Autor: |
Robert M. Moss, David M. Pickup, Alan V. Chadwick, T. Skinner, Robert J. Newport, A.M. Jones, Andrew D. Smith, S.W. Goatham, K.M. Wetherall |
Rok vydání: |
2008 |
Předmět: |
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Zdroj: |
Journal of Archaeological Science. 35:1317-1328 |
ISSN: |
0305-4403 |
Popis: |
This paper reports the results of an investigation into the mechanisms that have led to the build up of sulfuric acid in the timbers of the Mary Rose , with a particular focus on recently recovered timbers. Measurements have been made by sulfur and iron K-edge X-ray absorption near edge spectroscopy (XANES), X-ray microscopy and by X-ray diffraction (XRD). Results from S K-edge XANES studies reveal that the concentration of highly oxidised S decreases with depth into the timber, from ∼15 at.% of S at the surface to negligible levels after approximately 50 mm. Fe K-edge XANES reveals little variation with depth in which Fe 3+ ions are dominant. This sheds some light on the sulfur oxidation path, and indicates Fe 3+ ions are produced by the oxidation mechanisms that are currently underway. XRD studies have identified several mineral components that may form part of the oxidation chain. These are magnetite (Fe 3 O 4 ), jarosite (KFe 3 (SO 4 ) 2 (OH) 6 ) and calcite (CaCO 3 ). |
Databáze: |
OpenAIRE |
Externí odkaz: |
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