摘要
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.
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.
基金
Projects 50490270, 50474068, 50674085 supported by the National Natural Science Foundation of China
2005CB221504 by the National Key FoundationResearch Program of China
2006BAK04B02, 2006BAK03B06 by the National Science Program of China
NCET-06-0478 by the Ministry of Education New Century Outstanding Person Programming of China
2006B002 by the Science Foundation of China University of Mining and Technology
关键词
模拟技术
震源参数
岩石爆破
冲击波
rock burst
roadway supporting
destruction process
shock energy
shock distance
double ear effect