Article ID Journal Published Year Pages File Type
10628541 Corrosion Science 2005 10 Pages PDF
Abstract
A transition from predominant oxygen evolution to predominant iron dissolution was found in the range from 5 to 30 A/cm2. At current densities >35 A/cm2 the oxygen evolution is reduced to some percent of the total current. The Fe3+/Fe2+ formation ratio increases to 2, corresponding to a dissolution of Fe3O4.
Related Topics
Physical Sciences and Engineering Materials Science Ceramics and Composites
Authors
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