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Phys Rev Lett ; 84(25): 5784-7, 2000 Jun 19.
Artículo en Inglés | MEDLINE | ID: mdl-10991054

RESUMEN

The method of Parrinello and Rahman is generalized to include slip in addition to deformation of the simulation cell. Equations of motion are derived, and a microscopic expression for traction is introduced. Lagrangian constraints are imposed so that the combination of deformation and slip conform to the invariant plane shear characteristic of martensites. Simulation of a model transformation demonstrates the nucleation and propagation of a glissile dislocation interface.

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