期刊
JOURNAL OF THE AMERICAN CERAMIC SOCIETY
卷 87, 期 6, 页码 1102-1109出版社
AMER CERAMIC SOC
DOI: 10.1111/j.1551-2916.2004.01102.x
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Superplastic-like flow in a fine-grained MgAl2O4 polycrystal exhibits strain softening and hardening, which cannot be ascribed to cavity damage and grain growth during deformation, respectively. The softening and hardening can be related to a change in the internal stress, which depends on a decrease and an increase in the density of the intragranular dislocations, respectively, whose motion contributes to the relaxation of stress concentrations exerted through the predominant deformation mechanism of grain-boundary sliding. In these two regions, the rate of deformation is controlled by the continuous recovery of the dislocations limited by lattice diffusion of the oxygen ions.
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