Metastability in the MgAl₂O₄-Al₂O₃ system
Abstract
Aluminum oxide must take a spinel form (γ-Al2O3) at elevated temperatures in order for extensive solid solution to form between MgAl2O4 and α-Al2O3. The solvus line between MgAl2O4 and Al2O3 has been defined at 79.6 wt% AI2O3 at 1500°C, 83.0 wt% Al2O3 at 1600°C, and 86.5 wt% Al2O3 at 1700°C. A metastable region has been defined at temperatures up to 1700°C which could have significant implications for material processing and properties. Additionally, initial processing could have major implications on final chemistry.
Recommended Citation
K. R. Wilkerson et al., "Metastability in the MgAl₂O₄-Al₂O₃ system," Proceedings of the 13th Biennial Worldwide Congress on Refractories 2013 (2013, Victoria, Canada), pp. 303 - 308, John Wiley & Sons Inc., Sep 2014.
The definitive version is available at https://doi.org/10.1002/9781118837009.ch53
Meeting Name
13th Biennial Worldwide Congress on Refractories 2013 (2013: Sep. 10-13, Victoria, Canada)
Department(s)
Materials Science and Engineering
Keywords and Phrases
Aluminum oxides; Elevated temperature; Material processing; Metastabilities; Metastable region, Aluminum
International Standard Book Number (ISBN)
978-111883703-0
Document Type
Article - Conference proceedings
Document Version
Citation
File Type
text
Language(s)
English
Rights
© 2014 The American Ceramic Society, All rights reserved.
Publication Date
13 Sep 2014
Comments
Chapter 53