WANG Xuebin,LIU Tongxin,CEN Zihao,et al.Study on Evolution of the Fault Slip during the Normal Fault Footwall Mining based on a Continuum⁃Discontinuum Method[J].Journal of Disaster Prevention and Mitigation Engineering,2021,41(04):804-812.
WANG Xuebin,LIU Tongxin,CEN Zihao,et al.Study on Evolution of the Fault Slip during the Normal Fault Footwall Mining based on a Continuum⁃Discontinuum Method[J].Journal of Disaster Prevention and Mitigation Engineering,2021,41(04):804-812. DOI: 10.13409/j.cnki.jdpme.202105009.
Study on Evolution of the Fault Slip during the Normal Fault Footwall Mining based on a Continuum⁃Discontinuum Method
Based on a hybrid continuum-discontinuum method where the Lagrangian element method and the discrete element method are combined, a quasi-static model was proposed to simulate the long mining process. The stress drop method was developed for dealing with the problem that the aggregation formed by discrete elements of the coal seam can still sustain loads above its own bearing capacity. A more accurate mechanical model was established based on the geological conditions of the 6303 working face in the 3rd Jining coal mine. In order to overcome stress concentration problems in the previous mechanical model caused by the fault slip restriction due to limited displacement at the base of the model, an appropriate uniform stress was applied at the base of the fault hanging wall. The slip displacement of the fault before mining was eliminated, and a calculation method for the slip displacement of the hanging wall caused by mining was proposed. The following results were found. When the distance between the working face and the fault decreases, slip displacements of monitored nodes below the coal seam exhibit a slow increase, followed by a slow decrease and a sharp increase; slip displacements of the monitored nodes above the coal seam exhibit a slow increase, followed by a rapid increase. There are few differences in slip displacements of the monitored nodes for the same strata. Higher overburden strata will have obvious slip before lower overburden strata. The fault slip basically develops from top to bottom, and the slip degree of higher overburden strata is greater than that of lower overburden strata. When the distance between the working face and the fault is the same, if the mining interval is small, slip displacements of the monitored nodes above the coal seam are small. When the distance between the working face and the fault is less than or equal to 100 m, strata in the vicinity of the goaf slips obviously so that the support should be strengthened.
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