Raman imaging to quantify the thermal transformation degree of Pompeian yellow ochre caused by the 79 AD Mount Vesuvius eruption
Most of the wall paintings from Pompeii are decorated with red and yellow colors but the thermal impact of 79 AD MountVesuvius eruption promoted the partial transformation of some yellow-painted areas into red. The aim of this research is todevelop a quantitative Raman imaging methodology to relate...
| Autores: | , , , , |
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| Formato: | artículo |
| Fecha de publicación: | 2019 |
| País: | España |
| Recursos: | Universidad del País Vasco |
| Repositorio: | Addi. Archivo Digital para la Docencia y la Investigación |
| OAI Identifier: | oai:addi.ehu.eus:10810/36617 |
| Acesso em linha: | http://hdl.handle.net/10810/36617 |
| Access Level: | acceso abierto |
| Palavra-chave: | yellow ochre dehydratio Raman imaging color transformation quantitative analysis |
| Resumo: | Most of the wall paintings from Pompeii are decorated with red and yellow colors but the thermal impact of 79 AD MountVesuvius eruption promoted the partial transformation of some yellow-painted areas into red. The aim of this research is todevelop a quantitative Raman imaging methodology to relate the transformation percentage of yellow ochre (goethite,α-FeOOH) into red color (hematite,α-Fe2O3) depending on the temperature, in order to apply it and estimate the temperature atwhich the pyroclastic flow impacted the walls of Pompeii. To model the thermal impact that took place in the year 79 AD, ninewall painting fragments recovered in the archeological site of Pompeii and which include yellow ochre pigment were subjected tothermal ageing experiments (exposition to temperatures from 200 to 400 °C every 25 °C). Before the experiments, elementalinformation of the fragments was obtained by micro-energy dispersive X-ray fluorescence (μ-ED-XRF). The fragments werecharacterized before and after the exposition using Raman microscopy to monitor the transformation degree from yellow to red.The quantitative Raman imaging methodology was developed and validated using synthetic pellets of goethite and hematitestandards. The results showed almost no transformation (0.5% ± 0.4) at 200 °C. However, at 225 °C, some color transformation(26.9% ± 2.8) was observed. The most remarkable color change was detected at temperatures between 250 °C (transformation of46.7% ± 1.7) and 275 °C (transformation of 101.1% ± 1.2). At this last temperature, the transformation is totally completed sincefrom 275 to 400 °C the transformation percentage remained constant. |
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