$Fe_2O_3$ was reduced over the temperature range of 600-100$0^{\circ}C$ in both the atmospheres for the Fe-stable and FeO-stable states. It was found that the reduction follows first order kinetics and the reduction of $Fe_3O_3$ to $Fe_3O_4$ is the rate-control...
$Fe_2O_3$ was reduced over the temperature range of 600-100$0^{\circ}C$ in both the atmospheres for the Fe-stable and FeO-stable states. It was found that the reduction follows first order kinetics and the reduction of $Fe_3O_3$ to $Fe_3O_4$ is the rate-controlling step.
$Fe_2O_3$ was reduced over the temperature range of 600-100$0^{\circ}C$ in both the atmospheres for the Fe-stable and FeO-stable states. It was found that the reduction follows first order kinetics and the reduction of $Fe_3O_3$ to $Fe_3O_4$ is the rate-controlling step.
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