Mostrar el registro sencillo del ítem

dc.contributor.authorGerminario, Chiara
dc.contributor.authorCultrone, Giuseppe V. 
dc.contributor.authorDe Bonis, Alberto
dc.contributor.authorIzzo, Francesco
dc.contributor.authorLangella, Alessio
dc.contributor.authorMercurio, Mariano
dc.contributor.authorNodari, Luca
dc.contributor.authorR. Vyhnal, Christopher
dc.contributor.authorGrifa, Celestino
dc.date.accessioned2024-07-02T09:34:55Z
dc.date.available2024-07-02T09:34:55Z
dc.date.issued2024-04-06
dc.identifier.citationC. Germinario et al. Applied Clay Science 253 (2024) 107347. [https://doi.org/10.1016/j.clay.2024.107347]es_ES
dc.identifier.urihttps://hdl.handle.net/10481/92919
dc.description.abstractIn recent decades, μ-Raman spectroscopy has become a powerful technique for studying ceramics, with the advantage of performing fast, reproducible and reliable analyses that provide effective information on ceramic technology. In the present paper, the potential of μ-Raman spectroscopy was evaluated by comparing the results of spectroscopic analyses with a wide range of conventional compositional and mineralogical analyses. Particular fragments of pottery from the archaeological site of Pollena Trocchia (Campania, Italy), characterized by a variegated color zonation, a symptom of uncontrolled firing conditions, were subjected to in-depth analytical investigation. Data from the μ-Raman measurements were in very good agreement with the analytical set of conventional analyses and permitted to better constrain the firing temperatures, evaluate changes in the oxidative steps, and assert the provenance of volcanic raw materials. The results illuminated that pottery was crafted by mixing a low-CaO base clay with volcanic temper from the environs of Vesuvius and fired in a not well-controlled firing atmosphere, which determined the development of Fe(III) oxides at rims of sherds and Fe (II)-bearing phases at cores. Moreover, even in the absence of newly-formed minerals, firing temperatures were estimated between 900 and 950 ◦C, as suggested by the mineralogical and spectroscopic evidence of the prograde 10 Å dehydroxylated phyllosilicates.es_ES
dc.description.sponsorshipDepartment of Science and Technology of the University of Sannio (FRA Grifa)es_ES
dc.description.sponsorshipResearch group RNM179 of the Junta de Andaluciaes_ES
dc.description.sponsorshipProject B-RNM-188-UGR20 of the Regional Ministry of Universityes_ES
dc.language.isoenges_ES
dc.publisherElsevieres_ES
dc.rightsAtribución 4.0 Internacional*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/*
dc.subjectμ-Raman spectroscopyes_ES
dc.subjectArchaeological potteryes_ES
dc.subjectCeramic materials es_ES
dc.titleμ-Raman spectroscopy as a useful tool for improving knowledge of ancient ceramic manufacturing technologieses_ES
dc.typejournal articlees_ES
dc.rights.accessRightsopen accesses_ES
dc.identifier.doi10.1016/j.clay.2024.107347
dc.type.hasVersionVoRes_ES


Ficheros en el ítem

[PDF]

Este ítem aparece en la(s) siguiente(s) colección(ones)

Mostrar el registro sencillo del ítem

Atribución 4.0 Internacional
Excepto si se señala otra cosa, la licencia del ítem se describe como Atribución 4.0 Internacional