Spectroscopic and computational modeling reveals iron oxide phase stability in hydrogen reducing environments, indicating trace oxygen preserves protective layers.
This study combines density functional theory (DFT) and ab initio thermodynamics calculations with X-ray photoelectron spectroscopy (XPS) investigations to identify the reduction properties of the Fe₂O₃ (001) surface with implications for corrosion resistance, hydrogen transport, and energy safety. Ab initio thermodynamics modeling predicts fully hydroxylated surface stability across a broad range of pressures (1 × 10⁻²³ to 1 × 10⁵ mbar) and temperatures below 700 K, consistent with previous experimental studies. Above 800 K, exposures to 1 × 10⁻⁴ mbar H₂, 1 × 10⁻⁴ mbar O₂, or 1 × 10⁻⁴ mbar H₂ + 1 × 10⁻⁴ mbar O₂ each yield unique XPS signals indicating a loss of -OH coverage, aligning with DFT predictions. Insight into the mechanism of reduction as a function of H₂ exposure is provided, as well as conditions that promote further reduction toward Fe₃O₄. Theoretical and experimental investigations indicate the ability to maintain the Fe₂O₃ protective layer of iron oxides that have been exposed to H₂ environments by including trace amounts of aqueous O₂.
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Hudson et al. (2025) studied this question.
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