capillary condensation

基本解釋

At medium and high RH, it is capillary condensation, and the main factor is pore volume.
在中高相對濕度下，調(diào)濕作用主要是依靠毛細凝聚作用，調(diào)濕性能由孔容積決定。
The results are shown as follows:1. When the relative vapor pressure reached to 72-75%, capillary moisture condensation began to appear in the tested soil.
結(jié)果表明：（1）供試土壤在相對水氣壓達72—75％時，開始明顯呈現(xiàn)出毛管凝聚作用；
With the increase of mean cluster size(MCS)at different water activities, multi-layer sorption and capillary condensation occur, which lead to the diminution of diffusion coefficients in P…
結(jié)果顯示，隨著水蒸氣活度的增加，膜內(nèi)水分子簇尺寸增大，并在膜的微孔內(nèi)產(chǎn)生多層吸附甚至毛細管冷凝，導致擴散系數(shù)迅速降低。
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