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• W2793014767 abstract "Recent high temperature H2S corrosion study reported that a thermodynamically less stable iron oxide layer can also form in addition to iron sulfide. In this work, H2S corrosion experiments were conducted at 120 °C for different exposure times, ranging from 1 to 21 days. The inner layer was identified by Transmission Electron Microscopy (TEM) as Fe3O4 (magnetite); Fe3O4 was always present over time despite it being less stable than iron sulfide. The observed formation sequence of iron sulfide at high temperature was mackinawite → troilite → pyrrhotite → pyrite. The role of the different corrosion product layers in corrosion is discussed." @default.
• W2793014767 created "2018-03-29" @default.
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• W2793014767 date "2018-05-01" @default.
• W2793014767 modified "2023-10-02" @default.
• W2793014767 title "Formation of iron oxide and iron sulfide at high temperature and their effects on corrosion" @default.
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• W2793014767 doi "https://doi.org/10.1016/j.corsci.2018.02.045" @default.
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