
APA	Hasan, Muhammad,Shang, Yanjun,Akhter, Gulraiz,&Jin, Weijun.(2018).Evaluation of groundwater potential in Kabirwala area, Pakistan: A case study by using geophysical, geochemical and pump data.GEOPHYSICAL PROSPECTING,66(9),1737-1750.
MLA	Hasan, Muhammad,et al."Evaluation of groundwater potential in Kabirwala area, Pakistan: A case study by using geophysical, geochemical and pump data".GEOPHYSICAL PROSPECTING 66.9(2018):1737-1750.