Magmatic intrusions induce intense thermal-force effects on coal seams, significantly altering their physicochemical structure and influencing gas behavior and spontaneous combustion propensity, thereby threatening mine safety. This study investigates magmatically altered coal (MAC) and corresponding unaltered coal from the Tiefa Coalfield. Integrated N2 adsorption, X-ray photoelectron spectroscopy, and desorption-displacement-oxidation experiments, combined with fractal theory and diffusion/reaction kinetics, were employed to systematically analyze pore and chemical structure evolution and its control on gas transport and reaction. Results show that magmatic alteration increases specific surface area and pore volume while reducing pore size. Fractal and multifractal analyses reveal rougher surfaces, more complex spatial structures, and enhanced heterogeneity and connectivity. Chemically, MAC undergoes aromatization and condensation, reducing unstable oxygen-containing groups, developing an aromatic carbon skeleton, and generating persistent free radicals and catalytic sulfone sulfur. These changes lead to gas desorption with high capacity but slow release: increased limit diffusion capacity, decreased initial diffusion coefficient, and prolonged median desorption time. In the displacement and oxidation stages, MAC exhibits higher gas displacement and oxygen consumption rates. The apparent activation energy during slow oxidation decreases by approximately 50%, the crossing-point temperature drops significantly, and CO/CO2 concentrations are consistently higher. This study elucidates that magmatic alteration synergistically creates a physicochemical environment with high adsorption capacity, excellent pore connectivity, and low reaction barriers, collectively increasing spontaneous combustion propensity. It provides a critical theoretical basis for preventing and controlling spontaneous combustion risks in magmatically affected mines.
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