The ash transformation and deposition behavior of pyrite and illite, w
hich are commonly identified with slagging, are influenced by the mann
er in which the minerals occur in the fuel. An enhanced computer contr
olled scanning electron microscopy technique was used to analyze the m
ineral content of individual coal particles in samples of two pulveriz
ed fuels. The particle-by-particle analysis determined whether individ
ual mineral grains were included or excluded. It also provided informa
tion on which mineral species were likely to be found in the same coal
particle with pyrite or illite. Illite typically appeared as included
particles and was associated with a variety of other silicate species
. In contrast, pyrite tended not to associate with other minerals and
showed a significantly higher fraction of excluded particles. Such det
ailed observations of coal mineral distributions and associations prov
ide additional insight into the mechanisms which govern fly ash format
ion.