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The influence of slope collapse on water exchange between a pit lake and a heterogeneous aquifer |
Bo Zhang1,2, Xilai Zheng1,2, Tianyuan Zheng(), Jia Xin1,2, Shuai Sui1,2, Di Zhang4 |
1. Shandong Provincial Key Laboratory of Marine Environment and Geological Engineering, Ocean University of China, Qingdao 266100, China 2. Key Laboratory of Marine Environmental Science and Ecology (Ministry of Education), College of Environmental Science and Engineering, Ocean University of China, Qingdao 266100, China 3. Department of Environmental Informatics, Helmholtz Centre for Environmental Research-UFZ, Leipzig 04318, Germany 4. Key Laboratory of Surficial Geochemistry, Ministry of Education, Department of Hydrosciences, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210023, China 5. College of Engineering, Ocean University of China, Qingdao 266100, China |
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Abstract Slope collapse will reduce the water exchange. Slope collapse will affect the spatial distribution of the water exchange. Precipitation have the most impact on the dynamics of the water exchange. Due to the increase in open pit mining, pit lakes have become common surface water features, posing a potential risk to subsurface aquifer. In this study, a pit lake–groundwater interaction model is built based on the general program MODFLOW with the LAK3 package. For the first time, the effects of lake-slope collapse and aquifer heterogeneity on pit lake–groundwater interactions are analyzed by dividing the lake into six water exchange zones based on the aquifer lithology and groundwater level. Our investigation and simulations reveal a total water exchange from groundwater to the lake of 349000 m3/a without collapse of the pit lake slope, while the total net water exchange under slope collapse conditions is 248000 m3/a (i.e., a reduction of 1.40-fold). The monthly net water exchange per unit width from groundwater to the lake reaches the largest in April, shifting to negative values in zone IV from June to August and in zone V in June and July. Moreover, the monthly net water exchange per unit width decreases from north to south, and the direction and magnitude of water exchange are found to depend on the hydraulic gradients between the lake and groundwater and the hydraulic conductivity of the slope collapse.
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Keywords
Pit lake
Slope collapse
Groundwater–surface water interactions
Numerical simulation
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Corresponding Author(s):
Tianyuan Zheng
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Issue Date: 18 February 2019
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