Fly ash formation and behaviour during combustion of willow (supplemen
ted by 20 wt% of wood pellets) was studied experimentally in a 3-12 MW
circulating fluidized bed boiler. Particle size distributions in a si
ze range d(ae) < 8 mu m were obtained by a Berner low pressure impacto
r in the convection path at a temperature of 650 degrees C and downstr
eam the convection path (160 degrees C). For particles above 8 mu m si
ze analysis was performed from a cyclone sample collected at 160 degre
es C. Size distributions contained two distinctive modes. The major in
organic elements in the coarse mode particles (d(ae) > 1 mu m) formed
from the non-volatilised ash residue were Ca, K, P, Mg and S. The fine
ash particles (d(ae) < 1 mu m) formed from vaporised ash forming cons
tituents were composed of alkali (mainly potassium) sulphates, chlorid
es and, according to chemical equilibrium calculations, carbonates. K2
SO4 was condensed prior to our sampling station at 650 degrees C. Cond
ensed KCl and K2CO3 were observed only at the latter sampling station
at 160 degrees C. About 50% oi the coarse ash particles were deposited
on the heat exchanger surfaces between 650 degrees C and 160 degrees
C, whereas the concentration of the fine mode sulphate particles was n
ot observed to decrease from 650 degrees C to 160 degrees C. (C) 1998
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