Previous analysis of ash generated during coal gasification using a hi
gh calcium coal (SUFCo) suggested that iron sulfide was the dominant s
ulfide species in the system. During a recent analysis of ash material
removed from a gasification pilot unit using Pittsburgh No. 8, a high
iron coal, sub-mu m to 5 mu m euhedral iron sulfide crystals were ide
ntified on the outer surface of the ash. X-ray diffraction suggests bo
th pyrrhotite and troilite were present in the ash. No other sulfides
were identified. Within the iron sulfide crystals were siliceous fly-a
sh particles. Possible modes of formation which include vapor depositi
on, accumulation and annealing of fume particles, or recrystallization
of iron sulfide droplets were investigated.