1977 Volume 85 Issue 981 Pages 242-247
Kinetics and mechanism of the eutectoid decomposition of spinel phase CuFe5O8 into CuFeO2 and Fe2O3 have been studied with special emphasis on the effects of Fe2O3-dissolution into and Fe2O3-precipitation from the spinet phase. Techniques employed are X-ray diffraction and optical microscopic analyses and Curie temperature measurement.
It is shown that the excess Fe2O3 over the stoichiometric composition checks the decomposition with different mechanisms depending on the temperature. Thus, Fe2O3-rich spinel separates CuFeO2+2Fe2O3 at 850°C, whereas at 500°C the excess Fe2O3 separates simultaneously with CuFeO2+2Fe2O3. Pre-precipitation of Fe2O3 from hypereutectoid spinet accelerated the rate of decomposition with a marked effect at 850°C. Kinetic analysis of the decomposition isotherms proposed that the effect of pre-precipitation should be attributed to the increased number of active sites for nucleation. The microscopic observations of the sintered bodies are in favor of this view.