Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
5440119 | Corrosion Science | 2016 | 12 Pages |
Abstract
Greigite (Fe3S4) and/or mackinawite (FeS1âx) are observed at the outer border of the corrosion product layer. The presence of mackinawite is discussed relatively to the establishment of stable anoxic burial conditions. The nails from the subaquatic site present pyrite globules in the transformed medium. The formation of pyrite (FeS2) is attributed to the proximity of wood. The iron sulphides formation may also be explained by the presence of sulphate-reducing bacteria in the burial environment.
Related Topics
Physical Sciences and Engineering
Materials Science
Ceramics and Composites
Authors
Sophie Grousset, Marine Bayle, Alexandre Dauzeres, Didier Crusset, Valérie Deydier, Yannick Linard, Philippe Dillmann, Florence Mercier-Bion, Delphine Neff,