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近距离煤层开采上覆采空区岩层二次活化机制研究OA

Study on the secondary activation mechanism of overlying goaf strata in close distance coal seam mining

中文摘要英文摘要

近距离双层煤开采经常会引起地表的二次变形与沉降,上覆采空区也会对正在回采的下部工作面带来安全生产方面的问题为探究下部煤层开采期间,上覆采空区岩层二次活化破断特征规律及其对下部工作面带来的影响,以西北地区某煤矿近距离双煤层开采为背景,运用微震分析、数值模拟和相似模拟试验等方法对下部煤层开采期间上覆采空区顶板岩层二次活化机制进行了研究.研究发现:回采初期微震事件主要集中在 317 工作面顶板上方低位岩层中,至317 工作面回采中期,微震事件密集区发展到了 221 工作面及其上方粗粒砂岩中,可见微震事件有向高位岩层发展的趋势;受 317 工作面采动影响,221 采空区顶板活化破断高度有所增加,上位基本顶弯曲下沉加大,顶板二次活化高度从上部采空区垮落稳定到基本稳定增加 10 m 左右,上覆岩层初步表现出"初活化—稳定—再活化"的模式.相似模拟试验表明,221 工作面回采后,直接顶垮落,上覆破断顶板范围内岩层重量作用于工作面底板;随 317 工作面推采,221 采空区顶板进一步弯曲下沉,上下两采空区空间导通并重叠,221 工作面顶板二次破断、垮落,破断后的岩块相互挤压铰接,随着工作面的推进,基本顶和直接顶挤压成一个整体,呈现出"初活化—稳定—再活化"模式.

Mining of close distance double coal seams often causes secondary deformation and subsidence of the ground surface,and the overlying goaf also brings safety production problems to the lower working face being mined.To investigate the characteristics and laws of the secondary activation and fracture of the overlying goaf strata and their impacts on the lower working face during the mining of the lower coal seam,taking the mining of close distance double coal seams in a coal mine in Northwest China as the back-ground,the secondary activation mechanism of the roof strata in the overlying goaf during the mining of the lower coal seam was studied by means of microseismic analysis,numerical simulation and similar simulation tests.The results show that:in the initial mining stage,micro-seismic events were mainly concentrated in the lower strata above the roof of the 317 working face,and in the middle mining stage of the 317 working face,the dense area of micro-seismic events developed to the 221 working face and the coarse-grained sandstone above it,indicating that micro-seismic events tend to develop toward higher strata.Affected by the mining of the 317 working face,the activation and fracture height of the roof in the 221 goaf increased,the bending and subsidence of the upper main roof intensified,and the secondary activation height of the roof increased by about 10 m from the caving stability to the basic stability of the upper goaf,and the overlying strata initially showed a"primary activation-stability-reactivation"mode.Simil-ar simulation tests show that after the mining of the 221 working face,the immediate roof caved,and the weight of strata within the range of the overlying fractured roof acted on the floor of the working face.With the advance of the 317 working face,the roof of the 221 goaf further bent and subsided,the spaces of the upper and lower goafs were connected and overlapped,and the roof of the 221 working face was secondarily fractured and caved.The fractured rock blocks were mutually extruded and hinged,and with the ad-vance of the working face,the main roof and the immediate roof were extruded into an integral body,presenting the"primary activa-tion-stability-reactivation"mode.

刘云;李慧

太原理工大学 矿业工程学院,山西 太原 030024太原理工大学 矿业工程学院,山西 太原 030024

矿业与冶金

微震监测岩层二次活化数值模拟冲击地压地表沉陷

micro-seismic monitoringsecondary activation of stratanumerical simulationrock burstsurface subsideuce

《煤矿安全》 2026 (4)

96-108,13

国家自然科学基金资助项目(52474139,52474107)

10.13347/j.cnki.mkaq.20250371

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