不同粒径构造煤微观分形特征与渗流机理研究OA
Study on microscopic fractal characteristics and seepage mechanism of tectonically deformed coal with different particle sizes
为探究不同粒径对构造煤微观结构与渗流特性的调控机理,支撑构造煤赋存区瓦斯灾害防控与煤炭高效开采,以新疆艾维尔沟矿区二道沟煤矿的构造煤和原生煤为研究对象,采用扫描电子显微镜对[425,850)μm、[250,425)μm、[180,250)μm、[150,180)μm、[125,150)μm 5 个粒径区间煤样的微观孔隙特征进行观测.结合图像二值化处理与盒维数分形法,定量表征不同粒径构造煤微观孔隙结构的分形特征;基于分形理论构建煤体渗流模型,系统揭示了粒径效应对构造煤渗流特性的内在影响机制.结果表明:原生煤孔隙分布致密且连通性差,而构造煤孔隙类型以碎粒孔、矿物充填孔、角砾孔为主,孔隙形态多样且类型复杂;随着构造煤粒径的减小,其微观孔隙特征的复杂性与非均质性持续增强;分形维数计算结果显示,构造煤分形维数随粒径减小而逐步增大,直观反映了微观孔隙特征复杂程度的提升;分形渗流模型计算结果显示,构造煤的渗透率与分形维数、孔隙直径等微观结构参数显著相关,其中分形维数越大,渗流过程中小孔隙占比越高,煤体渗流阻力随之显著增大.
To investigate the regulatory mechanism of particle size on the microstructure and seepage characteristics of tectonically deformed coal,and further provide theoretical support for gas disaster prevention and control as well as high-efficiency coal mining in tectonically deformed coal-bearing areas,this study took the tectonically deformed coal and primary coal from Erdaogou Coal Mine in Aiweiergou Mining Area of Xinjiang as the research objects.Scanning electron microscope(SEM)was employed to ob-serve the micro-pore characteristics of coal samples classified into five particle size ranges:[425,850)μm,[250,425)μm,[180,250)μm,[150,180)μm and[125,150)μm.Combined with image binarization processing and box-counting fractal method,the fractal characteristics of the micro-pore structure of tectonically deformed coal with different particle sizes were quantitatively character-ized.Based on fractal theory,a coal mass seepage model was established to systematically reveal the intrinsic influence mechanism of particle size effect on the seepage characteristics of tectonically deformed coal.The results indicate that:the pores of primary coal are densely distributed with poor connectivity,while the pore types of tectonically deformed coal are dominated by fragment pores,mineral-filled pores and breccia pores,presenting diverse and complex morphologies.With the decrease in particle size of tectonic-ally deformed coal,the complexity and heterogeneity of its micro-pore characteristics are continuously enhanced.The calculation results of fractal dimension show that the fractal dimension of tectonically deformed coal increases gradually with the reduction of particle size,which directly reflects the improvement of the complexity of micro-pore characteristics.The calculation results of the fractal seepage model reveal that the permeability of tectonically deformed coal is significantly correlated with microstructural para-meters such as fractal dimension and pore diameter.Specifically,a larger fractal dimension corresponds to a higher proportion of small pores during the seepage process,which consequently leads to a significant increase in the seepage resistance of coal mass.
陆卫东;赵鹏翔;金欢;李树刚;刘元嘉;金权;王李军;韩霜莹
新疆工程学院 安全科学与工程学院,新疆 乌鲁木齐 830023||新疆工程学院 新疆煤矿灾害智能防控与应急重点实验室,新疆 乌鲁木齐 830023西安科技大学 安全科学与工程学院,陕西 西安 710054||西部矿井瓦斯智能抽采工程研究中心,陕西 西安 710054新疆工程学院 安全科学与工程学院,新疆 乌鲁木齐 830023||新疆工程学院 新疆煤矿灾害智能防控与应急重点实验室,新疆 乌鲁木齐 830023西安科技大学 安全科学与工程学院,陕西 西安 710054新疆工程学院 安全科学与工程学院,新疆 乌鲁木齐 830023||新疆工程学院 新疆煤矿灾害智能防控与应急重点实验室,新疆 乌鲁木齐 830023西安科技大学 安全科学与工程学院,陕西 西安 710054辽宁工程技术大学 安全科学与工程学院,辽宁 葫芦岛 125105西安科技大学 安全科学与工程学院,陕西 西安 710054
矿业与冶金
粒径扫描电子显微镜构造煤分形维数渗流模型
particle sizescanning electron microscope(SEM)tectonically deformed coalfractal dimensionseepage model
《煤矿安全》 2026 (4)
1-11,11
新疆维吾尔自治区"天山英才"培养计划科技创新领军人才资助项目(2024TSYCLJ0026)
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