Microseismic monitoring and numerical simulation of the formation of water inrush pathway caused by coal mining
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摘要:
以某礦綜放工作面開采過程為背景,利用微震監測技術進行現場監測,并借助有限差分FLAC3D進行數值分析,研究在采動應力場不斷變化過程中底板巖體微震破裂事件的時空演化規律,揭示煤層采動條件下潛在導水通道的孕育、發展和貫通過程.微震監測結果表明:微震事件數一定程度上反映了開采擾動對底板巖體破壞程度的影響;采煤期間,回采工作面附近微震事件呈現密集分布,底板巖體采動破壞嚴重,底板破裂深度達15 m.數值分析表明:由于煤層采動導致采場周圍應力重分布,工作面前方應力增高,采空區下方應力降低,底板巖體隨工作面回采經歷了應力集中、釋放并最終破壞;底板塑性破壞區深度達14 m.
Abstract:Based on the condition of a fully-mechanized working face, two research means, i. e. microseismic monitoring and FLAC3D numerical simulation, were introduced to study the formation and evolution of floor failure and water conducted pathways caused by coal mining. The space-time evolution law of microseismic rupture events was studied for the floor rock mass during the changing process of the mining stress field. The process of inoculation, development and penetration of potential water channels was also revealed under the condition of coal mining. Field microseismic monitoring shows that microseismic event accumulation is directly proportional to drilling footage. The number of microseismic events to some extent reflects the disturbance degree of mining activities on the floor rock. The distribution of microseismic events is intensive near the coal mining face, which shows that the floor rock mass is seriously damaged during coal mining. The greatest failure depth of the floor estimated from mine microseismic monitoring is 15 m. Numerical analysis indicates that due to mining disturbance effect, the rock stress around the mine stope is redistributed during coal mining. The abutment pressure increases in front of the coal mining face and the stress reduces in the mined areas. Stress concentration and release make contribution to the destroying of the floor rock. The maximum failure depth is up to 14 m calculated from numerical simulation.
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Key words:
- coal mining /
- disturbance /
- microseism analysis /
- numerical simulation /
- water inrush
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