3
Crystal nucleation
If the liquid is cooled beyond the corresponding freezing point T
m
at which the liquid and
crystalline phases coexist in equilibrium, a thermodynamic driving force builds up towards
forming the crystal. In this chapter we will discuss how the liquid transforms into a crystal,
focusing on how the changes in the liquid are initiated and on the nature of the crystalline
region that is formed. This process is referred to as nucleation. The thermodynamic force
favoring the formation of the crystal seed in the supercooled liquid competes with the pro-
cess of forming an interface between the solid and the liquid. The cost of the interfacial
free energy therefore presents a barrier to the formation of the new phase. Only when the
driving force is made large enough by moving deep into the supercooled state does crystal-
lization occur on laboratory time scales. Thus pure water can be cooled to −20
◦
C or below
without freezing. Our focus here will be mainly on the process of crystallization of solid
from the melt. The condensation of vapor into liquid is a very thoroughly studied process
that has been discussed in various reviews (Stanley, 1971; Evans, 1979; ten Wolde et al.,
1998). For condensation from a low-density gas or crystallization from dilute solution, it
is easier to identify the nucleating bubbles since they differ widely in composition from
the surrounding phase. In a crystal forming from a melt the nucleating droplet is far less
distinct. It is somewhat problematic to define the cluster in the bulk of the melt in terms of
a certain set of particles. One possible route is to identify the coordination numbers, which
differ between the liquid and the crystalline phase. We will simplify our discussion here
by limiting the discussion to one-component systems and also focus on what is termed
homogeneous nucleation (Oxtoby, 1992a, 1992b; Gunton, 1999), which occurs in the bulk
of the pure liquid phase. We also briefly explore here the issue of heterogeneous nucleation
(Turnbull, 1969) started by impurities or occurring on the surfaces.
3.1 Classical nucleation theory
In the classical nucleation theory we associate a number of particles with the nucleus of
the new phase having a sharp interface with the bulk liquid. In this theory of the nucleation
process the nucleus of the crystal, no matter how small, is treated using macroscopic ther-
modynamic principles. Let us first consider the formation of N
i
clusters, each consisting
of i monomers, and N single monomers (N N
i
). Assuming that clusters mix ideally
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