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| Mechanisms of rock burst instability in deep coal roadway with high three-way stress difference area |
| LIU Guolei1,LIANG Wenzhao2,3,MA Qiufeng1,WANG Zedong4,QU Xiaocheng5 |
(1. School of Resources and Environmental Engineering,Shandong University of Technology,Zibo,Shandong 255022,China;2. State Key Laboratory for Tunnel Engineering,China University of Mining and Technology(Beijing),Beijing 100083,China;
3. School of Mechanics and Civil Engineering,China University of Mining and Technology(Beijing),Beijing 100083,China;
4. School of Emergency Management and Safety Engineering,China University of Mining and Technology(Beijing),Beijing 100083,China;5. Beijing Anke Xingye Technology Co.,Ltd.,Beijing 100083,China) |
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Abstract Addressing the issue of rock bursts and instability in deep coal roadways with high three-way stress differences,this study employs theoretical analysis,numerical simulations,and engineering case studies to reveal the mechanisms of rock bursts and instability in such areas. Based on the Mohr-Coulomb criterion,the definition of the three-way stress difference is modified to ,providing a quantitative damage criterion for coal body units. High three-way stress differences in deep coal mines are categorized into horizontal tectonic stress type and vertical stress type based on their origins. After roadway excavation in high-stress difference areas,the coal rib experiences significant crack development and increased damage extent. Additionally,there are higher movement speeds,larger displacements,and faster destruction rates. The peak value of the three-way stress difference,distributed radially around the surrounding rock,defines the interface between the failure and non-failure zones. The failure zone suppresses the increase in three-way stress difference in the non-failure zone,while the three-way stress difference distribution in the non-failure zone plays a dominant role in controlling the stability of the coal roadway. A stability parameter,Ss,is proposed to describe the stability of the surrounding rock of coal roadways or in unexcavated coal configuration areas. When the surrounding rock's Ss is less than the critical [Ss] of the non-failure zone boundary,accumulated deformation in the non-failure zone drives coal from the failure zone towards the roadway,leading to instability. When Ss decreases sharply,the non-failure zone rapidly fails,and significant deformation accumulation drives the coal body in the failure zone to experience a rock burst. This mechanism is validated through a case study of a rock burst incident in the high three-way stress area formed by a coal pillar at the Huafeng coal mine.
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