A mathematical model describing moisture migration by diffusion in a solid
sphere with variable diffusion coefficient is proposed. An analytical expre
ssion for dependence of the diffusion coefficient with moisture content was
derived based on the assumption that the activation energy for diffusion v
aries linearly with the desorption energy.
The expression for moisture dependence of diffusion coefficient was used to
simulate drying of parboiled rice in the temperature range 50-90 degreesC.
The mathematical model shows good agreement between observed and predicted
drying rate curves.