Martensites

Ferrite and Martensite
Martensites are metastable configurations, typically formed by quenching a crystalline solid past a structural transition. Structurally they are quite distinctive, having a well defined substructure consisting of regular arrays of either twins or slipped regions occurring over length scales much larger than atomic dimensions. Also the nucleation and growth kinetics of Martensites differ in-general from that of the equilibrium phase. Often their formation is athermal  viz. the amount of Martensite produced at any temperature is independent of time and in many system the Martensite front grows ballistically at speeds comparable to the speed of sound. Martensites have been extensively studied by metallurgists because of their varied technological applications ranging from the heat-treatment of steels to the fabrication of smart structureswhich can be programmed to respond to external stimuli by changing their shape. The overall objective of our research on Martensites is to understand and interpret these empirical observations as well as build up a consistent picture of Martensite phenomenology from the point of view of non-equilibrium statistical mechanics.


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