Abstract
9Cr–1Mo steel forms in CO2 at 550 °C a duplex oxide layer containing an outer magnetite scale and an inner Fe–Cr rich spinel scale. The inner spinel oxide layer is formed according to a void-induced oxidation mechanism. The kinetics of the total oxide growth is simulated from the proposed oxidation model. It is found that the rate limiting step of the total oxide growth is iron diffusion through high diffusion paths such as oxide grain boundaries in the inner Fe–Cr rich spinel oxide layer. In the proposed oxidation model, a network of nanometric high diffusion paths through the oxide layer allows the very fast supply of CO2 inside pores formed at the oxide/metal interface. Its existence is demonstrated to be physically realistic and allows explaining several observed physical features evolving in the oxide layer with time.
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Acknowledgments
The authors are thankful to Mme G. Moine and Mr. A. Abdelouahab for having carried out the corrosion tests and the FESEM pictures.
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Rouillard, F., Martinelli, L. Corrosion of 9Cr Steel in CO2 at Intermediate Temperature III: Modelling and Simulation of Void-induced Duplex Oxide Growth. Oxid Met 77, 71–83 (2012). https://doi.org/10.1007/s11085-011-9273-3
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DOI: https://doi.org/10.1007/s11085-011-9273-3