Zhu Jie, Shao Tangsha, Li Guiyou, Yang Yuhang, Chen Zhen, Lan Tianxiang, Wang Jinge, Zhao Yuhan, Liu Shuangqing
School of Mechanics & Civil Engineering, China University of Mining & Technology (Beijing), Beijing 100083, China.
Materials (Basel). 2022 Jun 26;15(13):4500. doi: 10.3390/ma15134500.
Investigation on the pore-fracture features and crack propagation behavior of coal is necessary to prevent coal mine disasters. The pore structure features of coal samples taken from high gas seam were obtained by mercury injection porosimetry (MIP) and gas adsorption methods. The process of deformation and failure for coal samples under three-point bending conditions were obtained. The results demonstrate that the adsorption pores with diameter less than 100 nm are the most developed and their surfaces are the roughest (the average surface fractal dimension is 2.933). The surface of micro-cracks is smoother ( is 2.481), which is conducive to gas seepage. It may be the explanation for that 14-3# coal seam is a high gas seam, while there was almost no gas outburst accident so far. At the initial stage of crack propagation, the main crack on the coal sample expanded along the direction of the natural cracks. In the process of crack propagation, the surface fractal dimension of the main crack increased, suggesting that the bending degree of the main crack enhanced. The brittle characteristics of coal samples can be reflected by the ratio of the dissipated energy to the accumulated energy.
研究煤的孔隙裂隙特征及裂纹扩展行为对于预防煤矿灾害至关重要。通过压汞法(MIP)和气体吸附法获得了取自高瓦斯煤层的煤样的孔隙结构特征。得到了煤样在三点弯曲条件下的变形破坏过程。结果表明,直径小于100nm的吸附孔最为发育,其表面最粗糙(平均表面分形维数为2.933)。微裂纹表面较光滑(为2.481),有利于瓦斯渗流。这可能是14-3#煤层为高瓦斯煤层但迄今为止几乎没有瓦斯突出事故的原因。在裂纹扩展初期,煤样上的主裂纹沿天然裂纹方向扩展。在裂纹扩展过程中,主裂纹的表面分形维数增大,表明主裂纹的弯曲程度增强。煤样的脆性特征可通过耗散能量与积聚能量的比值来反映。