Abstract
AbstractThis paper reports a study and discusses the role of Fe ions in the inhibition of corrosion of iron phosphate glasses. The structure of the 40Fe2O3–60P2O5 (mol%) glass, having a confirmed dissolution rate in aqueous solution at 90°C superior to borosilicate glasses, was investigated. Samples were crystallized at characteristic temperatures defined by differential thermal analysis and analyzed by X‐ray diffraction. Crystalline phases of Fe2Fe[P2O7]2 and Fe4[P2O7]3 were detected. The hyperfine parameters from the Mössbauer spectrum indicate that both Fe2+ and Fe3+ ions are in octahedral coordination, and 18% of the Fe3+ ions in the starting batch are reduced to Fe2+ ions after melting. The broad and symmetric spectra centered in g≈2.0 from the EPR measurements indicate the presence of two or more Fe interacting ions occupying sites of relatively high local symmetry.
Published Version
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