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At mixed dislocations, the β1 precipitates form into a variety of arrays, often comprising particles of the same orientation variant.
Furthermore, with energy dispersive spectroscopy (EDS), we show that there is an increase in the nickel concentration at the interface between each orientation variant.
By distinguishing deformation variant from orientation variant, the theoretical connection and distinction between PTMC and phase field microelasticity theory are discussed, and their predictions are compared with experimental observations.
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Six orientation variants and translation domains have been observed.
A cubic to tetragonal transformation leads to simultaneous nucleation and growth of several orientation variants.
De Wolff defects corresponding to two orientation variants can coexist in the same pyrolusite crystallite.
In each case, the morphology and spatial distribution of the orientation variants are characterized.
Locally, each group of martensite plates consisted of four orientation variants that are twin-related to one another.
The coherent phase transformation between two equilibrium single-phase states producing several orientation variants of the product phase is considered.
In each plate colony, there are four distinct plates in terms of the crystallographic orientation of the thicker lamellar variants and therefore, in total, eight orientation variants.
The development of the transformation through nucleation, growth and coarsening of orientation variants is simulated for both single crystal and polycrystalline materials.
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