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Differentiation between anonymous paintings of the 17th and the early 18th century by composition of clay-based grounds
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SYSNO ASEP 0447648 Druh ASEP J - Článek v odborném periodiku Zařazení RIV J - Článek v odborném periodiku Poddruh J Článek ve WOS Název Differentiation between anonymous paintings of the 17th and the early 18th century by composition of clay-based grounds Tvůrce(i) Hradil, David (UACH-T) RID, SAI
Hradilová, J. (CZ)
Bezdička, Petr (UACH-T) SAI, RID, ORCID
Švarcová, Silvie (UACH-T) SAI, RID, ORCIDZdroj.dok. Applied Clay Science. - : Elsevier - ISSN 0169-1317
Roč. 118, DEC (2015), s. 8-20Poč.str. 13 s. Jazyk dok. eng - angličtina Země vyd. NL - Nizozemsko Klíč. slova paintings ; clay-based grounds ; X-ray powder micro-diffraction ; historical technology Vědní obor RIV CA - Anorganická chemie CEP GA14-22984S GA ČR - Grantová agentura ČR Institucionální podpora UACH-T - RVO:61388980 UT WOS 000365056400002 EID SCOPUS 84941241834 DOI 10.1016/j.clay.2015.08.038 Anotace Numerous anonymous paintings are preserved in depositories of European galleries. The reasons why they are not being shown to the public differ, but one of them is their doubtful attribution and relative dating. There is a large amount of unsigned paintings of varying artistic quality and also lots of copies of unknown provenance. We have found out that mineralogical analysis based on X-ray powder micro-diffraction measurements is able to provide exact parameters for the classification of earthy ground layers of paintings into well-defined types. In the period of the 17th and the early 18th century, these types were regionally specific, because various coloured clay-based materials became popular thanks to significant changes in the painting technology. They gradually substituted previously used white chalk and/or gypsum (gesso). Within comparative research performed on paintings from Czech collections, we were able to distinguish those of Italian and those of Central-European provenance. We have defined five types of grounds that differ in clay minerals' structures (presence of expandable and interstratified structures, various crystallinity indices etc.) and their relative contents, and, in addition, in characteristic elemental ratios and admixtures, either natural or artificial. Pracoviště Ústav anorganické chemie Kontakt Jana Kroneislová, krone@iic.cas.cz, Tel.: 311 236 931 Rok sběru 2016
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