Iron speciation in ancient Attic pottery pigments: a non-destructive SR-XAS investigation

被引:18
作者
Bardelli, Fabrizio [2 ]
Barone, Germana [3 ]
Crupi, Vincenza [1 ]
Longo, Francesca [1 ]
Maisano, Giacomo [1 ]
Majolino, Domenico [1 ]
Mazzoleni, Paolo [3 ]
Venuti, Valentina [1 ]
机构
[1] Univ Messina, Dept Phys, I-98166 Messina, Italy
[2] Maison Geosci, Inst Sci Terre ISTerre, F-38400 Grenoble, France
[3] Univ Catania, Geol Sci Dept, I-95129 Catania, Italy
关键词
XANES; EXAFS; XRF; ancient decorated pottery; non-destructive analysis; pigmentation; iron; RAY; XANES; EDGE; FE; MINERALS; XAFS; BLUE; XRF;
D O I
10.1107/S0909049512023990
中图分类号
TH7 [仪器、仪表];
学科分类号
0804 ; 080401 ; 081102 ;
摘要
The present work reports a detailed investigation on the speciation of iron in the pigments of decorated pottery fragments of cultural heritage relevance. The fragments come from the Gioiosa Guardia archaeological site in the area of the 'Strait of Messina' (Sicily, Southern Italy), and date back to VI-V century BC. The purpose of this study is to characterize the main pigmenting agents responsible for the dark-red coloration of the specimens using non-destructive analytical techniques such as synchrotron radiation X-ray absorption spectroscopy (SR-XAS), a well established technique for cultural heritage and environmental subjects. Absorption spectra were collected at the Fe K-edge on the Italian beamline for absorption and diffraction (BM8-GILDA) at the European Synchrotron Radiation Facility in Grenoble (France). In order to determine the speciation of Fe in the samples, principal component analysis and least-squares fitting procedures were applied to the near-edge part of the absorption spectra (XANES). Details on the local structure around the Fe sites were obtained by analyzing the extended part of the spectra (EXAFS). Furthermore, an accurate determination of the average Fe oxidation state was carried out through analysis of the pre-edge peaks of the absorption spectra. Samples resulted composed of an admixture of Fe2O3 (hematite or maghemite) and magnetite (Fe3O4), occurring in different relative abundance in the dark- and light-colored areas of the specimens. The results obtained are complementary to information previously obtained by means of instrumental neutron activation analysis, Fourier transform infrared absorbance and time-of-flight neutron diffraction.
引用
收藏
页码:782 / 788
页数:7
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