4.7 Article

Anisotropic wood-water interactions determined by gravimetric vapor sorption experiments

Journal

CELLULOSE
Volume 30, Issue 6, Pages 3869-3885

Publisher

SPRINGER
DOI: 10.1007/s10570-023-05093-z

Keywords

Vapor sorption; Vapor transport; Diffusivity; Permeability; Sorption; Wood

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Gravimetric vapor sorption experiments were conducted on beech wood samples to determine the directional permeability, diffusion, and sorption coefficients in different wood directions. The diffusion coefficient was evaluated from dynamic vapor sorption experiments using a double stretched exponential model, ranging from 0.10 x 10(-10) to 1.52 x 10(-10) m(2)/s depending on wood direction and relative humidity. Moisture sorption isotherms were constructed and fitted to models to calculate the sorption coefficient, which ranged from 2.4 to 3.0 mol/(m(3) Pa). The permeability coefficient was calculated from dynamic vapor transport experiments and varied from 0.56 x 10(-10) to 4.38 x 10(-10) mol/(m s Pa) based on flow direction and RH conditions. This experimental approach is suitable for studying wood-moisture interactions.
Gravimetric vapor sorption experiments were performed on beech wood samples to determine the directional permeability, diffusion and sorption coefficients in the three orthotropic wood directions. Dynamic Vapor Sorption (DVS) experiments allowed for the direct evaluation of the diffusion coefficient from the analysis of the kinetic sorption profile using a double stretched exponential model with values ranging from 0.10 x 10(-10) to 1.52 x 10(-10) m(2)/s and depending on the wood direction of the sample and the RH-values. Moisture sorption isotherms (MSIs) were constructed and fitted to a modified Guggenheim-Anderson-de Boer and a Sorption Site Occupancy model, which allowed for the calculation of the sorption coefficient which was found to be between 2.4 and 3.0 mol/(m(3) Pa). Dynamic Vapor Transport (DVT) experiments were performed to calculate the permeability coefficient from the vapor flow rate and it ranges between 0.56 x 10(-10) and 4.38 x 10(-10) mol/(m s Pa) as a function of the flow direction and RH conditions. These results indicate that such an experimental approach is suitable for determining wood-moisture interactions.

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