Ripening
(also called recrystallization) is a process that occurs
commonly in nature and industry that shifts the size distribution
of an ensemble of crystals toward a smaller number of larger crystals.
Ostwald ripening is by far the best known recrystallization mechanism
and sometimes is mistakenly considered as the only mechanism for shifting
the crystal size distribution. Ostwald ripening accounts for recrystallization
under thermodynamic control and is driven only by the well-known size
dependence of solubility. There are, however, other recrystallization
mechanisms that can be observed on laboratory timescales for crystals
of any size under certain conditions. Internal stress dispersion is
a thermodynamic ripening mechanism that depends not on surface energies
but rather on crystal defects. In addition, there are two other mechanisms
that are kinetic in nature. The most efficient is driven by the size
dependence of growth and dissolution rates at low supersaturation.
Finally, a mechanism proposed by Punin is driven by the difference
between growth and dissolution rates due to crystal defects. All the
four mechanisms can be at work simultaneously. The efficiency of ripening
can be enhanced by temperature oscillations, but only the thermodynamic
mechanisms can work at constant temperature. In this paper, we discuss
the fundamentals of these four ripening mechanisms and revisit in
detail Punin’s mechanism because it is the least well articulated
in the literature.