Ideas proposed at
the beginning of the 20th century to describe
the temperature dependence of crystal growth rates have become accepted
as the “standard model.” Specifically, it was proposed
that rates are controlled by a thermodynamic driving force, liquid/solid
interfacial surface energy requires crystal growth to occur at step
or kink sites, and particle diffusion/viscous relaxation also controls
the rate of growth. However, as described in this article, these underlying
assumptions are inconsistent with the fact that crystal growth from
supercooled melts is microscopically irreversible, and the well-known
fact that short- and intermediate-range order in melts and crystals
is essentially equivalent, precluding the existence of sharp interfaces
and the need for material diffusion. By contrast, we recently introduced
the Transition Zone Theory of crystallization, TZTc, a
condensed matter analogue of Eyring’s transition state theory
that uses Kauzmann’s conception of configurational entropy
and Adam and Gibbs’ ideas of cooperativity to describe the
ensemble characteristics governing crystal growth rates. Here, the
TZTc model is applied to the same sets of inorganic oxides
and organic molecules that were used to evaluate the apparent decoupling
of viscosity from the standard model, as well as to several other
materials. Without exception, the TZTc model provides a
superior fit to temperature-dependent crystal growth-rate data. With
a single model accurately describing diverse crystallizing systems,
the three parameters extracted from TZTc, for the first
time, provide a platform with which to compare and contrast chemical/physical
factors that influence crystallization reactions.