The morphology of chars sampled from various laboratory-scale reactors
operating at temperatures from 800 to > 1400 degrees C, together with
chars collected directly in the flame zone in a full-scale pulverized
fuel combustion experiment, was examined. A coal and coal blend domin
ated by vitrinite-rich microlithotypes together with four coals domina
ted by inertinite-rich microlithotypes were used to produce the combus
tion chars. Char samples produced at temperatures above similar to 130
0 degrees C have a morphotype composition very similar to the composit
ion of the full-scale char samples, whereas the morphotype composition
s of those produced at similar to 1150 degrees C or lower are signific
antly different. Correlation between coal petrography and char morphol
ogy and determination of char reactivity should thus be attempted only
using chars produced at temperatures comparable with those for the in
tended use of the coal. A clear distinction between the high-temperatu
re char samples (burnout 50-60 wt% daf) emerges which is related mainl
y to the parent coal petrography and probably secondarily to the rank.
Vitrite, clarite and vitrinertite V may be correlated with the porous
tenuisphere and crassisphere morphotypes, whereas inertite, durite, v
itrinertite I, duroclarite and clarodurite may be correlated with the
crassinetwork-mixed-network-mixed morphotype group. Copyright (C) 1996
Elsevier Science Ltd.