Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
1469054 | Corrosion Science | 2014 | 4 Pages |
Abstract
To simulate the atmospheric corrosion of steels, magnetite (Fe3O4) rust particles were prepared in aqueous media containing iron powder (α-Fe) and artificial α-, β- and γ-FeOOH particles at pH = 6.0 and 50 °C for 24 h. The Fe3O4 formation was not recognized by treating the iron powder with α-FeOOH. When the iron powder treated with β- and γ-FeOOH, these materials were dissolved to generate Fe3O4 and α-FeOOH particles. The amount of formed Fe3O4 particles was in the order of β-FeOOH > γ-FeOOH ≫ α-FeOOH, which was strongly related to the density and solubility of FeOOH.
Related Topics
Physical Sciences and Engineering
Materials Science
Ceramics and Composites
Authors
Hidekazu Tanaka, Ryohei Mishima, Nagisa Hatanaka, Tatsuo Ishikawa, Takenori Nakayama,