A MOSSBAUER STUDY OF THE BEHAVIOR OF IRON CATIONS IN IRON OXIDE-CONTAINING MELTS AT 1400-DEGREES-C

A Mossbauer spectroscopy technique has been developed to study the distribution of iron cations in slag melts as a function of distance from a reaction surface. A wide range of slag compositions of interest to the nonferrous smelting industry was reduced and oxidized using mixtures of CO, CO2, and Ar. Mossbauer spectra were collected on quenched slag samples for varying conditions between iron saturation and magnetite saturation, 1(10(-13)) to 4(10(-6)) atm P(O2) at 1400-degrees-C. Slag sections were analyzed with a spatial resolution of approximately 500 mum, and details of the ferric and ferrous distribution at the surface and in subsurface regions were studied. In FexO-SiO2-Al2O3 melts exposed to a reducing gas mixture, there is a gradient in ferric iron concentration decreasing toward the surface. In the FexO-Al2O3 melt, the reduction of ferric anions at the surface appears to release O2- ions, which increases the coordination of Fe2+. However, in the presence of silica, which is surface active and acidic, reduction of ferric iron does not lead to an excess of O2- at the surface. Lime has a dramatically different effect. It reverses the ferric gradient so that, even during reduction, the ferric concentration at the surface is enhanced. Ferric oxide is surface active in these melts, and under certain conditions. liquid-phase mass transfer is rapid enough to replenish the surface. The presence of a polymer-forming ion, Fe3+, at the surface results in a scarcity of O2- ions and a reduced coordination of Fe2+. In the presence of both SiO2 and CaO, the behavior of ferric iron during reduction depends, to an extent, on the CaO/SiO2 ratio. The behavior of iron oxide melts during reduction is very complex, and the surface-active nature of SiO2 and ferric oxide has a significant influence on the reaction. A quantitative analysis of the overall reaction would have to take these factors into account.