Abstract

High-temperature sulfidation behavior of Fe-Mo alloys (containing 10 and 20 at.% Mo) was studied over the temperature range of 70000 °C above a pure sulfur pool with the sulfur-vapor of 10 2–10 5 Pa. The sulfidation kinetics followed the parabolic rate law in all cases. The corrosion rates increased with increasing temperature and sulfur pressure but decreased with increasing Mo content. The scales formed on the alloys were complex and bilayered, consisting of an outer layer of iron sulfide (FeS/Fe 1 x S) and an inner heterophasic layer of mostly FeMo 4S 6, FeMo 2S 4, Fe 1 x S, MoS 2 (only detected at P s 2 = 10 5 Pa) and uncorroded Fe 3Mo 2. Platinum markers were located at the interface between the inner and outer scales, suggesting that the outer scale grew by the outward transport of an Fe ion and the inner scale grew by the inward S diffusion, as similar to the results in the literature.

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