Vapor diffusion in porous media in the presence of its own liquid may be enhanced due to pore-scale processes,such as condensation and evaporation across isolated liquid islands.Webb and Ho (1997) developed a mechanistic pore-scale model of these processes under steady-state conditions in which condensation and evapporation on the liquid island were equal.The vapor diffusion rate was significantly enhanced by these liquid island processes by up to an order of magnitude compared to a dry porous media.However,vapor transport by diffusion is often complicated by transient effects,such as in drying applications,in which net evaporation of liquid may further augment the vapor flux from diffusion.The influence of transient effects on the enhancement factors for vapor diffusion is evaluated in this paper.In addition,the effect of vapor pressure lowering on the enhancement factor and on pore-scale vapor fluxes is shown.
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