深部开采诱发煤与瓦斯突出的煤体失稳机制

Mechanism of coal instability of coal and gas outburst induced by deep mining

  • 摘要:
    目的 随着浅部煤炭资源逐渐枯竭,深部复杂开采环境显著增大了煤与瓦斯突出的危险性和危害程度,亟需探究深部开采条件下煤体力学失稳机制,指导深部煤矿安全开采。
    方法 采用物理试验、数值模拟和理论分析相结合的手段,开展500、1 000和1 600 m不同深度条件下煤与瓦斯突出物理模拟试验,建立煤体变形场、瓦斯流动场和煤体损伤场的多场耦合模型,揭示深部开采条件下突出煤体力学失稳机制。
    结果和结论 (1) 突出物理模拟试验结果表明,随埋深增加,煤层卸压速度加快,相对突 出强度分别增大至29.05%、38.05%和42.70%;同时,突出后煤层温度降幅更为显著,最大温降分别到达0.17、0.37和0.55 ℃;突出煤粉运移速度也更高,速度峰值分别为22.08、22.87和26.58 m/s。整体上,埋深越大,突出动力现象越强。(2) 突出数值模拟发现,随着侧压系数降低和瓦斯压力升高,煤体损伤区域由半圆形演变为蝶形,并主要沿垂直方向扩展;损伤孔洞偏转角增大,分别为8.1°、19.0°和34.4°。在埋深1 000和1 600 m时,渗透率最大值均出现在暴露面处,分别是初始渗透率的10.8倍和47.5倍;同时,暴露面处存在最大渗透力,且随埋深增加而增大,依次为3.62、7.74和11.93 MPa/m。(3) 根据开采由中深部向特深部转变过程中垂直应力、渗透率与渗透力的变化特征,将煤层划分为快速变化区、波动变化区和稳定不变区。在深部开采条件下,高地应力与高压瓦斯以高垂直应力和高渗透力的形式作用于煤体,导致煤体破坏、塑性区域扩大,并显著增加突出危险性。(5) 进一步基于深部煤体力学特性分析,探讨了煤与瓦斯突出在准备、激发、发展、终止4个阶段的力学演化过程,系统阐明了高地应力和高渗透力联合主导的深部煤体失稳机制,为深部煤与瓦斯突出的力学演化过程提供了新的理论视角。针对深部煤体损伤特征和波动区的高渗透力特性,深部防突工程应重点强化立体卸压增透措施,打破应力集中与高压瓦斯积聚的耦合环境,降低波动区的突出能量。

     

    Abstract:
    Objective With the gradual depletion of shallow coal resources, the complex deep mining environment has significantly increased the risk and severity of coal and gas outburst. It is urgent to investigate the mechanical instability mechanism of coal under deep mining to ensure the safe mining of deep coal seams.
    Methods A combination of physical experiments, numerical simulations, and theoretical analyses was adopted to conduct physical simulation tests of coal and gas outbursts at different burial depths of 500 , 1000  and 1600 m. A multi-field coupling model of coal deformation field, gas flow field, and coal damage field was established to reveal the mechanical instability mechanism of outburst coal under deep mining conditions.
    Results and Conclusions  (1) Physical simulation results of outbursts showed that with increasing burial depth, the pressure relief rate of coal seams accelerated, and the relative intensity of outburst increased to 29.05%, 38.05% and 42.70%, respectively. Meanwhile, the temperature drop of coal seams after outbursts became more significant, with maximum temperature reductions reaching 0.17 , 0.37 and 0.55  ℃, respectively. The migration velocity of outburst coal particles was also higher, with peak velocities of 22.08, 22.87 and 26.58 m/s, respectively. Overall, a greater burial depth corresponded to a stronger dynamic outburst phenomenon. (2) Numerical simulations of outbursts revealed that with a decreasing lateral pressure coefficient and increasing gas pressure, the coal damage zone evolved from a semicircular shape to a butterfly shape and propagated mainly in the vertical direction. The deflection angle of the damage cavity increased to 8.1°, 19.0° and 34.4°, respectively. At burial depths of 1000  and 1600 m, the maximum permeability appeared at the exposed face, which was 10.8 and 47.5 times the initial permeability, respectively. Meanwhile, the maximum seepage force existed at the exposed face and increased with burial depth, reaching 3.62 , 7.74  and 11.93 MPa/m, respectively. (3) According to the variation characteristics of vertical stress, permeability, and seepage force during the transition from medium-deep to ultra-deep mining, coal seams can be divided into rapid change zone, fluctuation change zone, and stable zone. Under deep mining conditions, high in-situ stress and high gas pressure acted on coal in the form of high vertical stress and high seepage force, causing coal failure, expansion of the plastic zone, and a significant increase in outburst risk. Furthermore, based on the analysis of mechanical properties of deep coal, the mechanical evolution process of coal and gas outbursts in four stages (preparation, initiation, development, and termination) was discussed, and the mechanical instability mechanism of deep outburst coal was revealed.

     

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