Above 5 degrees C, ferric sulfide disproportionates into mixtures of p
yrite (PY), pyrrhotite (PH), and elemental S, with the relative amount
s depending upon disproportionation temperature and time. The PH/PY mi
xtures are used as catalysts for coal liquefaction, with the optimum m
ixture corresponding to disproportionation at 200 degrees C for 1 h. R
eactions of Fe during disproportionation and liquefaction are postulat
ed and confirmed by AA, AES, and XRD. The iron loading has a nonlinear
effect on conversion and yield.