The influence mechanism of dynamic metamorphism on the evolution of micro-nano pore structure in tectonically deformed coal (TDC)
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摘要: 【目的】 煤中微纳米孔隙结构是瓦斯的主要赋存空间之一,探讨动力变质影响下构造煤微纳米孔隙结构的演化机制,有助于深入理解煤与瓦斯突出机理。【方法】 综合利用CO2吸附实验、傅里叶变换红外光谱(FTIR)测试和分子动力学模拟研究宿州祁南矿72煤层发育的不同类型构造煤微纳米孔隙结构演化特征及机理。【结果和结论】 结果表明:随着构造变形增强,超微孔(0.3~0.7 nm)孔径整体向小孔径方向偏移,微纳米孔隙体积分形维数和比表面积分形维数增大,非均质性增大,孔隙结构复杂度升高;分子结构测试和分子动学模拟结果表明,脆性变形构造煤主要发生应力降解作用,煤分子结构中氢键、脂肪侧链和含氧官能团的断裂和解离促使分子结构活动性增强,并在构造应力作用下煤大分子结构初步被压缩;脆韧性和韧性变形构造煤可以发生显著的应力缩聚作用,煤中芳香结构发生旋转、折叠和重组等化学变化,形成排列更紧密的构造煤分子结构构型。因此,随着构造变形作用增强,煤大分子结构被不断压缩改变,分子结构间隙被分割,导致微纳米孔隙结构的形态和大小发生改变,孔隙复杂度升高,孔径整体向小孔径方向偏移。Abstract: Micro-nano pore structure is one of the main occurrence spaces of gas. Exploring the evolutionary mechanism of micro-nano pore in TDC under the influence of dynamic metamorphism can help to deepen the understanding of coal and gas outburst mechanisms. The evolutionary characteristics and mechanism of micro-nano pore structure of different types of TDCs developed in 72 coal seam of Qi'nan Coal Mine in Suzhou were studied by CO2 adsorption experiment, Fourier transform infrared spectroscopy (FTIR) test and molecular dynamics simulation. The results show that with the increase of tectonic deformation, the pore size of ultra-micropores (0.3 ~ 0.7 nm) shifts to the direction of small pore size, the fractal dimension of micro-nano pore volume and the fractal dimension of specific surface area increase, the heterogeneity increases, and the complexity of pore structure increases. The results of molecular structure test and molecular dynamics simulation indicate that brittle deformed coals mainly occur through stress degradation. The breaking and dissociation of hydrogen bonds, aliphatic side chains, and oxygen-containing functional groups in the coal molecular structure enhance the activity of the molecular structure, and under the action of tectonic stress, the coal macromolecular structure is initially compressed; The brittle-ductile and ductile deformed coals undergo significant stress condensation, and the aromatic structure in coal can undergo chemical changes such as rotation, folding, and recombination, forming a more tightly arranged molecular structure configuration of coal. Therefore, with the enhancement of tectonic deformation, the structure of coal macromolecules is continuously compressed and changed, and the gaps between molecular structures are divided, resulting in changes in the morphology and size of micro-nano pore structures, an increase in pore complexity, and an overall shift in pore size towards smaller pore sizes.
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