The drying of potato slabs in air flow is analysed by the simultaneous
numerical solution of the differential heat balance and diffusion equ
ations for a shrinking body. A uniform temperature profile in the soli
d and temperature dependent diffusion coefficient is assumed. Comparis
on between predicted and experimental mean moisture content and temper
ature variations in the sample provides a satisfactory agreement for t
he moisture range from approximately 5 . 0 to 0 . 4 kg water/kg dry so
lid. For this moisture range it can be assumed that the diffusion coef
ficient is not a function of moisture content.