压力和粒径影响下原生煤和构造煤非稳态扩散特性研究

    Study on unsteady diffusion characteristics of primary coal and tectonic coal under the influence of pressure and particle size

    • 摘要: 为了深入研究煤中瓦斯解吸扩散特性,通过开展不同瓦斯压力(0.8、1.3、2.4、3.3 MPa)和不同粒径(0.074~0.250、0.250~0.500、0.500~1.000、1.000~3.000 mm)的原生煤和构造煤的瓦斯解吸扩散试验,探讨了压力和粒径对原生煤和构造煤中瓦斯解吸量和瓦斯解吸速率的影响,建立了瓦斯非稳态扩散模型,分析了煤样的非稳态扩散特性。研究结果表明:原生煤和构造煤的瓦斯解吸量均随压力增加而增加,原生煤的瓦斯解吸量随压力增大的增长幅度比构造煤更大,导致两者的总瓦斯解吸量差距随压力增大而缩小;原生煤和构造煤瓦斯解吸量均随粒径减小而增加,粒径的减小仅会改变原生煤瓦斯解吸量的增长趋势,而不改变构造煤瓦斯解吸量的增长趋势;压力的增大对原生煤和构造煤瓦斯解吸速率变化幅度影响较小;而粒径的减小使原生煤的瓦斯解吸速率变化趋势由先快后慢变为快速减小,而不会使构造煤的瓦斯解吸速率变化趋势发生改变;构造煤瓦斯扩散系数的非稳态扩散特性随着压力的增加变化更为明显,而原生煤瓦斯扩散特性变化不大;粒径的减小可以使原生煤瓦斯解吸扩散特性从稳态向非稳态转变,而粒径的减小导致构造煤瓦斯解吸扩散非稳态特性更为明显,但是不改变非稳态扩散的本质。

       

      Abstract: In order to further study the characteristics of gas desorption and diffusion in coal, the gas desorption and diffusion experiments of primary coal and tectonic coal with different gas pressures (0.8, 1.3, 2.4, 3.3 MPa) and different particle sizes (0.074-0.250, 0.250-0.500, 0.500-1.000, 1.000-3.000 mm) were carried out. The effects of pressure and particle size on gas desorption and gas desorption rate in primary coal and tectonic coal were discussed. The unsteady diffusion model of gas was established and the unsteady diffusion characteristics of coal samples were analyzed. The main conclusions are as follows: the gas desorption amount of primary coal and tectonic coal increases with the increase of pressure. The growth rate of gas desorption amount of primary coal with the increase of pressure is larger than that of tectonic coal, which leads to the decrease of the total gas desorption amount gap between the two. The gas desorption amount of primary coal and tectonic coal increases with the decrease of particle size. The decrease of particle size only changes the growth trend of gas desorption amount of primary coal, but does not change the growth trend of gas desorption amount of tectonic coal. The increase of pressure has little effect on the change of gas desorption rate of primary coal and tectonic coal. The decrease of particle size makes the change trend of gas desorption rate of primary coal change from fast to slow to rapid decrease, but does not make the change trend of gas desorption rate of tectonic coal change. The unsteady diffusion characteristics of tectonic coal gas diffusion coefficient change more obviously with the increase of pressure, while the diffusion characteristics of primary coal gas do not change much. The decrease of particle size can make the gas desorption and diffusion characteristics of primary coal change from steady state to unsteady state, and the decrease of particle size leads to the unsteady characteristics of gas desorption and diffusion of tectonic coal more obvious, but it does not change the essence of unsteady diffusion.

       

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