Fired pure Fe2O3 and 0.5-5.0% MgO-doped Fe2O3 compacts, were isotherma
lly reduced with CO at 1173-1473 K. The course of reduction was follow
ed up by thermogravimetric technique. The structure of compacts were m
icroscopically examined while the different phases were identified by
X-ray diffraction analysis. Mercury pressure porosimeter was used to c
haracterize the pore structures. The isothermal reduction curves obtai
ned showed that MgO revealed different effects on the reduction behavi
our of Fe2O3. At the initial stages up 25% extents, the doping of MgO
showed no measurable influence on the reduction process. At the interm
ediate stages (25-85% extents), the doping of 0.5% MgO retarded the re
duction while the presence of 1.0% MgO promoted the reduction of Fe2O3
. The retardation and promotion effects were increased with the extent
of reduction and decreased with rise in temperatures. At final stages
of reduction, a slowing down in the rate due to the doping of MgO was
observed which was attributed to the formation of hardly reducible ma
gnesiowustite phase. The rate controlling step in the reduction proces
s was determined from the values of apparent activation energy, gas-so
lid mathematical formulations and the microstructure of partially redu
ced compacts. It was found that the reduction was controlled by a comb
ined effects of gaseous diffusion and interfacial chemical reaction at
the initial stages. While at the latter stages, a solid-state diffusi
on is contributed to interfacial chemical reaction as the rate control
ling mechanism depending on MgO content in compacts.