A non-destructive approach for the characterization of glass artifacts: The case of glass beads from the Iron Age Picene necropolises of Novilara and Crocefisso-Matelica (Italy)

被引:4
|
作者
de Ferri, Lavinia [1 ,5 ]
Mezzadri, Francesco [2 ]
Falcone, Roberto [3 ]
Quagliani, Valeria [1 ]
Milazzo, Fabio [4 ]
Pojana, Giulio [1 ]
机构
[1] Univ Ca Foscari Venice, Dept Philosophy & Cultural Heritage, Dorsoduro 3484-D, I-30123 Venice, Italy
[2] Univ Parma, Dept Chem Life & Environm Sustainabil Sci, Parco Area Sci 11-A, I-43124 Parma, Italy
[3] Stn Sperimentale Vetro, VG Briati 10, I-30141 Venice, Italy
[4] Belle Arti & Paesaggio SABAP Marche, Lab Restauro Archeol Soprintendenza Archeol, Piazza Senato 15, I-60100 Ancona, Italy
[5] Norwegian Univ Sci & Technol, Dept Mech & Ind Engn, Richard Birkelands Vei 2B, Trondheim, Norway
关键词
Glass beads; Iron Age; Reflectance Spectroscopy; X-Ray Diffraction; X-Ray Fluorescence; ROMAN GLASS; CHEMICAL-ANALYSES; ANCIENT GLASS; RAW-MATERIALS; PIGMENTS; OPACIFIERS; CERAMICS; XRF; IDENTIFICATION; TECHNOLOGIES;
D O I
10.1016/j.jasrep.2019.102124
中图分类号
K85 [文物考古];
学科分类号
0601 ;
摘要
A totally non-destructive approach was employed to characterize beads from two Picene necropolises (NovilaraPU and Crocefisso-Matelica-MC) dating back to between 9th and 6th centuries B.C. Investigations were carried out principally by means of Reflectance Spectroscopy determining Co2+, Cu2+ and Fe3+ as the main chromophores, and by Raman Spectroscopy to distinguish samples realized with other materials, in particular bones and shells were recognized. Furthermore, Raman spectroscopy identified hematite as a coloring phase in the unique red bead discovered as unmelt crystals in blue and yellow beads. Additionally, X-Ray Diffractometry investigations indicated Ca-phosphates, bindhemite and the less common brizzite, as opacifiers in white and yellow beads, while chemical data collected through X-Ray Fluorescence evidenced differences between findings from the two localities and/or within the same site. Beads were found to belong to the Low Magnesium Glass (LMG) and High Magnesium Low Potassium (HMLK) classes with most blue beads being comprised of cobaltiferous alum salts and a relatively impure sand, and a calcareous sand having been used for all other analyzed beads. Finally, differentiations performed on the basis of MgO amounts tended to indicate the samples from Crocefisso as being more similar to Bronze Age compositions than the Novilara ones which are closer to typical Iron Age proportions. In addition, high amounts of lead have been detected in all the yellow beads, but they could be positively correlated to Sb2O3 only for samples recovered in the Novilara necropolis, thus indicating the use of lead antimonates as coloring agents.
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页数:16
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