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dc.contributor.authorGarcía-Florentino, Cristina
dc.contributor.authorMaguregui Hernando, Maite
dc.contributor.authorMorillas Loroño, Héctor
dc.contributor.authorBalziskueta, Urko
dc.contributor.authorAzkarate Garai-Olaun, Agustín ORCID
dc.contributor.authorArana Momoitio, Gorka
dc.contributor.authorMadariaga Mota, Juan Manuel ORCID
dc.date.accessioned2019-01-07T15:58:50Z
dc.date.available2019-01-07T15:58:50Z
dc.date.issued2016-12
dc.identifier.citationJournal of Raman Spectroscopy 47(12) : 1458–1466 (2016)es_ES
dc.identifier.issn1097-4555
dc.identifier.urihttp://hdl.handle.net/10810/30652
dc.description.abstractPunta Begoña Galleries were built in 1918 in Getxo (Basque Country, North of Spain) but were abandoned in 1960. Nowadays, their conservation state is very poor. In this work, portable Raman spectroscopy was applied to evaluate the original composition and possible deterioration products of the mortars used in the inner walls and those covering the concrete of the ceilings allowing us to select the most appropriate sampling points. In the laboratory, Raman microscopy and Raman imaging, assisted with scanning electron microscopy equipped with an energy dispersive spectrometer (SEM‐EDS), X‐ray diffraction and energy dispersive X‐ray fluorescence (ED‐XRF) imaging, allowed to identify the key compounds to understand the deterioration processes taking place in the mortars of the galleries. The main components of the mortars from the walls were calcite and gypsum. In some cases, alite (Ca3SiO5) and belite (Ca2SiO4) were identified; these components are characteristic of Portland cement clinker. The main components of the mortar covering the concrete were calcite, quartz, aragonite and gypsum. The aragonite identification confirmed the use of beach sand as the aggregate in the mortar. The concrete from the ceiling of the lower gallery is covered with three different mortar layers; the outermost layer is covered with a black crust. In the three mortars, the main components are similar to those used in the mortar covering the concrete from the upper gallery. Thanks to Raman, ED‐XRF and SEM‐EDS imaging, it was possible to map the distribution of the main components through the three mortar layers and also to identify the presence of dolomite {[CaMg(CO3)2]}, which was not possible to detect following single‐point micro‐Raman analyses.es_ES
dc.description.sponsorshipThis work has been funded by the Ministry of Economy and Competitiveness and the European Regional Development Fund (ERDF) through the project DISILICA‐1930 (ref. BIA2014‐59124‐P) and by the cooperation agreement between the University of the Basque Country (UPV/EHU) and the City Council of Getxo (OTRI2014‐0639). C. García‐Florentino is grateful to the University of the Basque Country (UPV/EHU), which funded her predoctoral fellowship. Technical support provided by Raman‐LASPEA Laboratory and General X‐ray Service of the SGIKer (UPV/EHU, Ministry of Economy and Competitiveness of Spain, Basque Government, ERDF and European Social Fund) is also gratefully acknowledged.es_ES
dc.language.isoenges_ES
dc.publisherWileyes_ES
dc.relationinfo:eu-repo/grantAgreement/MINECO/BIA2014‐59124‐Pes_ES
dc.rightsinfo:eu-repo/semantics/openAccesses_ES
dc.subjectportable Ramanes_ES
dc.subjectRaman imaginges_ES
dc.subjectED-XRF imaginges_ES
dc.subjectmortarses_ES
dc.subjectsoluble saltses_ES
dc.titlePortable and Raman imaging usefulness to detect decaying on mortars from Punta Begoña Galleries (Getxo, North of Spain)es_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.holder(c)2016 Wileyes_ES
dc.relation.publisherversionhttps://onlinelibrary.wiley.com/doi/full/10.1002/jrs.4949es_ES
dc.identifier.doi10.1002/jrs.4949
dc.departamentoesGeografía, prehistoria y arqueologíaes_ES
dc.departamentoesQuímica analíticaes_ES
dc.departamentoeuGeografia,historiaurrea eta arkeologiaes_ES
dc.departamentoeuKimika analitikoaes_ES


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