Ca-alpha -sialon compacts pressureless-sintered to intermediate temperature
s, which consisted of both alpha -sialon and unreacted alpha -Si3N4 grains,
were investigated with transmission electron microscopy for an overall com
position Ca1.8Si6.6Al5.4O1.8N14.2. Special attention was paid to identifica
tion of the possible crystallographic orientation between alpha -sialon and
the alpha -Si3N4 particles. In contrast to the frequently occurring hetero
epitaxial nucleation of alpha -sialon in rare-earth-doped samples with low
x values, this study showed that most of the newly formed alpha -sialon gra
ins had no epitaxial orientation relationship with the alpha -Si3N4 particl
es, suggesting nonepitaxial heterogeneous nucleation to be a more probable
mechanism for the Ca-alpha -sialon phase with high Ca concentrations.