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dc.contributor.authorFranquello Zoffman, María Luisa
dc.contributor.authorRobador González, María Dolores
dc.contributor.authorRamírez del Valle, Verónica
dc.contributor.authorDurán Benito, Adrián
dc.contributor.authorJiménez de Haro, María Carmen
dc.date.accessioned2026-07-01T08:01:09Z
dc.date.available2026-07-01T08:01:09Z
dc.date.issued2008
dc.identifier.citationFranquello Zoffman, M. L., Robador González, M. D., Ramírez del Valle, V., Durán Benito, A., y Jiménez de Haro, M. C. (2008). Roman Ceramics of HydRaúlic Mortars Used to Build the Mithraeum House of Merida (Spain). Journal of Thermal Analysis and Calorimetry, 92(1), 331-335.es
dc.identifier.issn1388-6150
dc.identifier.urihttp://hdl.handle.net/20.500.12251/5588
dc.description.abstractRoman ceramics of two hydRaúlic mortars used to build the pond and water channel of Mithraeum house from Merida (Spain) have been studied. The sizes of the ceramic fragments found were different in both of the samples studied, showing different behaviour in the reactions with the lime. The X-ray diffraction of the ceramic shows the presence of quartz, mica (biotite), anorthite and hematite accompanied by amorphous phase, being observed scarce vitrification. The presence of mica confirms a firing temperature for manufacturing the ceramic below 900 degrees C. In one of the ceramics studied, X-ray diffraction did not show calcite. However, in the FTIR appear bands that could be assigned to carbonates absorptions and likewise, carbonates were identified in the DTA-TG curves. Ca and small quantities of Si and Al were also identified by SEM-EDX on the surface of the pores that could be due to an amorphous phase formed in the reaction of lime with the Si and Al of the ceramic. On the other hand, in other ceramic samples carbonates (about 10%) were detected. The carbonates have been found filling the pores, sometimes accompanied by a new calcium-aluminium-silicate phase produced by the reaction between the lime and the amorphous phase of the ceramic. The carbonates and the new phases formed inside the pores are responsible for the decrease of the porosity and for the formation of new phases during the heating of the ceramics.es
dc.language.isoenges
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 Internacional*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.titleRoman Ceramics of HydRaúlic Mortars Used to Build the Mithraeum House of Merida (Spain)es
dc.typearticle
dc.issue.number1es
dc.journal.titleJournal of Thermal Analysis and Calorimetryes
dc.page.initial331es
dc.page.final335es
dc.rights.accessRightsopenAccesses
dc.subject.keywordHormigónes
dc.subject.keywordMorteroses
dc.subject.keywordPropiedades mecánicases
dc.subject.unesco1203.17 Informáticaes
dc.subject.unesco3305.90 Transmisión de Calor en la Edificaciónes
dc.subject.unesco3312 Tecnología de Materialeses
dc.subject.unesco2201 Acústicaes
dc.subject.unesco2201.02 Acústica Arquitectónicaes
dc.subject.unesco3328.16 Transferencia de Calores
dc.subject.unesco3312.08 Propiedades de Los Materialeses
dc.subject.unesco3312.09 Resistencia de Materialeses
dc.subject.unesco3312.03 Materiales Cerámicoses
dc.subject.unesco6201 Arquitecturaes
dc.subject.unesco5506.01 Historia de la Arquitecturaes
dc.subject.unesco5311 Organización y Dirección de Empresases
dc.subject.unesco5312 Economía Sectoriales
dc.volume.number92


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