Flat elasticity theory application for the description of stressed state and fracture of solids under phase transitions
The stress function is proved to be biharmonic for an elastically isotropic crystal undergoing phase transition which follows spontaneous dilatation. For an elastically anisotropic crystal which is neither improper nor proper ferroelastic, as well as for the improper ferroelastic, the stress functio...
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Veröffentlicht in: | Journal of materials science 1992-12, Vol.27 (23), p.6401-6410 |
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Format: | Artikel |
Sprache: | eng |
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