In situ Raman spectroscopy, surface-enhanced Raman spectroscopy, scanning electron microscopy (SEM), and measurements of corrosion potential were used to investigate the films formed on iron in 288°C water with dissolved oxygen concentrations that ranged from 0 to 208 ppb. The film that formed on iron immersed in water containing 0 to 22 ppb oxygen consisted mostly of faceted, loosely packed particles of magnetite (Fe3O4). It was inferred from SEM and Raman spectra that the film on iron was composed of two layers. The faceted particles of Fe3O4 made up the outer layer and an inner conformal layer of Fe3O4 formed the inner layer. Passivation of the iron surface began at dissolved oxygen concentrations of 8 ppb and was a two-step process. First, between 8 ppb and 22 ppb oxygen, there was an increase in the protectiveness of the Fe3O4. Second, between 22 ppb and 53 ppb, the combination of SEM and Raman spectra suggested that the outer surface of Fe3O4 transformed to α-Fe2O3, which completed passivation.

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