Abstract
Phase transitions of gallium orthophosphate (GaPO4) have been studied by thermal analysis between ambient temperature and 1100°C. In situ X-ray powder diffraction at selected temperatures confirmed the three known polymorphic structure types of low-quartz, low-cristobalite and high-cristobalite GaPO4, respectively. Whereas the as-synthesized powder retained its low-quartz structure up to 970°C, powders cycled up to 1100°C exhibited three phase transitions (low-cristobalite → (≈620°C) high-cristobalite → (≈800°C) low-quartz → (≈970°C) high-cristobalite) while heating up and one phase transition (high-cristobalite → (≈590°C) low-cristobalite) while cooling down. However, the high-cristobalite/low-quartz heating transformation was found to be kinetically hindered. Isothermal in situ X-ray powder diffraction revealed a remarkable temperature dependence of this reaction kinetics.
Item Type: | Journal article |
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Faculties: | Geosciences > Department of Earth and Environmental Sciences > Crystallography and Materials Science |
Subjects: | 500 Science > 550 Earth sciences and geology |
Language: | English |
Item ID: | 18496 |
Date Deposited: | 10. Mar 2014, 14:09 |
Last Modified: | 29. Apr 2016, 09:15 |