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dc.rights.licenseopenen_US
hal.structure.identifierInstitut de Mécanique et d'Ingénierie [I2M]
dc.contributor.authorVERDET, Cécile
hal.structure.identifierInstitut de Mécanique et d'Ingénierie [I2M]
dc.contributor.authorSALMON, Fabien
IDREF: 228324467
hal.structure.identifierInstitut de Mécanique et d'Ingénierie [I2M]
dc.contributor.authorSIRIEIX, Colette
IDREF: 071604650
hal.structure.identifierInstitut de Mécanique et d'Ingénierie [I2M]
dc.contributor.authorLACANETTE, Delphine
dc.date.accessioned2021-10-28T07:33:19Z
dc.date.available2021-10-28T07:33:19Z
dc.date.issued2021-06-22
dc.identifier.issn0956-540Xen_US
dc.identifier.otherhttps://doi.org/10.5281/zenodo.3974137en_US
dc.identifier.urioai:crossref.org:10.1093/gji/ggab239
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/118766
dc.description.abstractEnSUMMARY Water migration within the rock mass during a fire has not yet been studied. Here, an innovative high-resolution micro-ERT method is developed at a centimetric scale to measure this phenomenon. The method is two-step based: first, a correction of the electrode effect, and second, the correction of resistivity for rapid variations in temperature with high values. Water migration is successfully described within the wall of an underground limestone quarry with three phases: from fire ignition to 36 min, the surface dries to a 3-cm depth and a higher saturated layer forms deeper than 0.10 m; from 36 min to 46 min (fire supply stops), the rock dries out and water migrates from deeper parts of the rock wall, deeper than 20 cm, towards the surface; finally, after fire extinction, the water migrates through a readjustment phase until it returns to its initial state.
dc.language.isoENen_US
dc.sourcecrossref
dc.subject.enElectrical resistivity tomography (ERT)
dc.subject.enHeat generation
dc.subject.enHeat flow
dc.subject.enRapid time variations
dc.title.enWater saturation variation in a fire-heated limestone gallery monitored by ERT
dc.typeArticle de revueen_US
dc.identifier.doi10.1093/gji/ggab239en_US
dc.subject.halSciences de l'ingénieur [physics]/Mécanique [physics.med-ph]en_US
dc.subject.halSciences de l'Homme et Société/Archéologie et Préhistoireen_US
bordeaux.journalGeophysical Journal Internationalen_US
bordeaux.page660-668en_US
bordeaux.volume227en_US
bordeaux.hal.laboratoriesInstitut de Mécanique et d’Ingénierie de Bordeaux (I2M) - UMR 5295en_US
bordeaux.issue1en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionBordeaux INPen_US
bordeaux.institutionCNRSen_US
bordeaux.institutionINRAEen_US
bordeaux.institutionArts et Métiersen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcedissemin
hal.identifierhal-03406795
hal.version1
hal.date.transferred2021-10-28T07:33:25Z
hal.exporttrue
workflow.import.sourcedissemin
dc.rights.ccPas de Licence CCen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Geophysical%20Journal%20International&rft.date=2021-06-22&rft.volume=227&rft.issue=1&rft.spage=660-668&rft.epage=660-668&rft.eissn=0956-540X&rft.issn=0956-540X&rft.au=VERDET,%20C%C3%A9cile&SALMON,%20Fabien&SIRIEIX,%20Colette&LACANETTE,%20Delphine&rft.genre=article


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