The temperature-programmed combustion of coal was studied and reactive
intermediates were observed by gas sampling directly above the sample
in a thermogravimetric analyser-mass spectrometer (t.g.a.-m.s.). Spec
ies detected included OCS, OCN, HCN and (CN)(2). NO levels observed at
the exit of the t.g.a. differed from those measured directly above th
e sample, the former usually being higher. This observation can be att
ributed to the conversion of volatile nitrogen-containing species to N
O by homogeneous gas-phase reactions. The temperature-programmed combu
stion of maceral concentrates was also studied, to assess differences
due to heterogeneity in the coal. The differences between the macerals
were in species detected and their relative concentrations. Fusinite
macerals tended to produce the highest levels of NO measured directly
above the sample, compared with vitrinites and semifusinites, and the
highest levels of sulfur species. The results are discussed in terms o
f the release of volatile nitrogen species and the reduction of NO pro
duced in char gasification on the surface and in the pores of the char
.