Simultaneous heat and mass transfer equations were developed to simula
te the infrared radiative heating of agricultural crops. The equations
assume that moisture diffuses to the outer boundaries of the material
in liquid form and evaporation occurs at the surface of the kernel. E
nergy for moisture evaporation is supplied by the infrared radiant ene
rgy. The equations were validated with experimental data on surface te
mperature and average moisture content of barley kernels. Average devi
ations of predicted surface kernel temperature and average kernel mois
ture from experimental data were 3.9 degrees C and 0.6% (w.b.), respec
tively. These comparisons were performed using kernels having initial
moisture contents of 12.2%, 17.0% and 23.17%. Sensitivity analysis of
process parameters showed that infrared burner temperature, distance o
f infrared burner from the grain bed, grain initial moisture content a
nd grain heating time significantly affected kernel temperature. Burne
r temperature and burner height had no significant effect on grain fin
al moisture content.