IR and EXAFS spectroscopies were used to study the products of the hyd
rolysis of iron(lll) sulfate. A hypothesis for the structure of amorph
ous basic iron sulfate is made from a comparison of its IR spectra and
radial atomic distribution curves with the corresponding data for jar
osite. Analysis of the interatomic distances and manifestations of the
sulfate ion in the low- and high-temperature IR spectra shows that in
the amorphous product of the hydrolysis, unlike in the jarosite, the
sulfate ion is not involved in the first coordination sphere of the ir
an atoms, but is held in the structure by hydrogen bonds. Reasons for
the high catalyzing ability of the amorphous basic iron sulfate are su
ggested.