The Combined Effect of Stress Mutation and Displacement Evolution on Overlying Rock Collapse From Physical Experiment and Numerical Simulation Study

IF 1.2 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Geofluids Pub Date : 2026-04-12 DOI:10.1155/gfl/7729757
Gang Wang, Daixin Deng, Jing Liu
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Abstract

This study investigates the complex failure mechanisms of overlying strata deformation induced by longwall mining, with a focus on the 21221 mining face in Qianqiu mine. Combining physical similarity simulation and numerical analysis, the research analyzes the abrupt changes in stress and displacement within the overlying rock mass during mining face advancement. The results show that roof failure occurs periodically, with collapse height and area progressively increasing as the intact bearing zone shifts upward, exerting continuous pressure on the stope. Mining disturbance significantly affects the roof ~40 cm ahead of the working face, where deformation and collapse are governed by gravitational forces and rock lithology. The maximum principal stress concentrates at the goaf edges, and vertical stress mutation accurately indicates impending roof fracture locations. Critically, the failure of hard conglomerate layers triggers a strong regional mutation in the mining-induced stress field. These results provide important insights into the dynamic evolution and instability precursors of overlying strata in deep mining conditions.

Abstract Image

物理实验与数值模拟研究应力突变与位移演化对覆岩崩塌的联合影响
以千丘矿21221工作面为研究对象,研究了长壁开采覆岩变形的复杂破坏机理。采用物理相似模拟与数值分析相结合的方法,分析了采动工作面推进过程中上覆岩体内部应力和位移的突变规律。结果表明:顶板破坏是周期性发生的,随着完整承载区向上移动,顶板破坏高度和破坏面积逐渐增大,对采场产生持续的压力;采动扰动对工作面前方~40 cm顶板影响显著,顶板变形和塌陷主要受重力和岩石岩性控制。最大主应力集中在采空区边缘,垂向应力突变准确指示顶板即将破裂位置。重要的是,硬砾岩层的破坏会在采动应力场中引发强烈的区域突变。这些结果为深部开采条件下上覆岩层的动态演化和失稳前兆提供了重要的认识。
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来源期刊
Geofluids
Geofluids 地学-地球化学与地球物理
CiteScore
2.80
自引率
17.60%
发文量
835
期刊介绍: Geofluids is a peer-reviewed, Open Access journal that provides a forum for original research and reviews relating to the role of fluids in mineralogical, chemical, and structural evolution of the Earth’s crust. Its explicit aim is to disseminate ideas across the range of sub-disciplines in which Geofluids research is carried out. To this end, authors are encouraged to stress the transdisciplinary relevance and international ramifications of their research. Authors are also encouraged to make their work as accessible as possible to readers from other sub-disciplines. Geofluids emphasizes chemical, microbial, and physical aspects of subsurface fluids throughout the Earth’s crust. Geofluids spans studies of groundwater, terrestrial or submarine geothermal fluids, basinal brines, petroleum, metamorphic waters or magmatic fluids.
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