Thermochemical decomposition of pyrite in air-gas medium has been studied b
y means of PI IOM-Q 1500D Derivatograph. The derivatograms have been obtain
ed at a heating rate of 5 K min(-1) and air flowrate of 25 l h(-1) to final
temperatures of 833, 933 and 1273 K, chosen on the basis of the stepwise o
xidation of pyrite. The solid product is analyzed using X-ray powder diffra
ction and Mossbauer spectrometer techniques. The formation of nonstoichiome
tric sulfides (pyrrhotines) as intermediates has been confirmed. The second
stage of decomposition is the oxidation of these pyrrhotines to hematite.
The recorded weight losses are lower than the theoretically possible becaus
e of the formed nonstoichiometric iron sulfides. The complicated structure
of the intermediate products has been confirmed by means of other technique
s.