Abstract
A thermodynamic model for predicting sulphur distribution ratio L
S between CaO–FeO–Fe2O3–Al2O3–P2O5 slags and liquid iron, i.e. the ion and molecule coexistence theory (IMCT)–L
S model, has been developed for slags in a large variation range of slag oxidisation ability based on the IMCT. The developed IMCT–L
S model has been verified with measured data of oxygen, phosphorus and sulphur distribution equilibria between the slags and liquid iron from the literature. The results indicate that the desulphurisation reaction is mainly controlled by reaction (CaO)+[S] = (CaS)+[O] in the reducing zone with the optimised standard molar Gibbs free energy change of
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