1985 年 49 巻 5 号 p. 357-363
In relation to the alkali recycle in a blast-furnace, the rate of vaporization of potassium from slags was investigated. At temperatures between 1723 and 1923 K and under argon atmosphere, the mass loss from the slag melted in a graphite crucible as a reductant was continuously measured by means of a thermo-balance.
At lower temperatures, the mass loss was due almost to the vaporization of K, but at higher temperatures, particularly in the slags with high concentrations of SiO2, there was concurrent evolution of K and SiO from the slag. The rate of vaporization was represented by the first-order-type rate equation. The rate constant were in the range from 9.5×10−8 to 4.6×10−7 m/s at 1773 K. It was found that the rate constant increased with increasing basicity of blast-furnace-type slags. The apparent activation energy varied from 173 to 314 kJ/mol with slag composition. It was observed that the rate of K vaporization was strongly dependent on the wetting of slag on the graphite crucible wall. The vaporization of K from the slag was controlled by the chemical processes at the slag-graphite interface.