A mechanistic study is detailed in which coal ash is heated with its s
hrinkage measured continuously up to a temperature of 1600 degrees C.
The temperatures corresponding to the rapid rate of shrinkage correspo
nd to the formation of eutectics identified on phase diagrams. Samples
were therefore heated to these temperatures, cooled rapidly and exami
ned using a scanning electron microscope (SEM) to identify the associa
ted chemical and physical changes. The progressive changes in the rang
e of chemical composition (from SEM), the extent of undissolved ash pa
rticles and porosity were then quantified and related to homogenisatio
n, viscosity and ash fusion mechanisms. Alternate ash fusion temperatu
res based on different levels of shrinkage have also been suggested to
characterise the ash deposition tendency of the coals. (C) 1998 Elsev
ier Science B.V. All rights reserved.