The thermodynamic theory of the growth of Dauphine twinning in quartz under stress
- 14 December 1978
- journal article
- Published by IOP Publishing in Journal of Physics C: Solid State Physics
- Vol. 11 (23), 4665-4679
- https://doi.org/10.1088/0022-3719/11/23/013
Abstract
The equilibrium condition is deduced for the stable coexistence, under stress, of Dauphine twins. It is shown that this condition is determined by the principle that a generalised Gibbs free energy be minimised. At equilibrium the generalised Gibbs free energy density of each twin must have the same value. If stresses are applied such that the equilibrium condition is not satisfied, this principle determines which twin will survive the resulting untwinning process. The theory is developed rigorously using finite strain theory. It is shown that, if four relations between the elements of a certain asymmetric tensor are satisfied, the stress coexistence condition is satisfied exactly, that is, to any order. The proof of this exact temperature-independent condition employs the method of the integrity basis for invariant functions of the crystal point group.Keywords
This publication has 5 references indexed in Scilit:
- Finite strain coordinates and the stability of solid phasesJournal of Physics C: Solid State Physics, 1976
- Invariant functions and homogeneous bases of irreducible representations of the crystal point groups, with applications to thermodynamic properties of crystals under strainJournal of Physics C: Solid State Physics, 1974
- Non-hydrostatic thermodynamics of chemical systemsProceedings of the Royal Society of London. Series A. Mathematical and Physical Sciences, 1970
- Third-Order Elastic Coefficients of QuartzJournal of Applied Physics, 1966
- Piezoerescence—the growth of Dauphiné twinning in quartz under stressProceedings of the Royal Society of London. Series A. Mathematical and Physical Sciences, 1951