Abstract

Stationary regimes of the motion of phase boundaries accompanied by the heat release have been investigated. The heat produced can accelerate the phase boundary motion which in many two-phase systems is thermally activated (an example of practical importance being the grain boundary motion in the process of recrystallisation). This in turn increases the heat production rate. A system involved in this avalanche-like process can be stabilised by the heat removal via heat conductivity and heat exchange with the thermal bath establishing a stationary regime of the phase boundary motion. Both the temperature distribution around a stationarily moving phase boundary and its velocity have been analysed self-consistently. The conditions for the existence of one or two stationary regimes of the phase boundary motion have been obtained and the possibility of transitions between the two regimes accompanied by a jump-like change of the phase boundary velocity has been discussed.

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