动态和静态荷载下带隐蔽断层的地板涌水数值模拟和断裂力学模型分析

IF 2 3区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
Xianwei Zhao, Dengfeng Yang, Yanyan Zhu, Aiping Zeng
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引用次数: 0

摘要

隐伏断层在动静载荷作用下的开采活化是深部煤层开采发生底板涌水灾害的重要原因。通过数值模拟分析了隐伏断层底板开采引起的涌水通道的形成和演化机理,从断裂力学的角度构建了模型,探讨了动静联合载荷对裂隙水传播的影响。得出的结论是:开采应力和承压水的作用导致隐伏断层裂隙迅速扩展,渗透率显著提高,同时隐伏断层中的承压水对裂隙也有冲刷和扩展作用,加快了裂隙的发展速度。底板不同位置的隐伏断层的渗透规律存在时空差异,越靠近围岩,越容易发生隐伏断层活化和涌水。当地层中存在多个隐藏的小断层时,涌水增长区和水流稳定区之间会交替变化,具有相似的周期特征。动荷载的作用会增加裂缝中的孔隙压力,提高裂缝顶端的应力强度因子,更容易诱发裂缝扩展和贯穿破坏。推导了动荷载和静荷载作用下裂缝扩展和破坏的临界水压计算公式,进一步分析了楼板最小安全厚度的计算方法,讨论了水压、裂缝长度、倾角和开采深度对其的影响。动荷载的影响会增加裂缝中的孔隙压力,提高裂缝顶端的应力强度因子,更容易诱发裂缝扩展和贯穿破坏。最后,通过工程实例验证了理论分析结果。该研究成果可为预测和预防矿井底板涌水提供理论依据,有利于煤矿的安全和可持续开采。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Analysis on numerical simulation and fracture mechanics model of water inrush of floor with hidden faults under dynamic and static loads
The mining activation of hidden faults under dynamic and static loads is an important reason for the occurrence of floor water inrush disasters in deep coal seam mining. The formation and evolution mechanism of water inrush channel caused by mining on the floor of hidden faults were analyzed through numerical simulation, from the perspective of fracture mechanics, a model was constructed to explore the influence of combined dynamic and static loads on the propagation of water with cracks. A conclusion was drawn that the effects of mining stress and confined water have led to rapid expansion of hidden fault cracks and significant improvement in permeability, at the same time, the confined water in the hidden fault also has a scouring and expansion effect on the cracks, accelerating their development speed. There are spatial and temporal differences in the penetration patterns of hidden faults at different positions of floor, and the closer it is to the goaf, the more likely it is to experience activation of hidden faults and water inrush. When there are multiple hidden small faults in the floor, there is an alternating change between the water inrush growth area and the flow stable area with similar cyclic characteristics. The effect of dynamic load will increase the pore pressure in cracks, and increase the stress intensity factor at the crack tip, and more easily induce crack expansion and penetration failure. The critical water pressure calculation equation for crack propagation and failure under dynamic and static loads was derived, and the calculation method for the minimum safe thickness of the floor was further analyzed, the influence of water pressure, crack length, inclination angle, and mining depth on it was discussed. The effect of dynamic load will increase the pore pressure in cracks, and increase the stress intensity factor at the crack tip, and more easily induce crack expansion and penetration failure. Finally, the theoretical analysis results were verified by an engineering examples. The research results can provide theoretical basis for predicting and preventing water inrush from the mining floor, which is beneficial for the safe and sustainable mining of coal mines.
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来源期刊
Frontiers in Earth Science
Frontiers in Earth Science Earth and Planetary Sciences-General Earth and Planetary Sciences
CiteScore
3.50
自引率
10.30%
发文量
2076
审稿时长
12 weeks
期刊介绍: Frontiers in Earth Science is an open-access journal that aims to bring together and publish on a single platform the best research dedicated to our planet. This platform hosts the rapidly growing and continuously expanding domains in Earth Science, involving the lithosphere (including the geosciences spectrum), the hydrosphere (including marine geosciences and hydrology, complementing the existing Frontiers journal on Marine Science) and the atmosphere (including meteorology and climatology). As such, Frontiers in Earth Science focuses on the countless processes operating within and among the major spheres constituting our planet. In turn, the understanding of these processes provides the theoretical background to better use the available resources and to face the major environmental challenges (including earthquakes, tsunamis, eruptions, floods, landslides, climate changes, extreme meteorological events): this is where interdependent processes meet, requiring a holistic view to better live on and with our planet. The journal welcomes outstanding contributions in any domain of Earth Science. The open-access model developed by Frontiers offers a fast, efficient, timely and dynamic alternative to traditional publication formats. The journal has 20 specialty sections at the first tier, each acting as an independent journal with a full editorial board. The traditional peer-review process is adapted to guarantee fairness and efficiency using a thorough paperless process, with real-time author-reviewer-editor interactions, collaborative reviewer mandates to maximize quality, and reviewer disclosure after article acceptance. While maintaining a rigorous peer-review, this system allows for a process whereby accepted articles are published online on average 90 days after submission. General Commentary articles as well as Book Reviews in Frontiers in Earth Science are only accepted upon invitation.
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