夹矸影响下的含瓦斯煤裂隙演化规律探究

Exploration of fracture evolution in gas-containing coal under gangue influence

  • 摘要: 为了探究夹矸对含瓦斯煤裂隙演化的影响,本文以含瓦斯煤为研究对象,利用煤岩三轴加载系统与受载煤岩工业CT扫描系统进行实验,通过设置不同夹矸厚度与层数、恒定围压以及不同瓦斯气压加载,开展了含瓦斯煤裂隙扫描实验,获取了多种原始CT图像,利用三维重构技术,构建含瓦斯煤的数字化模型,实现了煤体内部裂隙空间结构的可视化并通过Avizo软件对裂隙结构参数进行计算,定量分析了含瓦斯煤裂隙演化的特性. 研究结果表明:含瓦斯煤试样三轴加载的破坏形式为剪切破坏,纯煤试样裂隙呈现出平行、交叉等复合型式;夹矸试样裂隙主要集中于煤体部分,只有一两条主要裂隙延伸至岩体部分并扩展贯穿夹矸层,夹矸层受损程度较小;双层夹矸试样损伤主要集中于两层夹矸之间的煤体部分,破裂后的宏观裂纹多表现为“A”字形的特征;夹矸影响下的含瓦斯煤破裂后的裂隙率、三维分形维数和平均配位数随瓦斯压力的增加而增加,裂隙率、三维分形维数和平均配位数随夹矸厚度和夹矸层数增加而降低;瓦斯压力的增加导致库伦破坏线与莫尔应力圆互相接近,逐渐接近试样的破坏条件,促使裂隙更加容易发育;夹矸厚度的增加,降低了裂纹扩展能量释放率,临界裂隙长度增大,裂隙扩展更难发生.

     

    Abstract: To investigate the influence of gangue interlayers on fracture evolution, this study takes gas-containing coal as its research object. First, fracturing experiments were conducted using a triaxial loading system designed for coal and rock. Samples with varying gangue interlayer thicknesses (0, 6, 10, 16, and 20 mm) and numbers of layers (0, 1, and 2) were loaded to failure with uniform axial pressure under a constant confining pressure of 2 MPa and different gas pressures (0.2, 0.4, 0.6, and 0.8 MPa). Subsequently, fracture-scanning experiments were performed on gas-containing coal using an industrial computed tomography (CT) scanning system for loaded coal and rock, obtaining various original CT images. With the help of VG Studio MAX three-dimensional (3D) reconstruction technology, two-dimensional CT slice sequences were converted into 3D digital models, allowing for the visual characterization of the spatial distribution of internal fracture networks in coal. Furthermore, the Avizo software was adopted to quantitatively extract mesoscopic structural parameters, such as fracture rate, 3D fractal dimension, and average coordination number. By closely combining the fracture mechanics theory and Mohr–Coulomb strength criterion, the fracture evolution characteristics in gas-containing coal were quantitatively analyzed. The results show that the failure mode of gas-containing coal samples exhibits significant shear failure. With an increase in gas pressure, shear cracks in pure coal samples further develop into composite forms, such as parallel and cross cracks. Fractures in the gangue interlayer samples are mainly concentrated in the coal part, with only one or two main fractures extending to and penetrating the gangue interlayer within the rock part. This indicates that the gangue interlayer is less damaged, and obvious faulting occurs in the 3D fracture network. In double-layer gangue samples, fractures are primarily distributed in the coal between the two gangue interlayers, generally showing that two fractures develop and merge, ultimately penetrating the sample. Simultaneously, transverse fractures form between the two main fractures, presenting an overall “A”-shaped fracture characteristic. Under the influence of gangue interlayers, the fracture rate, 3D fractal dimension, and average coordination number of gas-containing coal after failure increase with increasing gas pressure but decrease with increasing gangue interlayer thickness and number of layers. An increase in gas pressure promotes sample failure, enhances internal complexity, and improves pore connectivity. Conversely, an increase in gangue thickness and number of gangue layers inhibits fracture development and reduces the internal complexity and pore connectivity of samples. Increasing the gas pressure causes the Coulomb failure line and Mohr stress circle to approach each other, gradually reaching the failure condition of the sample, which promotes fracture development. Increasing the gangue interlayer thickness reduces the energy release rate of crack propagation, increases the critical fracture length, and consequently hinders crack propagation. This study provides a theoretical basis for understanding the failure mechanism of gas-containing coal with gangue interlayers and holds significant engineering importance for gas outburst prevention and control in coal mines.

     

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