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ESOMAT 2009, 02026 (2009)
DOI: 10.1051/esomat/200902026
Mechanisms of austenite-martensite transition
V. PaidarInstitute of Physics AS CR, 18221 Praha 8, Czech Republic
paidar@fzu.cz
Published online: 1 September 2009
Abstract
Martensitic transformations originate from the interaction of the short-wave
(atomic plane shuffling) and long-wave (homogeneous deformation) processes. The mutual role of
these movements is examined with the aim to elucidate formation mechanisms of the structures with
lower symmetry at the atomic level. Generic many-body potentials differing in the stability of
basic simple structures is employed in the calculations of the system energies in the course of
phase transition.
© Owned by the authors, published by EDP Sciences 2009
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