Journal of the American Ceramic Society · 2008 · 11 citations · 41 references
Natural SciencesChemistryMaterials ScienceCrystal StructureInorganic ChemistrySolid-state ChemistryMetal OxidesOzone ChemistryCrystalline Phase FormationIn Situ X-ray DiffractionKinetic StabilityOzonePhase FormationThermal DecompositionThermal Decomposition ReactionsThermochemistry Of Oxides
Ozone gas in an ambient pressure was blown to Cr 2 O 3 powder. The higher oxides, CrO 3 , Cr 2 O 5 , Cr 5 O 12 , and Cr 3 O 8 , could be synthesized above 373 K. Both CrO 3 and Cr 2 O 5 were found by in situ X‐ray diffraction measurements. It was known that they could be produced only at high pressure of oxygen and at high temperatures. The CrO 3 formed was melted at 470 K in an ozone atmosphere and decomposed above 500 K. Because of thermal decomposition of ozone and the higher oxides, no higher oxides were formed above 660 K. The phase formation was discussed using the kinetic stability diagram.
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