Microanalysis of clay-based pigments in painted artworks by the means of Raman spectroscopy
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F13%3A10188977" target="_blank" >RIV/00216208:11310/13:10188977 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/61388980:_____/13:00421825 RIV/00216224:14310/13:00071643
Výsledek na webu
<a href="http://dx.doi.org/10.1002/jrs.4381" target="_blank" >http://dx.doi.org/10.1002/jrs.4381</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1002/jrs.4381" target="_blank" >10.1002/jrs.4381</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Microanalysis of clay-based pigments in painted artworks by the means of Raman spectroscopy
Popis výsledku v původním jazyce
FT Raman spectroscopy and micro-Raman spectroscopy with lasers of three different wavelengths (1064 nm, 785nm and 532 nm) were used for analysis of reference samples of natural clay pigments including white clay minerals (kaolinite, illite, montmorillonite), green earths (glauconite and celadonite) and red earths (natural mixtures of white clay minerals with hematite). In addition, eight micro-samples obtained from historical paintings containing clay pigments in ground and colour layers have been examined. Powder X-ray diffraction and micro-diffraction were used as supplementary methods. It was found that laser operating at 1064nm provided the best quality Raman spectra for distinguishing different white clay minerals, but the spectra of green and redearths were affected by strong fluorescence caused by the presence of iron. Green earth minerals could be easily distinguished by 532 or 785nm excitation lasers, even in small concentrations in the paint layers. On the other hand, when a
Název v anglickém jazyce
Microanalysis of clay-based pigments in painted artworks by the means of Raman spectroscopy
Popis výsledku anglicky
FT Raman spectroscopy and micro-Raman spectroscopy with lasers of three different wavelengths (1064 nm, 785nm and 532 nm) were used for analysis of reference samples of natural clay pigments including white clay minerals (kaolinite, illite, montmorillonite), green earths (glauconite and celadonite) and red earths (natural mixtures of white clay minerals with hematite). In addition, eight micro-samples obtained from historical paintings containing clay pigments in ground and colour layers have been examined. Powder X-ray diffraction and micro-diffraction were used as supplementary methods. It was found that laser operating at 1064nm provided the best quality Raman spectra for distinguishing different white clay minerals, but the spectra of green and redearths were affected by strong fluorescence caused by the presence of iron. Green earth minerals could be easily distinguished by 532 or 785nm excitation lasers, even in small concentrations in the paint layers. On the other hand, when a
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
CB - Analytická chemie, separace
OECD FORD obor
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Návaznosti výsledku
Projekt
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Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2013
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Journal of Raman Spectroscopy
ISSN
0377-0486
e-ISSN
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Svazek periodika
44
Číslo periodika v rámci svazku
11
Stát vydavatele periodika
US - Spojené státy americké
Počet stran výsledku
8
Strana od-do
1570-1577
Kód UT WoS článku
000330107900015
EID výsledku v databázi Scopus
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