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Artificial weathering of Spanish granites subjected to salt crystallization tests: Surface roughness quantification

dc.contributor.authorLópez-Arce Martínez, Paula
dc.contributor.authorVaras Muriel, María Josefa
dc.contributor.authorFernández Revuelta, B.
dc.contributor.authorÁlvarez de Buergo, Mónica
dc.contributor.authorFort González, Rafael
dc.contributor.authorPérez-Soba Aguilar, Cecilia María
dc.date.accessioned2023-06-20T00:19:54Z
dc.date.available2023-06-20T00:19:54Z
dc.date.issued2010
dc.description.abstractFor hundreds of years, two types of granite (Zarzalejo and Alpedrete) from the Madrid region, Spain, have been extensively used as building stones. Fresh specimens of both stone types have been sampled from their respective quarries and subjected to sodium sulphate salt crystallization test (SCT). The resulting physical and chemical weathering patterns have been characterized by polarized light optical and environmental scanning electron microscopy. Water absorption under vacuum conditions and mercury intrusion porosimetry techniques were used to determine the pre- and post-SCT porosity and pore size distribution. The following non-destructive techniques were performed to assess stone durability and decay: ultrasound velocity (US) and surface roughness determination (SR) of intra- and inter-granular quartz, feldspar and biotite minerals at the centre as well as at the corners and edges of specimen surfaces. Before the SCT, US values were lower and SR values higher in Zarzalejo (ZAR) than Alpedrete (ALP) granite. After SCT, the US values declined while SR rose in both types of granites, with greater average differences in ZAR than ALP for both parameters. Feldspar and biotite and their inter-granular contacts were found to be the weakest and therefore the most decay-prone areas of the stone. The initial SR parameters were generally higher and rose more steeply after SCT at the corners and around the edges of the specimens. While behaviour was found to be similar in the two types of granite, variations were greater in ZAR, the less durable and more decay-prone of the two. Surface roughness measurement of mineral grains in granite stones is a very useful, in situ, non-destructive technique for quantifying salt crystallization-mediated physical and chemical weathering. The resulting quantification of decay and of related durability provides insight into the future behaviour of this type of stone, commonly used in historic buildings.
dc.description.departmentDepto. de Mineralogía y Petrología
dc.description.facultyFac. de Ciencias Geológicas
dc.description.refereedTRUE
dc.description.statuspub
dc.eprint.idhttps://eprints.ucm.es/id/eprint/17192
dc.identifier.doi10.1016/j.catena.2010.08.009
dc.identifier.issn0341-8162
dc.identifier.officialurlhttp://www.journals.elsevier.com/catena/
dc.identifier.urihttps://hdl.handle.net/20.500.14352/42407
dc.journal.titleCatena
dc.language.isoeng
dc.page.final185
dc.page.initial170
dc.publisherElsevier B.V.
dc.rights.accessRightsopen access
dc.subject.cdu552.3
dc.subject.keywordGranite
dc.subject.keywordSalt crystallization tests
dc.subject.keywordWeathering
dc.subject.keywordSurface roughness indexes
dc.subject.keywordDurability
dc.subject.keywordNatural stone
dc.subject.ucmPetrología
dc.titleArtificial weathering of Spanish granites subjected to salt crystallization tests: Surface roughness quantification
dc.typejournal article
dc.volume.number83
dspace.entity.typePublication
relation.isAuthorOfPublication00ca5323-0651-4b63-a8cf-fe26b08f39b8
relation.isAuthorOfPublication064006d7-ea47-428e-91e0-02ed1a12ae83
relation.isAuthorOfPublication.latestForDiscovery064006d7-ea47-428e-91e0-02ed1a12ae83

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