First,
less than 30 g of brown coal packed in a sphere stainless
net and placed in an air naturally circulating temperature-programmed
oven was found to start spontaneous combustion from the center of
the coal sphere when the oven temperature was raised to 135 °C.
This was because the heat generation rate by the oxidation of coal
was larger than the rate of heat dissipation rate by natural convection
at 135 °C. Next, to clarify the mechanism by which coal is heated
to 135 °C, the temperature increase of less than 10 g of the
fixed bed of dried brown coal was measured by contacting the coal
with flowing dry air or wet air at 50, 70, 95, and 107 °C. It
was found that the maximum temperature increase in the dry air was
almost null at 70 °C and only 5 °C or so even at 107 °C.
On the other hand, the maximum temperature increases were respectively
10, 25, 46, and 40 °C at 50, 70, 95, and 107 °C in the wet
air, suggesting that the adsorption of water vapor plays a crucial
role in increasing the coal temperature high enough for the spontaneous
combustion to start. A simple simulation program was developed for
expressing the temperature change observed by the above fixed bed
experiment by formulating the mass and enthalpy balance equations
with the separately measured heat generation rate by the coal–oxygen
interaction at 50–150 °C and the adsorption isotherm and
the heat of adsorption of water vapor on coal at 70 °C. The simulation
program well expressed the temperature change for the experiments
performed at 70 °C in both the wet air and the dry air, indicating
that the spontaneous heating of coal is brought about by the coupled
effect of the adsorption of water vapor and the coal oxygen interaction.
In addition, the simulation showed how the spontaneous combustion
of coal starts in the wet air.