Dg. Park et al., CRYSTALLIZATION OF PRECURSORS TO FORSTERITE AND CHROMIUM-DOPED FORSTERITE, Journal of the American Ceramic Society, 77(1), 1994, pp. 33-40
The pyrolysis and crystallization of poly(methacrylate) precursors and
xerogels of forsterite and chromium-doped forsterite were studied by
in situ high-temperature, dynamic X-ray diffraction and thermal analys
is. For both types of precursor, crystallization of forsterite occurre
d at lower temperature when doped with chromium. Also, exotherms above
700-degrees-C occurred 50-degrees-C lower when chromium was present.
When residual carbon in the xerogels was more than approximately 1%, a
n unidentified crystalline intermediate phase formed at approximately
800-degrees-C. Conversion of the intermediate phase to forsterite was
faster than amorphous material. Thus, full crystallinity was attained
at a lower temperature when the xerogels had some residual carbon.