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dc.contributor.authorShekofteh, Atefeh
dc.contributor.authorMolina, Eduardo
dc.contributor.authorArizzi, Anna 
dc.contributor.authorCultrone , Giuseppe V. 
dc.contributor.authorAhmadi, Hossein
dc.contributor.authorYazdi, Mehdi
dc.date.accessioned2025-05-30T10:10:39Z
dc.date.available2025-05-30T10:10:39Z
dc.date.issued2019
dc.identifier.citationShekofteh, A., Molina, E., Arizzi, A., Cultrone, G., Ahmadi, H., & Yazdi, M. (2018). Characterization and damage assessment of stones used in the Pasargadae World Heritage Site, Achaemenian period. International Journal of Architectural Heritage, 13(4), 521–536. https://doi.org/10.1080/15583058.2018.1436728es_ES
dc.identifier.urihttps://hdl.handle.net/10481/104362
dc.descriptionThis work was supported by the Research Group RNM179 of the Junta de Andalucía [RNM179];Research Project MAT2016-75889-R [MAT2016-75889-R];Ministry of science, research and technology of Iran [215520]. We would like to thank the Razi Applied Science Foundation (Tehran, Iran) and the Centro de Instrumentación Científica (CIC; University of Granada, Spain) for assistance with SEM-EDX analyses.es_ES
dc.description.abstractThe architectural remains at Pasargadae were built of three different stones classified according to their colors (beige, dark-gray, and green-gray). The stones show different macroscopic features, such as texture and decay patterns. The aim of this study is to identify the composition of the stones and to evaluate the main decay factors through petrographic studies in order to make conservation decisions more compatible. Petrochemical analyses show that the stones are in fact limestones with different features; two of them have a compact texture (beige and dark-gray stones), while the third has a fairly porous structure (green-gray stone). In some beige stone samples, dolomite was identified. Despite the fact that the presence of salt is a possible decay factor, X-ray diffraction analysis did not report any salt. According to SEM observations, the main reasons for decay in dark-gray and green-gray stones are the dissolution of calcite crystals and the swelling of clay minerals. The main decay factor in the beige stone, by contrast, is dissolution induced by microorganism activity. However, a patina formed by lichens on the surface of the beige stone, although aesthetically detrimental, protects it against further decay.es_ES
dc.description.sponsorshipJunta de Andalucía [RNM179]es_ES
dc.description.sponsorshipResearch Project MAT2016-75889-Res_ES
dc.description.sponsorshipMinistry of science, research and technology of Iran [215520]es_ES
dc.language.isoenges_ES
dc.publisherTaylor & Francises_ES
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 Internacional*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.subjectBiodeteriorationes_ES
dc.subjectClay swellinges_ES
dc.subjectDeteriorationes_ES
dc.subjectDissolutiones_ES
dc.subjectLimestone es_ES
dc.subjectPasargadae World Heritage Sitees_ES
dc.titleCharacterization and damage assessment of stones used in the Pasargadae World Heritage Site, Achaemenian periodes_ES
dc.typejournal articlees_ES
dc.rights.accessRightsopen accesses_ES
dc.identifier.doi10.1080/15583058.2018.1436728
dc.type.hasVersionVoRes_ES


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