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논문 기본 정보

자료유형
학술저널
저자정보
Dejian Wang (School of Resources and Environmental Engineering Hefei University of Technology China) Jiazhong Qian (School of Resources and Environmental Engineering, Hefei University of Technology, China) Weidong Zhao (School of Resources and Environmental Engineering Hefei University of Technology China) Xiaoliang Hou (School of Resources and Environmental Engineering Hefei University of Technology China) Wei Wang (School of Resources and Environmental Engineering, Hefei University of Technology, China) Lei Ma (School of Resources and Environmental Engineering, Hefei University of Technology, China)
저널정보
한국지질과학협의회 Geosciences Journal Geosciences Journal Vol.26 No.4
발행연도
2022.8
수록면
529 - 543 (15page)
DOI
10.1007/s12303-022-0004-3

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To disclose the distribution characteristics, the situation of flow and storage, and processes along flow paths of shallow groundwater in Tan-Lu fault zones, nine hundred and seven groundwater table elevations data and one hundred hydrochemical samples of shallow groundwater were taken from the Tan-Lu fault zone in Anhui province to analyze the characteristic of groundwater distribution. The geographic information system (GIS) method was used to analyze the spatial distribution characteristics of groundwater tables, total dissolved solids (TDS) and chloride ion (Cl?). Geophysical prospecting, drilling material and regional hydrogeological survey were utilized to disclose groundwater storage and flow regime in the fault zone. The results show that the Tan-Lu fault zone in Anhui province has controlled groundwater flow into the Jiashan basin, Hefei basin, Chaohu area and Qianshan basin, which developed from north to south in this area. Groundwater in theses basins have recharged from surrounding areas to form a water storage space. Geophysical prospecting and drilling technology revealed that the Tan-Lu fault zone provided a flow channel and storage space for groundwater. Faults provide preferential channels in some areas for the groundwater flow and circulation, eventually deep hot-water flows upward and discharges in the form of hot-springs. The identification of the groundwater flow pathway can help to provide a reliable scientific basis for regional spatial development and utilization of groundwater resources.

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