Several iron oxides and mixtures of iron oxides have been prepared by
heating the product of a sol-gel reaction between iron(III) nitrate an
d ethylene glycol in different atmospheres and at different temperatur
es. The materials were characterized by Mossbauer spectroscopy, powder
X-ray diffraction, and transmission electron microscopy. Ferrous iron
was found to be present in an appreciable amount in the products of t
he sol-gel reaction, but its origin is not yet understood. Heating at
300-degrees-C in N2 atmosphere, cooling in air to ambient temperature,
and heating again at 300-degrees-C in static air produced single-phas
e maghemite with a mean crystallite diameter (MCD) of 18 nm. Well crys
tallized hematite (MCD = 110 nm) was obtained at 300-degrees-C in O2 a
tmosphere. Mixtures of poorly crystallized maghemite and magnetite wer
e observed to exhibit room-temperature Mossbauer spectra which closely
resemble those reported for sodium-modified maghemite. A mixture of m
agnetite, wustite, and metallic iron was obtained by heating at 800-de
grees-C in N2 atmosphere. (C) 1994 Academic Press, Inc.