Abstract
The purpose of this study is to further investigate the classical Gibbs analysis of the heterogeneous system “stressed crystal–melt.” It is demonstrated that each equilibrium configuration is stable with respect to a special class of variations introduced by Gibbs. This basic result is compared with the opposite result on the universal morphological instability of phase interface separating a stressed crystal with its melt. Some plausible manifestations of the instabilities implied by the Gibbs model are qualitatively discussed.
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