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赵鹏翔,王玉龙,李树刚,等. 倾斜厚煤层仰斜综采工作面覆岩瓦斯缓渗区分域方法及分形特征研究[J]. 煤炭科学技术,2023,51(S2):1−13. doi: 10.13199/j.cnki.cst.2022-1444
引用本文: 赵鹏翔,王玉龙,李树刚,等. 倾斜厚煤层仰斜综采工作面覆岩瓦斯缓渗区分域方法及分形特征研究[J]. 煤炭科学技术,2023,51(S2):1−13. doi: 10.13199/j.cnki.cst.2022-1444
ZHAO Pengxiang,WANG Yulong,LI Shugang,et al. Division method and fractal characteristics of overburden gas slow permeability zone in up-dip fully mechanized face of inclined thick coal seam[J]. Coal Science and Technology,2023,51(S2):1−13. doi: 10.13199/j.cnki.cst.2022-1444
Citation: ZHAO Pengxiang,WANG Yulong,LI Shugang,et al. Division method and fractal characteristics of overburden gas slow permeability zone in up-dip fully mechanized face of inclined thick coal seam[J]. Coal Science and Technology,2023,51(S2):1−13. doi: 10.13199/j.cnki.cst.2022-1444

倾斜厚煤层仰斜综采工作面覆岩瓦斯缓渗区分域方法及分形特征研究

Division method and fractal characteristics of overburden gas slow permeability zone in up-dip fully mechanized face of inclined thick coal seam

  • 摘要: 为研究倾斜厚煤层仰斜综采工作面覆岩瓦斯缓渗区的分域方法及分形特征,以分形理论和灰色理论为基础,采用平面物理相似模拟试验方法,开展了仰斜综采工作面覆岩瓦斯缓渗区裂隙演化规律研究,得到了覆岩瓦斯缓渗区的动态扩展规律,进而构建了覆岩瓦斯缓渗区精细分域方法,并采用灰色关联分析方法对覆岩瓦斯缓渗区沿横向(工作面推进方向)和纵向(垂直于煤层底板向上方向)分形维数与离层量、破断裂隙密度及应力集中系数之间的最大关联度分别进行确定。研究结果表明:覆岩瓦斯缓渗区在第一次周期来压后初步形成,其后每次周期来压时,覆岩瓦斯缓渗区两侧的垮落角均不断减小而宽度和高度均不断增大。具体表现为从缓渗区初次形成至缓渗区充分发育期间,缓渗区开切眼侧和工作面侧的垮落角分别从68.3°和76.2°减小到44.7°和53.5°;而缓渗区的宽度和高度分别从16.3 m和19.2 m增大到52.1 m和38.4 m。根据建立的覆岩瓦斯缓渗区分域准则及流程,结合灰色关联分析方法,得到覆岩瓦斯缓渗区沿横向和纵向分形维数变化均与离层量变化相关性最强( r_1 =0.93, r_1^ * =0.91),并通过试验验证了理论计算的准确性。因此,在后期确定卸压瓦斯抽采钻孔(巷道)终孔(巷)时,可通过现场观测离层量对覆岩瓦斯缓渗区边界进行判断,研究结果对采空区卸压瓦斯精准高效抽采具有一定的指导意义。

     

    Abstract: In order to study the division method and fractal characteristics of the overburden gas slow permeability zone in up-dip fully mechanized face of inclined thick coal seam, based on the fractal theory and grey theory, the plane physical similarity simulation experiment was used to study the crack evolution law of the overburden gas slow permeability zone in up-dip fully mechanized face. The dynamic expansion law of the overburden gas slow permeability zone was obtained, and then the division method of the overburden gas slow permeability zone was constructed. The grey correlation analysis method was used to determine the maximum correlation degree between the horizontal direction (the advancing direction of the working face) and vertical direction (perpendicular to the upward direction of the coal seam floor) fractal dimensions of the overburden gas slow permeability zone and the separation amount, the fracture density and the stress concentration coefficient. The results show that the overburden gas slow permeability zone is initially formed after the first periodic weighting. After each periodic weighting, the caving angle on both sides of the overburden gas slow permeability zone decreases continuously and the width and height increase continuously. Specifically, from the initial formation of the slow permeability zone to the full development of the slow permeability zone, the caving angles of the open-off cut side and the working face side of the slow permeability zone are reduced from 68.3° and 76.2° to 44.7° and 53.5° respectively. The width and height of the slow permeability zone increased from 16.3 m and 19.2 m to 52.1 m and 38.4 m respectively. According to the established division criterion and process of the overburden gas slow permeability zone, combined with the grey correlation analysis method, it is obtained that the variation of fractal dimension along the horizontal and vertical directions of the overburden gas slow permeability zone has the strongest correlation with the variation of the separation amount ( r_1 =0.93, r_1^ * =0.91), and the accuracy of theoretical calculation is verified by experiments. Therefore, when the final hole (roadway) of pressure relief gas extraction borehole (roadway) is determined in the later stage, the boundary of the overburden gas slow permeability area can be judged by field observing the separation amount. The research results have certain guiding significance for accurate and efficient extraction of pressure relief gas in goaf.

     

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