Atmospheric-pressure temperature-programmed reduction (t.p.r.) was use
d to follow in pyrolysed subbituminous coal the changes in amount of p
yrite and in organic sulfur groups as a function of temperature. At hi
gher pyrolysis temperatures, pyrite and aliphatic and mixed aliphatic-
aromatic sulfides disappeared systematically and more complex sulfur c
ompounds such as aromatic sulfides and simple thiophenic structures we
re formed.