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Microstructure evolution by ECAP was evaluated in relation to deformation behavior.
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The microstructure evolution occurs by recovery, recrystallization and grain growth phenomena.
This microstructure evolution occurs by the motion of twin boundaries and the nucleation and annihilation of twins in the hierarchical microstructure.
Phase-field simulations carried out using a multi phase-field approach deliver insight into the microstructure evolution driven by the loss of coherency of the γ′ precipitates, which is induced by the accumulation of dislocations at the γ/γ′ interfaces.
The microstructure evolution operates mainly by shape changes and alignments of precipitates, but also by splitting of precipitates initially elongated along directions perpendicular to the stress-induced, elastically favorable directions.
Microstructure evolution was observed by optical microscope and scanning electron microscope.
A concerted microstructure evolution is possible by enhancement or suppression of the melt convection.
The mechanism of microstructure evolution is discussed by considering the thermodynamic and kinetic factors.
The microstructure evolution was investigated by cross-sectional transmission electron microscopy.
The hydration features associated with microstructure evolution are identified by NCEIM, Micro-Raman spectra and heat evolution test.
Texture and microstructure evolution were analysed by decoupling the effects of imposed shear and of dynamic recrystallization.
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