The N 1s spectra from four pulverized Australian coals and their chars prod
uced by pyrolysis for 2 s at 1100 degrees C and 1300 degrees C in a pressur
ized furnace are evaluated, with particular reference to the binding energy
region above 402 eV. The spectra for the feed coals were broadly similar t
o those reported previously for bituminous coals, in that pyrrolic nitrogen
was the dominant functional form in each case. A minor component between 4
03 and 404.5 eV was assigned to ammonium nitrogen in liberated mineral matt
er. The N Is spectra for the chars were also broadly similar to those expec
ted for pyrolysis under intermediate residence time conditions, in that the
proportion of pyrrolic nitrogen was no more than half that for the feed co
al. Intensity in the 402-404.5 eV region was more consistent with N-O speci
es formed post-pyrolysis than similar species formed as intermediates durin
g pyrolysis, Copyright (C) 1999 John Wiley & Sons, Ltd.