Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
10628541 | Corrosion Science | 2005 | 10 Pages |
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.
Keywords
Related Topics
Physical Sciences and Engineering
Materials Science
Ceramics and Composites
Authors
M.M. Lohrengel, Chr. Rosenkranz,