“…The heat effects of water adsorption and condensation are generally more significant at low temperatures, for example, 20 °C or less, and potentially increase the temperature of relatively dry materials up to 40–50 °C . However, moisture adsorption or condensation due to sudden change in the ambient humidity or addition of liquid water, for example, rainfall, can contribute heat at relatively higher temperatures, causing a temperature spike in the pile , and even triggering the spontaneous ignition of a pile under subcritical conditions. , On the other hand, water vaporization is strongly endothermic. The elevated temperature driving the evaporation and subsequent transport of water vapor outward through diffusion and convection cause heat loss from the pile, which restrains the temperature increase or cools the pile. , Such an effect is more important at relatively higher temperatures. ,, …”