The ash fusion characteristics and mineral behaviour of three kinds of indi
vidual coal ash and a series of two-component blended ashes were studied. T
he ash fusibility and chemical composition were measured and analysed. The
samples were heated progressively from 800 degrees C to the initial deforma
tion temperature (IT) at 100 degrees C intervals in reducing atmosphere. Mi
neral composition and type at each temperature interval were determined by
X-ray diffraction (XRD) analysis. The results show that blended ash softeni
ng temperatures do not change linearly with blending ratios. It can lie bet
ween or lower or higher than that of the individual parent coals. Some comb
inations of component coal's mineral produce low-melting eutectic minerals
at high temperature and this is the main reason causing the non-arithmetic
averaging of softening temperature of blended ash. It is consistent with th
e results from the ternary system phase diagram. (C) 1999 Elsevier Science
Ltd. All rights reserved.