Structure evolution of h.c.p./c.c.p. metal oxide interfaces in solid-state reactions

C Li1, G Habler1, T Griffiths1

  • 1Department of Lithospheric Research, University of Vienna, Althanstrasse 14, Vienna, 1090, Austria.

Summary

Interface migration in the Al2O3/MgAl2O4/MgO system is driven by partial dislocation glide, enabling cation exchange and zipper-like propagation. This process leads to MgAl2O4 grain growth and coarsening, offering insights into solid-state reactions.

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