Abstract

The coupling of coal spontaneous combustion and high methane is ubiquitously observed in coal mining and poses a significant jeopardy to production safety. The extant studies are largely focused on altering external methane conditions and fail to investigate the spontaneous combustion properties of methane-laden coal samples. This study conducted an evaluation of the microstructure of typical coal samples, followed by a fractal analysis. It discovered that the surface structure of the specimen is relatively homogeneous, and the mesopores (2–4 nm) exhibit a significant influence on the specific surface distribution. The overall pore structure is characterized by a multiplicity of peaks, which renders the coal sample markedly segmented during methane desorption, oxygen consumption, and gas products generation. The low-temperature oxidation tests under various working conditions reveal that methane desorption is a crucial factor in determining the spontaneous combustion pattern of the coal sample. The degree of methane desorption bears a close association with the oxygen concentration, and at an oxygen concentration of approximately 2 %, there is a turning point for gas generation and oxygen consumption. The present investigation provides a qualitative and quantitative exposition of the relevant laws, offering guidance for fire prevention and suppression in pertinent mines.

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