Mechanism of the water invasion of Gaoyang Iron Mine, China and its impacts on the mine groundwater environment

Springer Science and Business Media LLC - Tập 49 - Trang 1163-1172 - 2006
He Keqiang1, Guo Dong1, Wang Xianwei1
1Department of Civil Engineering, Qingdao Technological University, 266033, People’s Republic of China

Tóm tắt

With the development of mining of iron deposits in China, groundwater invasion and the impacts of groundwater drainage, such as regional groundwater table lowering, overlapping cones of depression, subsidence, and water quality deterioration are environmental problems which endanger mining production and human life. Effective prevention of water invasion or timely determination of the mechanism of water bursting and rational design of drainage plans are the most urgent mining challenges. The mechanism of water invasion and the environment impacts on the groundwater system of the Gaoyang Iron Mine, China were dealt with in this paper. A systematical investigation of the hydrogeological conditions and monitoring of groundwater dynamics of the mine were completed. Results show that the limestone of the middle Ordovician System constitutes the under floor of the iron deposit. This limestone is the main source of water invasion into the mine. Groundwater dynamic equilibrium conditions are broken due to mine drainage. Water invasion and drainage have caused a serious impact on the groundwater environment of the area.

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