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防冲击煤柱宽度变化期间微震活动规律研究

Study on microseismic activity law during change of anti-rockburst coal pillar width

  • 摘要: 为了研究呼吉尔特矿区冲击地压矿井煤柱宽度转换过渡初期微震事件时空活动规律,以门克庆煤矿3102工作面原宽35 m煤柱向宽120 m防冲煤柱过渡为背景,确定了宽120 m煤柱的防冲有效性并提出了过渡期间冲击地压综合防治措施。研究结果表明:受坚硬顶板、煤柱宽度变化的影响,煤柱宽度过渡期间大能量微震事件频发,但宽120 m防冲煤柱对顶板的承载作用能对本工作面及相邻工作面采空区进行阻隔,煤柱宽度过渡期内的微震事件主要集中于3102工作面内并略向煤柱区域偏移;对过渡期内的微震事件分析发现,大能量微震事件(≥105J)分布高度呈下降趋势,由高程+650 m逐渐下移至+620 m,从中高位的粗砂岩顶板转移至中低位的中砂岩顶板;高能量微震事件(103~105J)分布高度由高程+615 m上移至高程+625 m,中低位的中砂岩顶板活动加剧,震源高度呈上升趋势;低能量微震事件(<103J)分布高度由高程+615 m下移至+603 m左右,小能量震动逐渐向煤层转移;采用震源机制解对煤柱过渡期内的9次大能量事件的破裂方式、角度以及破裂半径进行分析,推测工作面震源连接线可能为一条弧形破裂带。提出了工作面煤柱宽度过渡期间的冲击地压综合防治措施,为其他类似条件下的矿井生产提供了经验。

     

    Abstract: In order to study the temporal and spatial activity law of microseismic events in the initial stage of coal pillar transformation transition in Hujlte Mining Ar ea,taking the original 35 m coal pillar to 120 m anti scour coal pillar in No.3102 working face of menkeqing coal mine as the background,the anti-rockburst effectiveness of 120 m coal pillar is determined, and the comprehensive prevention and control measures of rock burst during the transition period are proposed. The results show tha t: under the influence of the width change of hard roof and coal pillar,large energy microseismic events occur frequently during the transition period of coal pillar width,b ut the bearing effect of 120 m anti-rockburst coal pillar on the roof can block the goaf of this working face and adjacent working face. The microseismic events in the tra nsition period of coal pillar width mainly concentrated in No.3102 working face and slightly shifted to the coal pillar area.lt is found that the distribution height of high-en ergy microseismic events( 2105 J) shows a downward trend from +650 m to +620 m,and the distribution height of high-energy microseismic events( 103~ 105 J) increa ses from+ 615 m to + 625 m,and the activity of medium low-level medium sandstone roof is intensified and the focal height is up The results show that the distribution h eight of low-energy microseismic events(

     

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