Test of an equation for nonisothermal moisture transport in wood.
Nelson R.M. Jr.
Reported moisture and temperature distributions in wood exposed to a temperature gradient under conditions of zero flow were used to compute changes in moisture content per change in Kelvin temperature, dm/dT. Corresponding theoretical values were calculated from a model based on nonequilibrium thermodynamics. Comparison of the measured and theoretical values supports the notion that moisture transport in wood can be modeled successfully with thermodynamic methods.
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Эту запись предоставил Wolters Kluwer