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  • 夾矸影響下的含瓦斯煤裂隙演化規律探究

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

    • 摘要: 為了探究夾矸對含瓦斯煤裂隙演化的影響,本文以含瓦斯煤為研究對象,利用煤巖三軸加載系統與受載煤巖工業CT掃描系統進行實驗,通過設置不同夾矸厚度與層數、恒定圍壓以及不同瓦斯氣壓加載,開展了含瓦斯煤裂隙掃描實驗,獲取了多種原始CT圖像,利用三維重構技術,構建含瓦斯煤的數字化模型,實現了煤體內部裂隙空間結構的可視化并通過Avizo軟件對裂隙結構參數進行計算,定量分析了含瓦斯煤裂隙演化的特性. 研究結果表明:含瓦斯煤試樣三軸加載的破壞形式為剪切破壞,純煤試樣裂隙呈現出平行、交叉等復合型式;夾矸試樣裂隙主要集中于煤體部分,只有一兩條主要裂隙延伸至巖體部分并擴展貫穿夾矸層,夾矸層受損程度較小;雙層夾矸試樣損傷主要集中于兩層夾矸之間的煤體部分,破裂后的宏觀裂紋多表現為“A”字形的特征;夾矸影響下的含瓦斯煤破裂后的裂隙率、三維分形維數和平均配位數隨瓦斯壓力的增加而增加,裂隙率、三維分形維數和平均配位數隨夾矸厚度和夾矸層數增加而降低;瓦斯壓力的增加導致庫倫破壞線與莫爾應力圓互相接近,逐漸接近試樣的破壞條件,促使裂隙更加容易發育;夾矸厚度的增加,降低了裂紋擴展能量釋放率,臨界裂隙長度增大,裂隙擴展更難發生.

       

      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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