Oxidation properties of sintered Fe-3 mass%SiO
2 (Fe-3SiO
2) as well as Fe-1.5 mass%Si alloy (Fe-1.5Si) and Fe, for comparison, were investigated at 1273 K for up to 7.2 ks in air and air containing 10.5 vol%H
2O (air-10.5H
2O). In air-10.5H
2O, the Fe-3SiO
2 was oxidized faster than in air and also than the Fe-1.5Si in air-10.5H
2O. The scale was composed of a duplex structure, an inner FeO+Fe
2SiO
4 and an outer Fe-oxides layers, where many voids existed in both layers. The similar scale structure containing voids was observed for the Fe-3SiO
2 in air. Marker experiment with a small Pt wire was carried out for the Fe-3SiO
2 oxidized in air-10.5 vol%H
2O and the Pt-marker located between the inner and outer layers, suggesting that the inner layer grows due to inward migration of oxygen and the outer layer due to outward iron diffusion. In both air and air-10.5H
2O Fe showed a parabolic oxidation, forming exclusively an outer Fe-oxides scale. It was suggested that SiO
2, which changed to FeO+Fe
2SiO
4, acts as an obstacle for the outer layer recession, leading a formation of voids in the inner layer. Oxygen used to form the inner FeO+Fe
2SiO
4 layer was supplied by the dissociation of outer Fe-oxides, leaving voids, probably by a perforating dissociation mechanism. Both oxygen and water molecules could be diffusing species through the void.
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