1998
DOI: 10.1006/jcis.1997.5292
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Influence of Surface Wettability on Adsorption Isotherms of Water Vapor

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1998
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Cited by 33 publications
(27 citation statements)
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“…However, the same behaviour is shown in the paper by Chen and Wangaard (1968) for a different species, but in this case, the desorption cycle from the wet state is for a sample of originally dry wood that was subsequently equilibrated over water. Churaev et al (1998) discussed the nature of water vapour sorption isotherms on porous surfaces where there is incomplete wetting of the substrate during the sorption process. This involves calculations of contact angles formed between the convex capillary menisci in narrow pores at RH values below saturation.…”
Section: Resultsmentioning
confidence: 99%
“…However, the same behaviour is shown in the paper by Chen and Wangaard (1968) for a different species, but in this case, the desorption cycle from the wet state is for a sample of originally dry wood that was subsequently equilibrated over water. Churaev et al (1998) discussed the nature of water vapour sorption isotherms on porous surfaces where there is incomplete wetting of the substrate during the sorption process. This involves calculations of contact angles formed between the convex capillary menisci in narrow pores at RH values below saturation.…”
Section: Resultsmentioning
confidence: 99%
“…The concept of surface wettability of water surfaces in microcapillaries has been used more recently in a theoretical treatment of sorption isotherms. 35 It should be noted in this context that two types of hysteresis can be observed with cellulose, or a lignocellulosic material ( Fig. 1).…”
Section: Introductionmentioning
confidence: 98%
“…The term Πh is equivalent to the expression ΓΔm, which was introduced in [11] as a new thermodynamic function called excess surface work Φ. It is defined [12]: Excess surface work ESW = surface free energy + isothermal isobaric work of sorption.…”
Section: Theorymentioning
confidence: 99%
“…Further, for adsorption the sum of two exponential functions for the film thickness was applied, and the surface tension dependence on the pore size was considered. However, together with Churaev the author showed already in [10], that a sum of two exponential functions is helpful for the description of wetting phenomena in very large pores with pores sizes of several microns, but not necessarily for micropores as in MCM-41 zeolites. Further in the results ( [9] Tab.…”
Section: Introductionmentioning
confidence: 96%