4.5 Article

Darkening of lead- and iron-based pigments on late Gothic Italian wall paintings: Energy dispersive X-ray fluorescence, mu-Raman, and powder X-ray diffraction analyses for diagnosis: Presence of beta-PbO2 (plattnerite) and alpha-PbO2 (scrutinyite)

期刊

JOURNAL OF RAMAN SPECTROSCOPY
卷 51, 期 4, 页码 680-692

出版社

WILEY
DOI: 10.1002/jrs.5817

关键词

confocal Raman spectroscopy; haematite degradation; plattnerite; scrutinyite; wall paintings

资金

  1. MADyLIN project - Spanish Agency for Research AEI (MINEICO/FEDER-UE) [BIA2017-87063-P]

向作者/读者索取更多资源

This work reports the results of an extensive study carried out on the wall paintings preserved inside the Saint Stephen's chapel in Montani (Val Venosta, Bozen, Italy), by means of mu-Raman spectroscopy, portable X-ray fluorescence (XRF) spectrometry, and powder X-ray diffraction, in order to characterize materials and their alteration products that cause the blackening of paintings. In situ XRF analysis allowed identifying the areas of interest where the blackening appeared. The complementary analytical techniques allowed reconstructing a chromatic palette used by the artists that includes expensive pigments, such as lapis lazuli and cinnabar, indicating a wealthy client. Raman spectra at very low power recorded on blackened degraded samples showed the presence of a mixture of the two polymorphs of lead (IV) dioxide, plattnerite (beta-PbO2), and scrutinyte (alpha-PbO2), as degradation products of lead-based pigments. On these samples, no evidence of white lead was found, although a white lead conversion treatment had been applied on the paintings. The degradation of red lead (Pb3O4) into a mixture of plattnerite, scrutinyte, and anglesite (PbSO4) was demonstrated in some darkened samples. Furthermore, the degradation of haematite (Fe2O3) with the formation of magnetite (Fe3O4) and coquimbite (Fe-2(SO4)(3)center dot 9H(2)O) was also identified as responsible for the blackening of the paintings. The influence of original materials and environmental and anthropogenic factors such as the valley's orography and the presence of contaminating agents (SOx) is discussed to explain the decay phenomena.

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