Abstract
Davies et al. have shown that, when iron is oxidised at temperatures above 700°, the oxide film present on flat specimens contains mainly wüstite (FeO), in fact the three oxides FeO, Fe2O4 and Fe2O4 are all present, approximately in the ratio 95: 4: 1. Below 570°, FeO is not stable, as shown by the iron–oxygen equilibrium diagram2 and Collongues & Chaudron3 have shown that in vacuo wüstite decomposes to give iron and magnetite at temperatures below 570°. Wüstite formed as an oxide layer on iron oxidised at temperatures above 570° should also become unstable on cooling to room temperature. The following results show how the degree of wüstite breakdown can be easily estimated.
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