Devitrification of the Grain Boundary Glassy Phase in a High‐Alumina Ceramic Substrate
Cynthia A. Powell‐Doǧan, A. H. Heuer, H. M. O’Bryan
Abstract
Cynthia A. Powell‐Doǧan, A. H. Heuer, H. M. O’Bryan
Abstract
Devitrification of the (Na, Mg, Ca) aluminosilicate glass phase in a high‐alumina (>99%) ceramic substrate has been studied by TEM. MgAl 2 O 4 (spinel) and a Ca‐rich plagio‐clase (a solid solution between CaAl 2 Si 2 0 8 (anorthite) and NaAlSi 3 O 8 (albite)) are the dominant crystalline phases. Significant spatial variability exists both in the extent of crystallization and in the glass composition.
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Devitrification of the (Na, Mg, Ca) aluminosilicate glass phase in a high‐alumina (>99%) ceramic substrate has been studied by TEM. MgAl 2 O 4 (spinel) and a Ca‐rich plagio‐clase (a solid solution between CaAl 2 Si 2 0 8 (anorthite) and NaAlSi 3 O 8 (albite)) are the dominant crystalline phases. Significant spatial variability exists both in the extent of crystallization and in the glass composition.
Key concepts: Devitrification, Anorthite, Spinel, Mineralogy, Albite, Materials science, Crystallization, Aluminosilicate