Stress Transfer Law of the Floor of Overlying Residual Coal Pillars and Roadway Surrounding Rock Deformation and Support Technology When Crossing Residual Coal Pillars

IF 1.3 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Geofluids Pub Date : 2026-09-26 DOI:10.1155/gfl/7067361
Peng Sun, Hao Lan, Jing Chai, Dingding Zhang, Jianfeng Yang, Wenli Ji, Yongliang Liu, Kuiying Gao
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Abstract

To address severe mining hazards such as intense ground pressure, roof fragmentation, and support instability encountered when longwall faces pass beneath residual coal pillars in close-proximity coal seams, this study investigates the mining conditions of an inclined residual coal pillar in a shallow-buried, close-spaced coal seam at the Daliuta Coal Mine in the Shendong Mining Area. A comprehensive approach integrating theoretical analysis, numerical simulation, fiber-optic monitoring, and field measurements was employed to investigate the stress evolution of surrounding rock and mining-induced pressure response. A floor stress transfer model beneath the upper residual coal pillar was established, revealing stress transmission characteristics into the underlying strata, and numerical simulations confirmed that the stress-enhanced zone exhibits an ellipsoidal distribution and gradually attenuates with depth. Full-process simulations of the working face during the “entry–passage–exit” stages showed that stress concentration on the right side of the pillar consistently exceeded that on the left, whereas horizontal stress in the underlying coal wall increased with advance distance and peaked during the exit stage. The maximum stress concentration reached 12.83 MPa in the pillar and 15.74 MPa in the lower coal seam. Meanwhile, the peak advance abutment pressure increased from 6.47 MPa during the entry stage to 11.44 MPa during the exit stage, following the pattern of “exit > passage > entry.” Fiber-optic borehole monitoring indicated that the stress peak beneath the residual coal pillar reached 2.72 MPa, significantly higher than that beneath the goaf, and exhibited a dynamic “rise–peak–fall” evolution. Field monitoring further confirmed that the exit stage represents the most critical risk zone, with hydraulic support resistance peaking at 18,455 kN per support and a maximum pressure influence range of 7.5 m. Finally, integrating the theory of rock beam structures in shallow-buried coal seams, this study proposes that the rated working resistance of supports during the coal pillar extraction phase should not be less than 15,000 kN per frame. It further recommends implementing proactive control measures such as coal pillar reinforcement support to enhance load transfer. This study systematically elucidates the dynamic stress response mechanism of surrounding rock during the process of mining through residual coal pillars in close-to-the-face coal seams. It identifies the characteristics of intense mining pressure and key prevention and control priorities during the coal pillar extraction phase, providing theoretical foundations and engineering practice references for safe and efficient mining in similar geological conditions.

上覆残余煤柱底板应力传递规律及穿越残余煤柱巷道围岩变形与支护技术
针对近距离煤层中长壁工作面经过残余煤柱下方时遇到的强地压、顶板破碎、支护失稳等严重开采危害,对神东矿区大柳塔煤矿浅埋紧密煤层倾斜残余煤柱的开采条件进行了研究。采用理论分析、数值模拟、光纤监测和现场测量相结合的综合方法,研究了采场围岩应力演化及采动压力响应。建立了上部残余煤柱下底板应力传递模型,揭示了应力向下伏地层传递的特征,数值模拟证实了应力增强区呈椭球状分布,并随深度逐渐衰减。工作面“进-通-出”阶段全过程模拟表明,矿柱右侧应力集中始终大于左侧应力集中,下伏煤壁水平应力随推进距离增大而增大,并在出煤阶段达到峰值。顶柱最大应力集中达到12.83 MPa,下煤层最大应力集中达到15.74 MPa。同时,超前桥台压力峰值从进入阶段的6.47 MPa增加到退出阶段的11.44 MPa,呈现出“出口>;通道>;进入”的规律。光纤钻孔监测结果表明,残余煤柱下方应力峰值达到2.72 MPa,显著高于采空区下方应力峰值,并呈现出“升-峰-降”的动态演化规律。现场监测进一步证实,出口阶段是最关键的风险区域,液压支架阻力峰值为每个支架18,455 kN,最大压力影响范围为7.5 m。最后,结合浅埋煤层岩梁结构理论,提出煤柱抽采阶段支架的额定工作阻力应不小于15,000 kN /架。它进一步建议实施主动控制措施,如煤柱加固支持,以加强负荷转移。本研究系统地阐明了近工作面煤层残余煤柱开采过程中围岩的动应力响应机制。明确了煤柱回采阶段开采压力大的特点和重点防治重点,为类似地质条件下的安全高效开采提供了理论基础和工程实践参考。
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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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