This article focuses on the concept of a 'drying characteristic functi
on,' which is an effective way to correlate drying rate curves for con
vective drying of homogeneous nonporous, hygroscopic porous and non-hy
groscopic porous materials. The characteristic function, obtained by a
certain transformation of a drying rate curve, is independent of dryi
ng conditions and hence characterizes the transport kinetics in the ma
terial. The principle and some applications of the functions are revie
wed. The first application is estimation of drying rate curves. Becaus
e any drying rate curve can be transformed into the characteristic fun
ction and vice versa, the drying rate can be estimated for various dry
ing conditions from a single drying experiment. Another application is
determination of the moisture diffusivity. Using the 'flux ratio meth
od,' an analytical expression of the characteristic function can be ob
tained for any given moisture diffusivity. The expression enables one
to determine the moisture diffusivity for a wide range of moisture con
tent from a single drying experiment.