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| Study on development law of water-conducting fractures in overlying strata of three soft coal seam mining under thick loose layers |
| LAI Xingping1,2,3,ZHANG Xudong1,SHAN Pengfei1,2,3,CUI Feng1,2,3,LIU Bowei1,BAI Rui1 |
| (1. College of Energy Science and Engineering,Xi¢an University of Science and Technology,Xi'an,Shaanxi 710054,China;2. State Key Laboratory of Coal Resources in Western China,Xi'an University of Science and Technology,Xi'an,Shaanxi 710054,China;3. Key Laboratory of Western Mine Exploration and Hazard Prevention,Ministry of Education,Xi'an University of Science and Technology,Xi'an,Shaanxi 710054,China) |
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Abstract In order to grasp the law of overlying strata movement and water-conducting fracture development in three-soft coal seam mining under thick loose layers. Taking Chenghe mining area as the background,using the similarity simulation experiment,comprehensively using the research method of the total station monitoring,high-definition borehole TV monitoring,3DEC software and SPSS professional statistical analysis software,and introducing the mining damage theory,the overburden migration law,fracture development and evolution,and distribution characteristics of water-conducting fracture zone were studied under this condition. The results show that the Overburden migration presents asymmetry,the subsidence extreme value of rock strata in different layers always deviates to the side of open-off cut,and the movement range of the loose layer is larger than that of the top layer of the bedrock,showing a“hyperbolic-like”shape as a whole. According to the theoretical formula,the fracture angle of the bedrock is relatively small,ranging from 56° to 58°. The height of the caving zone and the caving-mining ratio are 13.75 m and 3.06 respectively,and the height of the water-conducting fracture zone and the fracture-mining ratio are 75 m and 16.67 respectively. The number of fractures gradually increases from the surface to the bottom and suddenly increases in the water-conducting fracture zone. The development of fissures is controlled by the mining stress field in the 33° east by north direction. The evolution of the water-conducting fracture zone presents five stages which are“slow development,gradual increase,large and sudden increase,periodic small increase and stable development”. Through 3DEC simulation,it is concluded that the height of water-conducting fracture zone has an exponential function relationship with the thickness of loose layer,a linear relationship with mining height,and a logarithmic function relationship with buried depth and inclined length of working face. Using SPSS professional statistical analysis software,the empirical formula for predicting the height of the water-conducting fractured zone is fitted based on the multiple nonlinear regression theory. By comparing the calculation results,the rationality of the regression empirical equation in predicting the height of the water-conducting fracture zone is verified. Because the K5 sandstone aquifer has a large unit water inflow and is close to the coal seam. In order to avoid the mining of the coal seam from being affected by the overburden K5 sandstone aquifer. According to the obtained prediction empirical formula,the maximum mining height of the coal seam should not surpass 3.8 m. This research has important reference value for water-conservation mining in coal mine under similar geological conditions.
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