Exploring Spontaneous Combustion Characteristics and Structural Disparities of Coal Induced by Igneous Rock Erosion

• Published in: Fire (Basel, Switzerland) Vol. 7; no. 5; p. 159
• Main Authors: Zhang, Mingqian, Li, Zongxiang, Chen, Zhifeng, Gao, Lun, Qi, Yun, Hu, Haifeng
• Format: Journal Article
• Language: English
• Published: Basel MDPI AG 01.05.2024
• Subjects: activation energy; Adsorption; Air leakage; Carbon dioxide; Coal; Coal mining; coal spontaneous combustion; Combustion; Environmental aspects; Experiments; functional group; Functional groups; Gases; igneous rock erosion; Igneous rocks; Infrared spectroscopy; Low temperature; Mercury; Metamorphism; Mines; Oxidation; Oxygen; Oxygen consumption; pore structure; Rocks, Igneous; Spectrum analysis; Spontaneous combustion; Structural stability; Temperature; Thermal properties; Thermogravimetric analysis; China; United States > US; Germany
• ISSN: 2571-6255; 2571-6255
• DOI: 10.3390/fire7050159

The erosion of igneous rocks affects the structural and spontaneous combustion characteristics of coal. A series of tests were conducted, including programmed heating, thermogravimetric analysis, FT-IR spectroscopy, low-temperature nitrogen adsorption, and pressed mercury experiments on samples from primary coal and coal eroded by igneous rocks from the Tashan Mine and Xiaonan Mine within the same coal seam. Based on these experiments, we analyzed various properties of coal, such as the oxidation characteristics, spontaneous combustion limit, active functional group content, chemical structure, and pore structure, from both macroscopic and microscopic perspectives. The results indicated significant trends after the erosion of igneous rocks: (1) there were increases in the oxygen consumption rate, as well as the CO and CO2 release rates; (2) the upper limit of air leakage intensity increased, the minimum thickness of floating coal decreased, and the lower limit of oxygen volume fraction decreased; (3) there was a decrease in the activation energy required for coal ignition; (4) there was a decrease in the active functional group content while improving the structural stability; and (5) there were the alterations in the pore structure of coal. These promoted the oxidation reactions between oxygen and the active groups within the coal matrix, increasing the propensity for spontaneous combustion, particularly in the igneous rocks with low oxidation activity.