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ANALÝZA ARCHEOLOGICKÉ KERAMIKY METODAMI SKENOVACÍ ELEKTRONOVÉ MIKROSKOPIE A RAMANOVY SPEKTROSKOPIE

dc.contributor.authorJezbera, Daniel
dc.contributor.authorLoskot, Jan
dc.contributor.authorMiškář, Dominik
dc.contributor.authorPleska, Miroslav
dc.contributor.authorThér, Richard
dc.date.accessioned2025-12-05T10:01:24Z
dc.date.available2025-12-05T10:01:24Z
dc.date.issued2021
dc.description.abstractThe combination of Raman spectroscopy (RS) and scanning electron microscopy (SEM) shows a good potential for nondestructive analysis of painted archaeological ceramics. SEM images reveal the topography and microstructure of both the ceramic clay and the engobes, and associated microanalyses based on energy-dispersive X-ray spectroscopy (EDS) allow to determine elemental composition of selected surface areas. The elemental composition coupled with obtained Raman spectra can provide meaningful suggestions of chemical substances contained in the sample. This was verified by analyzing a ceramic shard from the La Tène oppidum Třísov in South Bohemia. It was found that its red-brown engobe consists predominantly of hematite and contains also anatase and burnt organic residues. The presence of hematite is consistent with the fact that hematite dyes are typical of painted ceramics from this period and region.cze
dc.description.abstract-translatedThe combination of Raman spectroscopy (RS) and scanning electron microscopy (SEM) shows a good potential for nondestructive analysis of painted archaeological ceramics. SEM images reveal the topography and microstructure of both the ceramic clay and the engobes, and associated microanalyses based on energy-dispersive X-ray spectroscopy (EDS) allow to determine elemental composition of selected surface areas. The elemental composition coupled with obtained Raman spectra can provide meaningful suggestions of chemical substances contained in the sample. This was verified by analyzing a ceramic shard from the La Tène oppidum Třísov in South Bohemia. It was found that its red-brown engobe consists predominantly of hematite and contains also anatase and burnt organic residues. The presence of hematite is consistent with the fact that hematite dyes are typical of painted ceramics from this period and region.eng
dc.formatp. 320-324
dc.identifier.issn0009-2770
dc.identifier.obd43877771
dc.identifier.urihttp://hdl.handle.net/20.500.12603/1265
dc.identifier.wos000661745400007
dc.language.isocze
dc.peerreviewedyes
dc.publicationstatuspostprint
dc.publisherČeská společnost chemická
dc.relation.ispartofChemické listy, volume 115, issue: 6cze
dc.relation.publisherversionhttp://www.chemicke-listy.cz/ojs3/index.php/chemicke-listy/article/view/3861
dc.rights.accessOpen Access
dc.rights.licenseCC BY
dc.source.urlhttp://www.chemicke-listy.cz/ojs3/index.php/chemicke-listy/article/view/3861
dc.subjectarcheologická keramikacze
dc.subjectskenovací elektro-nová mikroskopiecze
dc.subjectenergiově disperzní spektroskopiecze
dc.subjectRamanova spektroskopiecze
dc.subjectbarviva a pigmentycze
dc.subjectengobacze
dc.subjectarchaeological ceramicseng
dc.subjectscanning electron microscopyeng
dc.subjectenergy-dispersive spectroscopyeng
dc.subjectRaman spectroscopyeng
dc.subjectdyes and pigmentseng
dc.subjectengobeeng
dc.titleANALÝZA ARCHEOLOGICKÉ KERAMIKY METODAMI SKENOVACÍ ELEKTRONOVÉ MIKROSKOPIE A RAMANOVY SPEKTROSKOPIEcze
dc.title.alternativeAnalysis of Archaeological Ceramics by the Methods of Scanning Electron Microscopy and Raman Spectroscopyeng
dc.typearticle

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