As in the case of homogenenous nucleation of a solid from its undercooled melt, in this case also, we are interested in calculating the critical size of the nucleus for homogeneous nucleation and the associated free energy changes.
In the case of a solid-solid phase transformation, in addition to the changes in bulk free energy and interfacial energy, typically, there is also a strain energy contribution which needs to be accounted for; this is because, typically, the volumes of the original and the resultant are not the same, and unlike fluids, solids can support shear stresses. This strain energy (known as misfit energy because this is related to the imperfect fitting of the transformed phase into the original volume) can be shown to be proportional to the volume of the tranformed phase. It is in this respect that the homogeneous nucleation of precipitation differs from that of the solid from its pure melt.
In other words, during solid-solid transformation, |