Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
6335084 | Applied Geochemistry | 2014 | 14 Pages |
Abstract
The average thickness of oxidized iron, as measured by the average of distances from the original to the final metal surface, was 13 ± 1 and 15 ± 1 μm for the massive rod and the micro-overpack, respectively. The corresponding Fe amount is about twice the amount of Fe present in the corrosion products. Thus a significant Fe fraction migrated in the nearby clay, likely as Fe(II), and could act as a significant buffer of the electrochemical potential.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Michel L. Schlegel, Christian Bataillon, Florence Brucker, Cécile Blanc, Dimitri Prêt, Eddy Foy, Matthieu Chorro,