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English[en]
a temperature gradient directed towards the surface, i.e. temperatures inside are higher than outside, giving rise to a higher partial pressure that drives the evaporating liquid to the surface consequently, the superficial layer does not dry up completely and the surfaces remain permeable
Chinese[zh]
由内向外的温度梯度,即内部温度高于外部温度,提高分压驱使水蒸气向表面蒸发 表层不会完全干涸,表面可保持渗透性

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