Abstract

Hydrated chromic oxide was prepared by the reduction of potassium dichromate in an autoclave using sucrose. The thermal dehydration of the parent gel in different atmospheres was studied comparatively using the techniques of thermal gravimetry, differential thermal analysis, X-ray diffraction analysis, FT-IR spectroscopy, and gas adsorption. The results of thermogravimetric and differential thermal analysis show that the temperature at which the glow phenomenon occurs is dependent on the gaseous atmosphere in the heat-treatment process and increases in the following order: air, nitrogen, and carbon dioxide. When heated in CO 2, the parent gel is transformed into crystalline α-Cr 2O 3 going through the phase of amorphous Cr 2O 3. In air, however, it is decomposed directly into crystalline α-Cr 2O 3 without going through the amorphous Cr 2O 3 phase. It is also found that microcrystallites of α-Cr 2O 3 have been formed before the glow phenomenon occurs at 390 °C in air and at 590 °C in CO 2, respectively. The mechanism for thermal dehydration in air and CO 2 is discussed.

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