摘要
Treatments based on the immersion of iron artefacts in NaOH or KOH solutions with or without cathodic polarisation of the metal core, used for conservation purposes, were applied to Gallo-Roman iron ingots excavated from the Mediterranean Sea. The transformation of the initial layer of beta-Fe-2(OH)(3)Cl was followed with time. The resulting phases were characterised by a complete set of multi-scale complementary techniques. It could be demonstrated that the main process involved successively the transformation of beta-Fe-2(OH)(3)Cl into Fe(OH)(2) and the oxidation of Fe(OH)(2) into alpha-/delta-FeOOH and magnetite. Cathodic polarisation accelerated, via migration processes, the removal of chloride ions.
- 出版日期2011-8
- 单位中国地震局