中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Feasibility of Monitoring Hydraulic Connections between Aquifers Using Time-lapse TEM: A Case History in Inner Mongolia, China

文献类型:期刊论文

作者Chen, Kang3; Zhang, Junyan2; Xue, Guoqiang1; Huang, Hao3; Chen, Weiying1; Hao, Jutao3; Yue, Yuezhen3
刊名JOURNAL OF ENVIRONMENTAL AND ENGINEERING GEOPHYSICS
出版日期2019-09-18
卷号24期号:3页码:361-372
ISSN号1083-1363
DOI10.2113/JEEG24.3.361
英文摘要Hydraulic connections between aquifers is usually studied through hydrochemical analysis or by pumping tests. However, hydrochemical analyses are usually conducted in areas of variable lithology. In addition, the hydrogeological data obtained by drilling and pumping tests are typically insufficient to get 3D distributions of hydraulic head. In this paper, the time-lapse transient electromagnetic method (TEM) is used to image groundwater migration between aquifers in Inner Mongolia, China. First, 1D geophysical models of aquifers are generalized according to the hydrogeological conditions of the region, and the feasibility of detecting the multiple aquifers by TEM is analyzed and discussed. Then, the 2D models of aquifers pre- and post- pumping test are established based on the distribution of groundwater in the aquifers, and the variation law of induced electromotive force measured on the surface is analyzed. The simulation results show that significant time-lapse electromagnetic anomalies can be observed between pre- and post- pumping test and the variation in the induced electromotive force reaches a distinguishable level between 0.7 ms and 100 ms due to the vertical change in the aquifer properties. Furthermore, the electromagnetic variation generated by hydraulic connection between aquifers is greater than 30% within the range of 3/4 of the transmitting loop. Finally, a successful case history to map hydraulic connections between aquifers is conducted using a time-lapse TEM pre- and post- a pumping experiment. This simulation and field experiment shows that time-lapse TEM could characterize and monitor the groundwater migration more effectively than pump tests or hydrogeochemical methods alone.
WOS关键词ELECTROMAGNETIC-FIELDS ; SALTWATER INTRUSION ; COAL-MINE ; WATER ; GROUNDWATER ; DIFFUSION ; EARTH
资助项目National Key R&D Program of China[2018YFC0407102] ; IWHR Basic Research Fund[SM0145B632017] ; IWHR Basic Research Fund[SM0145B9502017] ; key Research and Development Program of Shannxi Province[2017GY-175]
WOS研究方向Geochemistry & Geophysics ; Engineering
语种英语
WOS记录号WOS:000488213700003
出版者ENVIRONMENTAL ENGINEERING GEOPHYSICAL SOC
资助机构National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; IWHR Basic Research Fund ; IWHR Basic Research Fund ; IWHR Basic Research Fund ; IWHR Basic Research Fund ; key Research and Development Program of Shannxi Province ; key Research and Development Program of Shannxi Province ; key Research and Development Program of Shannxi Province ; key Research and Development Program of Shannxi Province ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; IWHR Basic Research Fund ; IWHR Basic Research Fund ; IWHR Basic Research Fund ; IWHR Basic Research Fund ; key Research and Development Program of Shannxi Province ; key Research and Development Program of Shannxi Province ; key Research and Development Program of Shannxi Province ; key Research and Development Program of Shannxi Province ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; IWHR Basic Research Fund ; IWHR Basic Research Fund ; IWHR Basic Research Fund ; IWHR Basic Research Fund ; key Research and Development Program of Shannxi Province ; key Research and Development Program of Shannxi Province ; key Research and Development Program of Shannxi Province ; key Research and Development Program of Shannxi Province ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; IWHR Basic Research Fund ; IWHR Basic Research Fund ; IWHR Basic Research Fund ; IWHR Basic Research Fund ; key Research and Development Program of Shannxi Province ; key Research and Development Program of Shannxi Province ; key Research and Development Program of Shannxi Province ; key Research and Development Program of Shannxi Province
源URL[http://ir.iggcas.ac.cn/handle/132A11/93891]  
专题地质与地球物理研究所_中国科学院矿产资源研究重点实验室
通讯作者Xue, Guoqiang
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China
2.China Univ Geosci, Sch Energy Resources, Beijing 100083, Peoples R China
3.China Inst Water Resources & Hydropower Res, State Key Lab Simulat & Regulat Water Cycle River, Beijing 100038, Peoples R China
推荐引用方式
GB/T 7714
Chen, Kang,Zhang, Junyan,Xue, Guoqiang,et al. Feasibility of Monitoring Hydraulic Connections between Aquifers Using Time-lapse TEM: A Case History in Inner Mongolia, China[J]. JOURNAL OF ENVIRONMENTAL AND ENGINEERING GEOPHYSICS,2019,24(3):361-372.
APA Chen, Kang.,Zhang, Junyan.,Xue, Guoqiang.,Huang, Hao.,Chen, Weiying.,...&Yue, Yuezhen.(2019).Feasibility of Monitoring Hydraulic Connections between Aquifers Using Time-lapse TEM: A Case History in Inner Mongolia, China.JOURNAL OF ENVIRONMENTAL AND ENGINEERING GEOPHYSICS,24(3),361-372.
MLA Chen, Kang,et al."Feasibility of Monitoring Hydraulic Connections between Aquifers Using Time-lapse TEM: A Case History in Inner Mongolia, China".JOURNAL OF ENVIRONMENTAL AND ENGINEERING GEOPHYSICS 24.3(2019):361-372.

入库方式: OAI收割

来源:地质与地球物理研究所

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