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现代矿业 ›› 2026, Vol. 42 ›› Issue (09): 165-170.

• 岩土工程 • 上一篇    下一篇

深部厚表土薄基岩覆岩破断特征数值模拟与微震监测验证

孔 震1 袁腾飞1 原培轩2 张航瑞2 沈振强2   

  1. 1. 兖煤菏泽能化有限公司赵楼煤矿;2. 中国地质大学(武汉)工程学院
  • 出版日期:2026-09-25 发布日期:2026-10-13

Numerical Simulation and Microseismic Monitoring Verification of Fracture Characteristics of Thick Topsoil and Thin Bedrock Overburden Rock in Deep Mine

KONG Zhen1 YUAN Tengfei1 YUAN Peixuan2 ZHANG Hangrui2 SHEN Zhenqiang2   

  1. 1. Zhaolou Coal Mine,Yanmei Heze Energy and Chemical Co.,Ltd.; 2. Faculty of Engineering,China University of Geosciences,Wuhan
  • Online:2026-09-25 Published:2026-10-13

摘要: 针对深部矿井厚表土薄基岩地层开采易出现区域性剧烈矿压显现的工程难题,以赵 楼煤矿 7303 工作面为研究对象,综合采用数值仿真与 KJ551 微震现场监测手段,系统分析工作面 回采全过程覆岩分阶段破断演化规律及采动垂直应力响应特征。数值模型复现不同推进距离下 直接顶、多层关键层弯曲离层与垮落全过程,模拟结果显示,工作面推进 20 m 时,直接顶初次破断, 与现场实测 18 m 垮落步距基本一致,基本顶周期来压步距约 20 m,采空区两侧煤壁最大垂直应力 可达 37.5 MPa;现场微震监测表明,覆岩破裂最高发育至煤层上方 140 m,完全贯通 114 m 厚承载基 岩,上部巨厚表土荷载经破碎基岩向前方煤体、巷道传递,形成 7301、7303 复合采场整体性覆岩扰 动,微震密集区、高应力区与现场矿压显现位置高度吻合,验证了应力驱动覆岩破裂与矿压灾变的 联动机制。数值仿真与现场监测结果相互印证,证明模型可精准还原薄基岩地层覆岩运移与应力 重分布全过程,研究成果可为同类赋存条件矿井深部安全开采提供理论参考;同时 KJ551微震监测 系统在深部高地应力环境降噪能力存在短板,后续需研发智能降噪算法与井地协同监测方案,提 升预警精度。

关键词: 厚表土薄基岩, 覆岩破断, 应力演化, 微震监测, 数值模拟

Abstract: In view of the engineering problem that the mining of thick topsoil and thin bedrock strata in deep mines is prone to regional severe mine pressure behavior,the 7303 working face of Zhaolou Coal Mine is taken as the research object,and the numerical simulation and KJ551 microseismic field monitor⁃ ing methods are comprehensively used to systematically analyze the stage-by-stage fracture evolution law and mining vertical stress response characteristics of the overburden during the whole mining process of the working face. The numerical model reproduces the whole process of bending separation and caving of imme⁃ diate roof and multi-layer key strata under different advancing distances. The simulation results show that the immediate roof first breaks when the working face advances 20 m,which is basically consistent with the field measured 18 m caving step distance. The periodic weighting step distance of the basic roof is about 20 m,and the maximum vertical stress of the coal wall on both sides of the goaf can reach 37.5 MPa. The on-site microseismic monitoring shows that the maximum development of overburden fracture is 140 m above the coal seam,and the 114 m thick bearing bedrock is completely penetrated. The upper thick top⁃ soil load is transmitted to the front coal body and roadway through the broken bedrock,forming the overall overburden disturbance of 7301 and 7303 composite stopes. The microseismic intensive area and high stress area are highly consistent with the location of on-site mine pressure,which verifies the linkage mechanism of stress-driven overburden rock fracture and mine pressure disaster. The numerical simulation and field monitoring results confirm each other,which proves that the model can accurately restore the whole process of overburden rock migration and stress redistribution in thin bedrock strata. The research re⁃ sults can provide theoretical reference for deep safe mining of mines with similar occurrence conditions. At the same time,KJ551 microseismic monitoring system has shortcomings in noise reduction ability in deep high ground stress environment. In the future,it is necessary to develop intelligent noise reduction algo⁃ rithm and well-ground collaborative monitoring scheme to improve early warning accuracy.

Key words: thick topsoil and thin bedrock, overburden rock fracture, stress evolution, microseismic monitoring, numerical simulation