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Research on downward crack closing of clay aquiclude in shallow coal seam safety mining

Journal of Coal Science & Engineering(China) 2011年第3期17卷 349-354页

作者： HUANG Qing-xiang ZHANG Wen-zhong School of Energy Engineering Key Laboratory of Western Mine Exploitation and Hazard Prevention of Ministry of Education Xi＇an University of Science and Technology Xi＇an 710054 China

The water resisting property of aquiclude is the key factor of water conservation and safety mining, and the mining induced cracks in aquiclude is major factor of water resisting property. The aquiclude is composed by loess layer and red clay layer in Yushuwan Coal Mine, and the water reaction property of clay and loess of aquiclude was tested by soil mechanics method. The permeability coefficient of the loess is 0.856 m/d and the clay is 0.434 m/d. The dilatability coefficient of the loess is 16.1% and the clay is 14.6%. Through physical solid-liquid simulation with whole stress-stain similarity, the distribution of ＂downward crack zone＂ and ＂upward crack zone＂ was found to be the major factor of aquiclude stability. The downward crack closing length is about 30% of the downward crack length. The expanding of clay and loess with water are principal factors of downward crack closing. At last, the mechanical model of downward crack closing was constructed, and the criterion of crack closing was put forward at all. This work will provides the theoretical base for aquiclude stability research and safety mining in shallow seam.

关键词： shallow coal seam simulation clay aquiclude downward crack crack closing

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