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Study on Mechanism of Influence of Mining Speed on Roof Movement Based on Microseismic Monitoring

机译:基于微震监测的采矿速度对屋顶运动的影响机制研究

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摘要

Based on the study of the movement rule of the rock strata under the influence of the mining speed in the typical working face of Dongjiahe coal mine, the distribution of microseismic events and the variation characteristics of microseismic parameters in the slow and fast advancing stage are compared and analyzed, and the mechanism of the rock strata activity under the influence of the mining advancing speed is revealed from the perspective of the microfracture. The results show that the movement of the roof strata and the stress adjustment of surrounding rock have certain timeliness. The maximum advanced distance of microseismic events in the slow and fast stages is 185 m and 130 m, respectively, and the maximum lag distance of microseismic events in the goaf is 120 m and 180 m, respectively. The time of stress adjustment of surrounding rock is short, and the load transfer of the roof is insufficient. The advanced distance of microseismic events is increased, and the lag distance decreases. The percentage of microseismic events in the total number of events is 47% and 38%, respectively, in the slow and fast stages of advancing. With the increase of mining speed, the intensity of roof strata activity in the goaf is weakened. The rock failure decreases and the volume of broken block increases, and roof collapse and rotary subsidence are insufficient. During the nonpressure period, the maximum development elevation of microseismic events is +350 m and +300 m, respectively, in the slow and fast stages, while with the development elevation of microseismic events in the roof pressure near +390 m, increasing the mining speed cannot change the final failure height of the overburden. During the analysis period of roof pressure, the concentrated release of microseismic energy in the faster stage is 183% of that in the slower stage. The increase of large moment magnitude event frequency leads to the decrease of b value. The risk of roof instability and strata behavior increases.
机译:基于对岩石地区的运动规则的研究,在煤矿典型工作面上采矿速度的影响,比较了微震事件的分布和微震参数在缓慢和快速推进阶段的微震参数变化特征并分析,并从微膛的角度揭示了采矿前进速度影响下的岩石地层活动的机制。结果表明,屋顶地层的运动和周围岩石的应力调节具有一定的性质。慢速和快速阶段中微震事件的最大高级距离分别为185米和130米,并且POF中微震事件的最大滞后距离分别为120米和180米。周围岩石的压力调节时间短,屋顶的负载转移不足。微震事件的高级距离增加,滞后距离减小。事件总数的微震事件百分比分别为47%和38%,以慢速和快速的推进。随着采矿速度的增加,屋顶地层活性的强度被削弱。岩石破坏减小,断层块的体积增加,屋顶塌陷和旋转沉降不足。在不压期间,微震事件的最大开发升高分别为慢速和快速阶段,同时随着屋顶压力的显微震动事件的显影升高,越来越多,增加了采矿速度无法改变覆盖层的最终失败高度。在屋顶压力的分析期间,在更快的阶段中微震能浓缩释放是较慢的阶段的183%。较大的力矩幅度事件频率的增加导致B值的降低。屋顶不稳定和地层行为的风险增加。

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