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Thermal stress-induced microcracking in building granite

dc.contributor.authorFreire-Lista, D. M.
dc.contributor.authorFort González, Rafael
dc.contributor.authorVaras Muriel, María Josefa
dc.date.accessioned2023-06-18T05:57:51Z
dc.date.available2023-06-18T05:57:51Z
dc.date.issued2016-05
dc.description.abstractMicrocracking induced by wide fluctuations in temperature affects granite quality and durability, making the stone more vulnerable to decay. Determining the extent of that effect is not always straightforward, however, given the excellent durability of these materials.Four types of construction granite quarried in the region of Madrid, Spain, and frequently used in both the built heritage and in de novo construction (Alpedrete, Cadalso de los Vidrios, Colmenar Viejo and Zarzalejo) were exposed to 42 thermal cycles (105-20 °C; UNE-EN, 14066, 2003). Petrographic and petrophysical properties were analysed using both destructive and non-destructive techniques. Microcracking generated in the granite stones by 42 thermal cycles had barely any impact on their petrophysical properties, which are the parameters normally assessed to establish material quality and durability. Their petrographic properties, which are not generally assessed in this type of studies, were affected, however. This study contends that petrographic analysis is needed to objectively quantify the actual quality and durability of the most highly resistant materials when petrophysical studies are inconclusive. Petrographic and fluorescence microscopy, along with fractography, are among the most prominent techniques for petrographic exploration. Thanks to the deployment of these techniques, mineral microcracking could be monitored throughout the present tests conducted.The microscopic findings revealed substantial micro-textural and microstructural change in and around the granite minerals, which play a prominent role in decay. The findings showed that pre-existing microcracks coalesced and generated further microcracking as decay progressed. Microcracking was most intense in Zarzalejo granite due to its textural characteristics determined by its high feldspar content. Microscopic observation revealed that the microstructure of feldspar minerals, with their crystallographic anisotropies and secondary mineral phases, favoured microcrack development. Zarzalejo granite exhibited lower quality and durability than Colmenar Viejo and Cadalso de los Vidrios granites, which were more resistant to heat treatment.
dc.description.departmentDepto. de Mineralogía y Petrología
dc.description.facultyFac. de Ciencias Geológicas
dc.description.refereedTRUE
dc.description.sponsorshipComunidad de Madrid
dc.description.sponsorshipUniversidad Complutense de Madrid
dc.description.statuspub
dc.eprint.idhttps://eprints.ucm.es/id/eprint/57414
dc.identifier.doi10.1016/j.enggeo.2016.03.005
dc.identifier.issn0013-7952
dc.identifier.officialurlhttps://www.sciencedirect.com/journal/engineering-geology/vol/206/suppl/C
dc.identifier.relatedurlhttp:// www.elsevier.com/locate/enggeo
dc.identifier.urihttps://hdl.handle.net/20.500.14352/23666
dc.journal.titleEngineering geology
dc.language.isoeng
dc.page.final99
dc.page.initial83
dc.publisherElsevier
dc.relation.projectIDGEOMATERIALS-2CM (S2013/MIT-2914)
dc.relation.projectIDUCM (921349)
dc.rights.accessRightsrestricted access
dc.subject.cdu552.1
dc.subject.keywordGranite
dc.subject.keywordMicrocracks
dc.subject.keywordPetrography
dc.subject.keywordPetrophysics
dc.subject.keywordDecay
dc.subject.ucmPetrología
dc.titleThermal stress-induced microcracking in building granite
dc.typejournal article
dc.volume.number206
dspace.entity.typePublication
relation.isAuthorOfPublication00ca5323-0651-4b63-a8cf-fe26b08f39b8
relation.isAuthorOfPublication.latestForDiscovery00ca5323-0651-4b63-a8cf-fe26b08f39b8

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