The mechanism of the thermal transformation of FeSO4.H2O in air has been st
udied under isothermal conditions at temperatures (150-460)degreesC using m
ainly Fe-57 Mossbauer spectroscopy and X-ray powder diffraction (XRD). Two
trends are typical for the thermal behaviour of FeSO4.H2O in air, a tendenc
y toward oxidation and dehydration. We suggested a new transformation model
consisting of two ways of oxidation, direct one and indirect one. Fe(OH)SO
4 was identified as a product of the direct way, Fe-2(SO4)(3) and superpara
magnetic: nanoparticles of gamma -Fe2O3 as products of the indirect way. Th
e suggested model of simultaneous reactions explains the unusual non-monoto
nous dependence of the oxidation level of the thermally treated samples on
temperature.