浅埋深交错煤层群覆岩运动规律及复合采空区自燃“三带”研究

    Research on overburden movement laws and spontaneous combustion “three zones” of composite goaf in shallow buried depth and stereo-intersected coal seam group

    • 摘要: 为深入探讨煤层群开采对覆岩运动规律及煤层自燃风险的影响,以大柳塔活鸡兔井12204与22206复合采空区为研究对象,系统研究煤层群开采导致的覆岩运动及地表沉陷特征,同时结合数值模拟,进一步认识复合采空区煤自燃风险。通过理论计算与无人机实测相结合的方法,对复合采空区的地表沉陷情况进行了全面评估,并利用三维离散元仿真软件3DEC模拟了复合煤层开采对覆岩运动的影响规律;同时,通过仿真结果验证模型精度,并结合Fluent软件,引入耗氧函数,进一步细化复合采空区自燃“三带”划分,分析了氧化带的空间分布特征及其对煤自燃风险的影响。理论计算结果显示:12204工作面重新压实区的地表最大沉陷量为3.54 m,22206工作面重新压实区的地表最大沉陷量为1.06 m。无人机实测结果表明:在采空区重叠区域,地表沉陷量高达5 m。模拟数据表明:煤层群开采的重叠区域地表沉陷系数为0.24,而下煤层煤柱上方的沉陷系数仅为0.12,煤层群开采导致的地表沉陷量为单层煤层开采的2倍;此外,下层煤层回采后覆岩会经历二次挤压变形,其垮落角较初次变形减小约9°。基于Fluent软件的氧气场模拟显示:下煤层进风侧的氧化带宽度约143 m,回风侧氧化带宽度为50 m,而上、下煤层底板氧化带的面积分别为26 676 m2和24 003 m2,表明上煤层的自燃风险更高,高氧区域主要集中在进风侧及裂隙发育区域。

       

      Abstract: To thoroughly investigate the effects of coal seam group mining on overburden movement and coal spontaneous combustion risks, this study focuses on the composite goaf of the 12204 and 22206 working faces in Daliuta Huojitu Mine; this study systematically studies the overburden movement and surface subsidence characteristics induced by coal seam group mining and further finds out the risk of coal spontaneous combustion risks in the composite goaf by integrating numerical simulations. Theoretical calculation combining with UAV-based measurements are used to comprehensively assess surface subsidence in the composite goaf. The study employed 3DEC numerical simulation software to simulate the impacts of composite coal seam mining on overburden movement. Simulation results were validated using surface subsidence data, and the Fluent software was utilized to refine the delineation of the spontaneous combustion “three zones” in the composite goaf by incorporating an oxygen consumption function. This facilitated an in-depth analysis of the spatial distribution characteristics of the oxidation zone and its implications for coal spontaneous combustion risks. Theoretical calculations revealed that the maximum surface subsidence in the recompaction zones of the 12204 and 22206 working faces was 3.54 m and 1.06 m, respectively. UAV-based differential elevation measurements indicated that the surface subsidence in the overlapping goaf region reached up to 5 m. Simulated data showed that the surface subsidence coefficient in the overlapping region of the coal seam group mining was 0.24, whereas the coefficient above the coal pillars in the lower coal seam was only 0.12. The surface subsidence caused by coal seam group mining was double that of single-seam mining. Furthermore, after the lower coal seam was mined, the overburden experienced secondary compressive deformation, with the caving angle reduced by approximately 9° compared to the initial deformation. The oxygen field simulation using Fluent demonstrated that the oxidation zone width on the intake side of the lower coal seam was approximately 143 m, while that on the return side was about 50 m. The oxidation zone areas of the upper and lower coal seam floors were 26 676 m2 and 24 003 m2, respectively, indicating a higher risk of spontaneous combustion in the upper coal seam. High oxygen volume fraction zones were primarily concentrated on the intake side and in fracture-developed areas.

       

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