The thermal decomposition of Fe-2(SO4)(3) in air has been investigated usin
g transmission Mossbauer spectroscopy, CEMS and X-ray powder diffraction. T
he hexagonal alpha-Fe2O3 and cubic beta-Fe2O3 with spinel structure have be
en identified as products of the decomposition. The influence of the Fe-2(S
O4)(3) particle size on the yield of beta-Fe2O3 in the final product is poi
nted out and discussed. The size of particles and the calcination temperatu
re are the most important kinetic factors determining the phase composition
(beta-Fe2O3/alpha-Fe2O3) of iron (III) oxide.