Uniaxial Compression Response and Instability Mechanisms of Parallel Dual Coal Pillar–Roof Combinations

IF 1.2 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Geofluids Pub Date : 2025-08-05 DOI:10.1155/gfl/8842332
Jingkai Li, Chunge Li, Shengjian Zhao, Changde Yang, Kun Niu, Quancai Ji, Zhiqiang Wang
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Abstract

The remaining coal pillars and roof form an integral coal pillar–roof system (CPRS) that plays an important role in the safety of the room mining goaf. In this research, two different sets of parallel dual coal pillar–roof combinations (PDCRCs) were developed to model the CPRS. One set of PDCRC is formed by two-component combinations featuring identical mechanical properties, whereas another set is constituted by two-component combinations exhibiting distinct mechanical properties. Building upon this foundation, a sequence of uniaxial compression tests was carried out on PDCRC. These tests integrated laboratory experimentation and numerical simulation with the particle flow code (PFC). From both macroscopic and microscopic perspectives, the load-bearing capacities, acoustic emission (AE) features, crack development processes, force chain evolution laws, and deformation features of the PDCRC were recorded. The results indicate that the initial failure of a specific coal can trigger and dominate the instability of its corresponding combination, thereby leading to a chain instability in the other combination and the entire system. For PDCRC composed of two combinations with identical mechanical properties, the two combinations share the external load equally and fail in coordination. Once any component combination loses its ability to withstand the external load, the other component combination and the entire system will immediately and synchronously lose their load-bearing capacity. For PDCRC composed of two-component combinations with distinct mechanical properties, the component combination with low strength first fails and loses its load-bearing capacity, resulting in the synchronous transfer of the originally external load to the high-strength component combination. Once the high-strength component combination loses its load-bearing capacity, the entire system becomes unable to sustain the external load simultaneously. The overall load-bearing capacity of PDCRC with identical mechanical properties is approximately equal to the sum of the two-component combinations, while that of PDCRC with distinct mechanical properties is less than the combined total. In summary, the premature instability of certain coal pillars serves as the primary initiating factor for the instability of the CPRS. When conducting stability assessments of room mining goafs, it is essential to adopt a holistic perspective to comprehensively evaluate the load-bearing capacity of the CPRS as an integrated whole.

Abstract Image

平行双煤柱-顶板组合的单轴压缩响应及失稳机理
剩余煤柱与顶板构成了一个完整的煤柱—顶板系统,对空房采空区的安全起着重要的作用。在本研究中,建立了两组不同的平行双煤柱-顶板组合(PDCRCs)来模拟CPRS。一组PDCRC由具有相同力学性能的两组分组合组成,而另一组PDCRC由具有不同力学性能的两组分组合组成。在此基础上,对PDCRC进行了一系列单轴压缩试验。这些测试将实验室实验和数值模拟与粒子流代码(PFC)相结合。从宏观和微观两方面记录了PDCRC的承载能力、声发射特征、裂纹发展过程、力链演化规律和变形特征。结果表明,某一特定煤种的初始破坏可触发并主导其相应组合的失稳,从而导致另一组合乃至整个体系的链式失稳。对于由两种力学性能相同的组合组成的PDCRC,两种组合平均分担外载荷,协同失效。一旦任何组件组合失去承受外部载荷的能力,其他组件组合和整个系统将立即同步失去其承载能力。对于力学性能不同的双组份组合组成的PDCRC,低强度组份首先失效,失去承载能力,导致原有的外载荷同步转移到高强度组份组合。一旦高强度构件组合失去承载能力,整个系统就无法同时承受外部载荷。力学性能相同的PDCRC整体承载能力近似等于两分量组合之和,而力学性能不同的PDCRC整体承载能力小于两分量组合之和。综上所述,某些煤柱的过早失稳是CPRS失稳的主要起始因素。在对采空区进行稳定性评价时,必须从整体角度对采空区作为一个整体的承载能力进行综合评价。
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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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