Characterization of pottery from Republic of Macedonia. III. A study of comparative mineralogical detection efficiency using micro‐Raman mapping and X‐ray diffraction

Abstract

Point‐to‐point micro‐Raman and X‐ray diffraction (XRD) techniques were employed for characterization of minerals present in the pottery body of 27 glazed Byzantine and Ottoman pottery shreds, excavated at two different archaeological sites in the Republic of Macedonia: in Skopje (Skopsko Kale) and in Prilep (Markovi Kuli and Sv. Atanas Church). The Raman spectra of 18 Byzantine samples (dating from 12th−14th century) and nine Ottoman samples (dating from 17th−19th century) revealed 26 different minerals. XRD measurements were further performed on the same powder samples to validate the mineralogical assessment obtained by point‐to‐point micro‐Raman spectroscopy. Although only 13 different mineral phases were obtained by the XRD, the results obtained from the Raman and XRD spectra for the most abundant minerals in the investigated pottery bodies match quite well. However, the identification of the less abundant minerals in the clay matrixes from the XRD data was very difficult, if at all possible. The results emphasize the specifics of the applied techniques and their limits. Additionally, wavelength dispersive X‐ray fluorescence spectroscopy was used for the elemental analysis. Copyright © 2011 John Wiley & Sons, Ltd.

Comparative analysis of wucai Chinese porcelains using mobile and fixed Raman microspectrometers

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Recent advances in linear and nonlinear Raman spectroscopy. Part VII

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“…Despite the complexity of the feldspar family, where the members are distinguished not only by the composition but also by the order degree, different important Raman spectroscopy studies on feldspars are present in the literature . Many investigators used Raman spectroscopy to characterize feldspar in ceramics because the correct identification of the right term could allow one to recognize the provenance of the raw materials or to better understand the firing conditions of the pottery. An important point to consider is that the correct phase identification (and, in turn, the possible geological origin) depends not only from the composition, but also from the structural order.…”