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hal.structure.identifierLaboratoire de Géophysique Interne et Tectonophysique [LGIT]
dc.contributor.authorRENARD, François
hal.structure.identifierInstitut de Chimie de la Matière Condensée de Bordeaux [ICMCB]
dc.contributor.authorBERNARD, Dominique
hal.structure.identifierEuropean Synchrotron Radiation Facility [ESRF]
dc.contributor.authorTHIBAULT, Xavier
hal.structure.identifierEuropean Synchrotron Radiation Facility [ESRF]
dc.contributor.authorBOLLER, Elodie
dc.date.issued2004
dc.identifier.issn0094-8276
dc.description.abstractEnPressure solution creep is one of the possible processes of mechano-chemical deformation that controls porosity and permeability variations in the upper crust. The three-dimensional geometry of the porous network of halite aggregates was imaged during compaction driven by pressure solution creep using X-ray synchrotron computed microtomography. This technique can be used to monitor individual grain contacts and whole aggregate textural changes during deformation. By reconstructing subvolumes, the 3D porosity of the aggregates was extracted. The time-resolved decrease in permeability during porosity reduction was calculated by solving the Stokes equations. The permeability remained isotropic and decreased from 2.1 to 0.15 Darcy after 18.2% compaction. Two microscopic mechanisms can explain the permeability reduction: grain indentation and pore connectivity reduction by precipitation on the free surface of pore throats.
dc.language.isoen
dc.publisherAmerican Geophysical Union
dc.title.enSynchrotron 3D microtomography of halite aggregates during experimental pressure solution creep and evolution of the permeability.
dc.typeArticle de revue
dc.identifier.doi10.1029/2004GL019605
dc.subject.halPlanète et Univers [physics]/Sciences de la Terre/Géophysique [physics.geo-ph]
dc.subject.halPhysique [physics]/Physique [physics]/Géophysique [physics.geo-ph]
dc.subject.halChimie/Matériaux
bordeaux.journalGeophysical Research Letters
bordeaux.pageL07607
bordeaux.volume31
bordeaux.peerReviewedoui
hal.identifierhal-00105232
hal.version1
hal.popularnon
hal.audienceNon spécifiée
hal.origin.linkhttps://hal.archives-ouvertes.fr//hal-00105232v1
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