The chemical speciation of iron in combustion-derived ash is an important factor in determining the likelihood of ash deposit formation and buildup. In this study, the transformation of iron were examined in ash produced by the combustion of a beneficiated Pittsburgh no. 8 bituminous coal under a range of oxygen concentration ranging from 0% to 100% O(2) in a drop tube furnace. The speciation of iron was found to be strongly dependent upon ash particle size, with the lowest fraction of glassy state iron found in the largest ash particles. Both the fraction of iron in a glassy state and the ratio of Fe(+++)(glass)/Fe(++)(glass) increased with increasing O(2) concentration in the furnace. For the submicron ash particles, about 10% of the iron is formed by direct disintegration of pyrite and pyrrhotite during combustion. Most of the iron is however, present as Fe(+++)(glass), which results from the vaporization, recondensation, and coagulation of iron and silicates. For ash particles with size between 1 and 9 microns, most of the ash derives from mineral coalescence within the reacting char, with additional contribution from extraneous minerals. The fraction of glassy iron in those particles is high because of the high contact probability between iron melt and silicates. For the coarsest ash particles with size greater than 9 microns, extraneous pyrite is changed into hematite, and iron in the core of the char is changed into a glassy state. (C) 2008 Elsevier Ltd. All rights reserved.