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Impacts of underground coal mining on phreatic water level variation in arid and semiarid mining areas: a case study from the Yushenfu mining area, China

Liu, Shiliang ; Dai, Song ; Zhang, Wenhui ; Li, Weiguo ; Liu, Yang ; Ren, Yingjie ; Li, Wenping

Environmental earth sciences, 2022-05, Vol.81 (9), Article 269 [Periódico revisado por pares]

Berlin/Heidelberg: Springer Berlin Heidelberg

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Título:
Impacts of underground coal mining on phreatic water level variation in arid and semiarid mining areas: a case study from the Yushenfu mining area, China
Autor: Liu, Shiliang ; Dai, Song ; Zhang, Wenhui ; Li, Weiguo ; Liu, Yang ; Ren, Yingjie ; Li, Wenping
Assuntos: Aquifers ; Biogeosciences ; Case studies ; Coal ; Coal mines ; Coal mining ; Conservation ; Earth and Environmental Science ; Earth Sciences ; Environmental Science and Engineering ; Error analysis ; Exploitation ; Geochemistry ; Geology ; Groundwater ; Groundwater management ; Groundwater resources ; Hydrology/Water Resources ; Leakage ; Leaky aquifers ; Microbalances ; Mining ; Monitoring ; Original Article ; Rain ; Rainfall ; Recovery ; Recovery time ; Sustainable development ; Terrestrial Pollution ; Underground mining ; Variation ; Vegetation ; Water conservation ; Water levels ; Water management ; Water resources ; Water resources management
É parte de: Environmental earth sciences, 2022-05, Vol.81 (9), Article 269
Descrição: Underground coal mining destroys overlying strata, and phreatic aquifer above the panel is destabilized, causing phreatic water level (PWL) variation. On-site monitoring of the PWL variation throughout the mining period is of great significance to the management and conservation of groundwater resources in arid and semiarid mining areas. The research on the decline of the PWL when phreatic aquifer leakage is concentrated, but there is little research on the fluctuation characteristics of PWL under the condition of phreatic aquifer without leakage. Therefore, using the #108 coalface in the Jinjitan colliery of the Yushenfu mining area as a case study to carry out the research on PWL fluctuation induced by underground coal mining. First, phreatic water without leakage throughout the coal mining period in the #108 coalface was determined. Second, considering surface subsidence induced by mining activities and PWL in fluviograph comprehensively, true PWL fluctuation characteristics were analyzed throughout the whole coal seam mining period. It is concluded that the buried depth of PWL presented a trend of “decreasing sharply—increasing sharply—decreasing slowly—increasing slowly—becoming stable” in the monitoring period of 1 year. Furthermore, a well flow model was established to simulate the PWL variation process before and after coal mining and to predict the PWL recovery time after coal mining. On these bases, the error analysis of the measured and predicted PWL recovery time, the relationship between the PWL fluctuation and the residual aquiclude thickness, the impact of rainfall on PWL recovery, the response of surface vegetation eco-environment, and phreatic water resources management and conservation were discussed. These research results are important for achieving a win–win situation strategy that balances the exploitation of coal resources and the conservation of phreatic water resources, promoting the sustainable development of coal mining.
Editor: Berlin/Heidelberg: Springer Berlin Heidelberg
Idioma: Inglês

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Impacts of underground coal mining on phreatic water level variation in arid and semiarid mining areas: a case study from the Yushenfu mining area, China

Liu, Shiliang ; Dai, Song ; Zhang, Wenhui ; Li, Weiguo ; Liu, Yang ; Ren, Yingjie ; Li, Wenping

Berlin/Heidelberg: Springer Berlin Heidelberg

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