Phase transitions of gallium orthophosphate (GaPO4) have been studied by th
ermal analysis between ambient temperature and 1100 degrees C. In situ X-ra
y powder diffraction at selected temperatures confirmed the three known pol
ymorphic structure types of low-quartz, low-cristobalite and high-cristobal
ite GaPO4, respectively. Whereas the as-synthesized powder retained its low
-quartz structure up to 970 degrees C, powders cycled up to 1100 degrees C
exhibited three phase transitions (low-cristobalite --> (approximate to 620
degrees C) high-cristobalite --> (approximate to 800 degrees C) low-quartz
--> (approximate to 970 degrees C) high-cristobalite) while heating up and
one phase transition (high-cristobalite --> (approximate to 590 degrees C)
low-cristobalite) while cooling down. However, the high-cristobalite/low-q
uartz heating transformation was found to be kinetically hindered. Isotherm
al in situ X-ray powder diffraction revealed a remarkable temperature depen
dence of this reaction kinetics.