摘要

Low rank coals are susceptible to spontaneous combustion, because oxidation rate of low rank coals are higher than that of high rank coals. Even low rank coals, however, must be heated over a critical temperature before spontaneous combustion starts. This work assumed that rapid spontaneous combustion of coal in stockpile will start from the heat up of coal fines on the surface of the stockpile by the heat supplied from the sun and moist air. Then direct measurement of possible temperature increase by the adsorption of water vapor on coal from ambient atmosphere was undertaken by using three kinds of brown coals/lignites and a bituminous coal. When about 100 mg of each brown coal pre-dried at 80 degrees C and cooled to 28 degrees C were exposed to an ambient and stationary atmosphere of 28 degrees C with 6777% relative humidity, the coal temperatures increased up to 4043 degrees C in a minute or so. When the brown coals pre-dried and cooled to 38 degrees C were exposed to a stagnant saturated air at 38 degrees C, the coal temperatures increased up to over 60 degrees C in a minute or so. This was found to occur by rapid adsorption of water vapor from the ambient atmosphere onto the coal. Next, a simple model based on mass and enthalpy balances was successfully formulated to simulate the water adsorption and temperature change. The model simulation then clarified that the amount of heat generated by the adsorption of water vapor are much larger than the heat generated by initial coal oxidation and that most of heat generated is transferred to the surrounding to be utilized to heat up the surroundings. Thus, the important role of the adsorption of water vapor from the ambient atmosphere on the spontaneous heating of coal fines in stockpile was clarified.

  • 出版日期2016-1