Abstract
The X-ray absorption fine structure (XAFS) spectrum of pure goethite around the Fe K absorption edge and that of the protective rust layer formed on weathering steel exposed for 17 years in an atmospheric environment around the Cr K edge, have been examined using synchrotron radiation X-rays. It was found that the rust layer on the weathering steel mainly consisted of Cr-goethite. By examining the fine structure at the Cr K edge and the Fe K edge, we concluded that Cr3+ in the rust layer is coordinated with O2+ and is positioned in the double chains of vacant sites in the network of FeO 3(OH)3 octahedra in the goethite crystal. This Cr 3+ site indicates that the protective effect of the rust layer is due to the dense aggregation of fine crystals of Cr-goethite with cation selectivity.
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Yamashita, M., Konishi, H., Mizuki, J., & Uchida, H. (2004). Nanostructure of protective rust layer on weathering steel examined using synchrotron radiation X-rays. Materials Transactions, 45(6), 1920–1924. https://doi.org/10.2320/matertrans.45.1920
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