VISCOSITY AND PHASE-TRANSFORMATION IN COAL ASH SLAGS NEAR AND BELOW THE TEMPERATURE OF CRITICAL VISCOSITY

The phase transformation of multicomponent aluminosilicates on liquidu s curves becomes an important parameter in the prediction of the slag behavior upon cooling. Three major factors are taken into consideratio n: (1) thermodynamic driving forces for a selection of stable phases o n liquidus curves, such as free energies of components at various temp eratures, (2) the effect of free energy of mixing on the tendency to p hase segregation in liquid solution on cooling, and (3) free energy ch ange at the solid-melt interface and entropy of fusion and their effec ts on the morphology of the crystalline phase(s). In order to identify the solid phase(s) crystallized from ash slag it is proposed, first, to calculate major binary free energy composition diagrams based on ma jor oxides in ash and, second, to select phase(s) with the free energy and composition constrained by free energy diagrams. It is postulated that the free energy of the solid-melt interface plays a significant role in the selection of crystal size; the small Delta G(int) constrai ns the formation of fine crystallites, while the large Delta G(int) in dicates the formation of large crystals in a slag. It is quite apparen t that the low Delta G(int) contributes to lowering the activation ene rgy of nucleation. Both examples, the nucleation of fine crystallites and the grwoth of large crystals, are evident in Beulah and Illinois N o. 6 ash slags. In ash slags the phase transformation may occur either by nucleation or by spinodal decomposition, both of which are recorde d in Beulah and Gascoyne ash slags. The spinodal decomposition causes a sharp increase of slag's viscosity. The differential thermal analysi s (DTA) technique shows endotherms in Pittsburgh No. 8 and Gascoyne Wh ite ash slags, on heating, near and above the temperature of critical viscosity that are assigned to the dissolution of solid phases into th e melt and anomalies in melt thermal conductivity, respectively.