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Many factors can induce rock burst. Shock energy and shock distance are two key factors affecting rock burst. The 32101 roadway of the Xingcun coal mine, which has a tendency for rock burst, was used as an example. The dynamic module of Itasca’s FLAC (Fast Lagrangian Analysis of Continua) 2D explicit finite-difference software was used to simulate the roadway’s destruction. The vibration velocity and displacements of the rock surrounding the roadway were modeled for different shock energies and hypocenter distances. The simulation results indicate that the vibration velocity and displacement of rock surrounding the roadway have a quadratic relationship to the shock energy and a power law relationship to the distance of the hypocenter from the roadway. A dynamic view of the process was obtained from a series of “snap-shots” collected at 100 different time steps. This shows an isolating “river” is first formed at the hypocenter. The region above the “river” is a low stress zone while below the “river” a high stress zone exists. This high stress zone surrounds the ribs of the roadway in a “double ear” pattern. Continuous and repeated action of the high stress in the “double ear” shaped zone destroys the roadway.
The 32101 roadway of the Xingcun coal mine, which has a tendency for rock burst, was used as an example. The dynamic module of Itasca’s FLAC ( Fast Lagrangian Analysis of Continua) 2D explicit finite-difference software was used to simulate the roadway’s destruction. The vibration velocity and displacements of the rock surrounding the roadway were modeled for different shock energies and hypocenter distances. The simulation results indicate that the vibration velocity and displacement of rock surrounding the roadway have a quadratic relationship to the shock energy and a power law relationship to the distance of the hypocenter from the roadway. A dynamic view of the process was obtained from a series of “snap-shots” collected at 100 different time steps. This shows an isolating “river” is first formed at the hypocenter. The region above the “river” is a low stress zone while below the “river ” a high stress zone exists. This high stress zone surrounds the ribs of the roadway in a “double ear ” pattern. Continuous and repeated action of the high stress in the “double ear ” shaped zone destroys the roadway.