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    深部巨厚煤层强开采扰动下的采场底板应力传播规律

    Law of stress propagation in stope floor under strong mining disturbance in deep extra-thick coal seams

    • 摘要: 针对深部巨厚煤层强开采扰动下采场底板应力传播规律尚不明确的问题,以陕西彬长小庄矿业有限公司40205综放工作面为工程背景,综合采用相似材料模拟、现场实测与理论解析方法,系统揭示了巨厚关键层破断控制下的底板应力传播规律。研究结果表明,相似模拟实验揭示了底板应力随回采推进呈阶段性演化,应变呈“稳定区-集中区-稳定区”三段式分布格局,高位关键层破断诱发底板应变剧烈波动。现场实测表明,40205综放工作面周期来压呈现“大小周期交替”特征,该特征与实验揭示的关键层分级破断规律一致。理论分析进一步阐明了大周期来压下最大垂直应力较平静期增长108%,应力集中系数增至3.0~3.2,高应力区影响深度扩展至18 m。最终明确了高位亚关键层破断通过改变覆岩荷载传递路径,导致采场围岩应力壳偏移,从而增强底板应力扰动强度与深部传播范围的力学机制。研究结果可为强采动条件下底板隔水层破坏深度预测及巷道布置层位优化提供依据。

       

      Abstract: To address the insufficient understanding of floor stress propagation under intense mining-induced disturbance in deep, extra-thick coal seams, the 40205 fully mechanized top-coal caving working face at Xiaozhuang Coal Mine, operated by Shaanxi Binchang Xiaozhuang Mining Co., Ltd., was selected as the engineering background. Similar material simulation, field measurements, and theoretical analysis were integrated to systematically investigate floor stress propagation governed by the fracture of an extra-thick key stratum. The results indicate that floor stress exhibits a staged evolution with the advance of the working face, while floor strain displays a three-zone distribution pattern consisting of a stable zone, a concentration zone, and another stable zone. Furthermore, the fracture of the high-level key stratum induces pronounced fluctuations in floor strain. Field measurements reveal that periodic weighting at the 40205 working face is characterized by alternating major and minor weighting cycles, consistent with the hierarchical fracture behavior of key strata observed in the physical simulation. Theoretical analysis further demonstrates that, during major periodic weighting, the maximum vertical stress increases by 108% compared with that during relatively stable periods, accompanied by an increase in the stress concentration factor to 3.0–3.2 and an extension of the high-stress influence zone to a depth of 18 m. These findings elucidate the mechanical mechanism whereby the fracture of a high-level sub-key stratum alters the load transfer path of the overburden, resulting in the displacement of the stress shell within the surrounding rock and consequently intensifying floor stress disturbance and its downward propagation. The findings provide a theoretical basis for predicting the failure depth of floor aquicludes and optimizing roadway placement horizons under intense mining-induced disturbance.

       

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