Abstract
Scale invariance in acicular martensites emerges as a consequence of a competition between the front velocity and the rate of nucleation of the martensite grains. A renormalization group for the stationary probability distribution of the martensite grain size, , has two fixed points—an unstable fixed point at , associated with a gamma distribution, and a stable (critical) fixed point at with a Lévy distribution, . Crossover functions and exponents governed by the unstable fixed point describe at intermediate . Acicular martensites thus represent a novel example of a flow towards self-organized criticality. Our results provide a method to compute dynamic quantities ( or ) from static optical micrographs of martensite grains.
- Received 15 February 1995
DOI:https://doi.org/10.1103/PhysRevLett.75.2164
©1995 American Physical Society