MONITORING AND NUMERICAL SIMULATION OF FORMATION OF WATER INRUSH PATHWAY CAUSED BY COAL MINING ABOVE CONFINED WATER WITH HIGH PRESSURE
XU Zhimin1,SUN Yajun1,GONG Siyuan2,ZHU Zongkui1
(1. School of Resources and Earth Science,China University of Mining and Technology,Xuzhou,Jiangsu 221116,China;
2. State Key Laboratory of Coal Resources and Safe Mining,China University of Mining and Technology,
Xuzhou,Jiangsu 221008,China)
Abstract:Mining-induced floor failure and formation of water conducted pathway is the necessary conditions for water inrush in coal mine,which are the basis for monitoring and predicting water inrush. In order to study the formation and evolution of floor failure and water conducted pathway caused by coal mining above confined water with high pressure in Xinyi coalmine,two research means,i.e. field monitoring and numerical simulation,are introduced. Subsequently,the variations of electrical resistivity,stress and pore water pressure of floor during mining process are analyzed. The result shows that the floor failure caused by coal mining above confined water with high pressure is influenced significantly by advanced supporting stress of working face and the failure depth of floor of working face 11011 is about 25 m,which is greater than general empirical value. Based on fluid-solid coupling theory,the established numerical simulation model of mining-induced floor failure can reflect the influencing factors of floor failure more accurately and objectively;and the maximum failure depth is up to 23.75 m,which is very close to field monitoring result. The variations of electrical resistivity,stress and pore water pressure can better reflect the whole process of mining-induced floor failure formation,water inrush pathway evolution and water filling. The conclusion indicates that the above-mentioned parameters can be used as the precursor information for monitoring and short-term predicting the water inrush hazards in coalmines.
徐智敏1,孙亚军1,巩思园2,朱宗奎1. 高承压水上采煤底板突水通道形成的监测与数值模拟[J]. 岩石力学与工程学报, 2012, 31(8): 1698-1704.
XU Zhimin1,SUN Yajun1,GONG Siyuan2,ZHU Zongkui1. MONITORING AND NUMERICAL SIMULATION OF FORMATION OF WATER INRUSH PATHWAY CAUSED BY COAL MINING ABOVE CONFINED WATER WITH HIGH PRESSURE. , 2012, 31(8): 1698-1704.
隋旺华,狄乾生. 开采沉陷土体变形与孔隙水压相互作用研究进展[J]. 工程地质学报,1999,7(4):303-309.(SUI Wanghua,DI Qiansheng. Study on interaction between soil mass deformation and pore water pressure during subsidence by mining[J]. Journal of Engineering Geology,1999,7(4):303-309.(in Chinese))
[1]
赵铁锤. 华北地区奥灰水综合防治技术[M]. 北京:煤炭工业出版社,2006:1-19.(ZHAO Tiechui. Integrated control technology for Ordovician limestone water in North China[M]. Beijing:China Coal Industry Publishing House,2006:1-19.(in Chinese))
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