Measurements have been made of the chemical diffusion coefficient of oxygen
in liquid iron oxide at temperatures from 1673 to 1888 K and in a calcium
ferrite (Fe/Ca = 2.57) at temperatures from 1573 to 1873 K, A gravimetric m
ethod was used to measure the oxygen uptake during the oxidation of the mel
ts by oxygen or CO2-CO mixtures. The rate was shown to be controlled by mas
s transfer in the liquid melt. The chemical diffusivity of oxygen in liquid
iron oxide at oxygen potential between air and oxygen was found to be 4.2
+/- 0.3 X 10(-3) cm(2)/s at 1888 K. That in iron oxide at oxidation state c
lose to iron saturation was established to be given by the empirical expres
sion log D = -6220/T + 1.12 for temperatures between 1673 and 1773 K. For t
he calcium ferrite (Fe/Ca = 2.57) at oxygen potential between air and oxyge
n, the diffusivity of oxygen was found to be given by log D = -1760/T - 1.3
1 for temperatures between 1673 and 1873 K.