采掘动载应力波特征及其诱发断层冲击地压机制研究
批准号:
52104204
项目类别:
青年科学基金项目(C类)
资助金额:
30.0 万元
负责人:
李学龙
依托单位:
学科分类:
安全科学与工程
结题年份:
2024
批准年份:
2021
项目状态:
已结题
项目参与者:
李学龙
中文摘要
采动诱发煤矿断层冲击地压愈发严重和复杂,探讨采掘动载应力波诱发断层冲击地压的机制是当前煤炭开采中亟需解决的科学问题。本项目研究煤岩破裂产生动载应力波的波形特征(振幅、频率、持续时间、能量),分析其与煤岩体岩性、破裂类型、微观形貌、裂纹扩展形态和尺度的相关性,得到其主要影响因素;利用煤系地层断层发育地质力学试验系统,研究采掘动载应力波在煤系地层的传播衰减规律,探究其对断层区域构造-采动叠加应力场和能量传递的影响规律,确定采掘动载应力波导致断层活化的“时-空-能”临界条件;构建断层活化动载应力波诱发冲击地压的理论模型,揭示采掘动载应力波与断层活化动载应力波之间的互动机制;结合现场监测和数值模拟,研究断层特性对断层活化动载应力波传播衰减、煤岩应力分布及采场稳定性的影响,阐明断层活化动载应力波诱发冲击地压的动力学过程。研究成果对深入认识采掘诱发断层冲击地压的机理及防治具有重要理论和实用价值。
英文摘要
Coal mine fault rock burst induced by mining becomes more serious and complex. It is an urgent scientific problem to explore the mechanism of fault rock burst induced by mining dynamic stress wave in the current coal mining engineering. This project will study the characteristics (amplitude, frequency duration and energy) of dynamic stress wave generated by coal rock fracture, and analyze their correlation with coal rock lithology, fracture type, microstructure, crack propagation morphology and scale, and then obtain the main influencing factors. Based on the geomechanical test system of fault development in coal measures strata, this project will study the propagation and attenuation law of mining dynamic stress wave in coal measure strata and its influence on tectonic stress and energy transfer in fault area, and determine the "time-space-energy" critical condition of fault activation caused by dynamic stress wave. Besides, the project will establish the theoretical model of rock burst induced by fault activation dynamic stress wave, construct the theoretical model of rock burst induced by dynamic stress wave generated by fault activation, reveal the interaction mechanism between mining dynamic stress wave and fault activation dynamic stress wave. Combined with field monitoring and numerical simulation, the project will explore the influence of fault characteristics on propagation and attenuation of fault activation dynamic stress wave, coal stress distribution and stope stability, so that reveal the dynamic mechanism of rock burst induced by fault activation dynamic stress wave. The research results have important theoretical and practical value for further understanding the mechanism and prevention of fault rock burst induced by dynamic stress wave.
冲击地压是严重的煤岩动力灾害,断层是煤矿中常见的地质构造,采掘活动容易诱发断层冲击地压,当前对采掘导致断层活化产生动载应力波诱发冲击地压的动力学过程研究还不充分。本项目研究了小尺度含裂隙(断层结构面)煤岩失稳破坏的形态特征,不同裂隙倾角煤岩的应力应变和能量演化特征,并且针对裂隙煤岩失稳破坏过程的应力波频谱和能量特征进行了研究,得到了影响煤岩失稳破坏产生应力波的主要因素;研究得到了动载应力波在煤系地层的传播衰减规律,冲击地压演化过程中微震波形的主频降低,幅值呈线性递增,发现诱发冲击地压的震源多为远程震源;测试了鲁西地区深部冲击地压矿井地应力的分布规律,采用结构动力学理论,从共振角度研究了应力波对煤岩体稳定性的影响,解释了远场震源导致冲击地压的原因,越靠近巷道表面或断层面,煤岩体月破碎,应力波越易与煤岩体发生共振效应,煤岩越容易发生结构失稳破坏,临近冲击失稳时,煤岩破裂从小尺寸串级过渡到大尺寸串级,波形的相似度及关联性也越来越大,波形的瞬时能量能够更明确体现应力波的累积损伤作用。建立了基于微震能量和频率的“双高”风险评价指标体系和基于优化线性加权模型的煤层冲击危险性综合评价方法。利用煤系地层断层发育地质力学试验系统,揭示了正断层形成过程中的应力及声发射能量演化特征,得到了正断层形成后断层区域的应力场及位移场分布规律。明确了正断层构造应力对断层保护煤柱稳定性的影响规律,揭示了构造应力与采动应力波影响下正断层保护煤柱的失稳破坏特征。相关研究为断层冲击地压的有效防治提供了科学指导。
厚硬顶板高静载流变条件下扰动破断诱发塌陷型矿震机理研究
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批准号:52574258
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项目类别:面上项目
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资助金额:50.00万元
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批准年份:2025
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负责人:李学龙
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依托单位:
国内基金
海外基金