Effect of hydrostatic pressure on the migration of tilt grain boundaries in Sn- and Al-bicrystals

Abstract

The use of hydrostatic pressure as an intensive parameter for investigation of grain boundaries (GBs) migration in bicrystals is potentially important in gaining additional information on the mechanism of GB migration. This is because an analysis of the pressure dependence of the GB mobility yields a new activation parameter of the migration process, namely the activation volume V* which quantitatively is the difference between the volumes of the system in the ground and activated states. Only a few experiments to study the pressure dependence of GB mobility are known [1,2]. These experiments were made on polycrystalline materials. They provide the average data for all GBs in polycrystal and do not permit the determination of the connection between GB structure and value of activation volume V* of GB migration. In studying the mobility of single boundaries of a given type, there is the possibility of connecting the activation volume with the GB structural peculiarities, in particular, of determining the misorientation dependence of the activation volume, that is, of determining V* for GBs having various degrees of ordering.