Our recently developed model for the viscosity of silicate melts is applied to describe and predict the viscosities of oxide melts containing iron oxide. In the present study, the viscosity experimental data under the reduced atmosphere, which is Fe saturation condition were critically reviewed and three pairs of adjustable model parameters related to ‘FeO’ were optimized to best reproduce all experimental data in the FeO–SiO₂–Al₂O₃–CaO–MgO–Na₂O–MnO–Ti₂O₃–TiO₂ system. The viscosities of a wide compositional and temperature range of binary, ternary and multicomponent melts were well reproduced by the present model within the scatter of experimental data.

我们最近开发的硅酸盐熔体粘度模型用于描述和预测含氧化铁的氧化物熔体的粘度。在本研究中，严格审查了还原气氛下（Fe饱和条件）下的粘度实验数据，并优化了三对与“ FeO”有关的可调模型参数，以最佳地再现FeO-SiO ₂ -Al中的所有实验数据。₂ O ₃ -CaO-MgO-Na ₂ O-MnO-Ti ₂ O ₃ -TiO ₂体系。在分散的实验数据范围内，本模型很好地再现了二元，三元和多组分熔体的广泛组成和温度范围内的粘度。