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dc.rights.licenseopenen_US
hal.structure.identifierInstitut de Mécanique et d'Ingénierie [I2M]
dc.contributor.authorALLEGRE, Vincent
IDREF: 15549998X
hal.structure.identifierArchéologie, Terre, Histoire, Sociétés [Dijon] [ARTeHiS]
hal.structure.identifierGénie des procédés frigorifiques pour la sécurité alimentaire et l'environnement [UR FRISE]
dc.contributor.authorDENIS, Alain
IDREF: 095129243
hal.structure.identifierUniversité de Bordeaux [UB]
dc.contributor.authorCOINTE, Alain
IDREF: 078155282
hal.structure.identifierUniversité de Bordeaux [UB]
hal.structure.identifierInstitut de Mécanique et d'Ingénierie [I2M]
dc.contributor.authorCOUREAU, Jean-Luc
IDREF: 063468832
dc.date.accessioned2022-03-30T14:02:33Z
dc.date.available2022-03-30T14:02:33Z
dc.date.issued2021
dc.date.conference2021-08
dc.identifier.urioai:crossref.org:10.3997/2214-4609.202120104
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/136567
dc.description.abstractEnThe mechanical response of a few maritime pines was investigated by a series of experiments at the field scale. During the overturning of two trees, a seismic array was deployed at the ground surface to continuously monitor the micro-seismicity associated with the failure of their root-system. We identified seismic events during the traction process applied to each tree. A threshold force value and a significant duration of the traction process seem to be needed in order for cracks to happen, and for seismic events to be recorded. We identified tens of seismic events, especially during the most advanced stages of the experiments, prior to complete failure of the root-system. However, a few events were observed during early stage of the experiment, when the mechanical solicitation was still in the elastic regime. Using pairs of geophones and seismic intensity ratios, we localized the epicenters of most of the events within the seismic network. According to the sensitivity of the array, all epicenters are roughly localized within a 1 square-meter area. The estimation of epicenters show that the events are aligned to the direction of traction, on the opposite side of the tree.
dc.language.isoENen_US
dc.publisherEuropean Association of Geoscientists & Engineersen_US
dc.sourcecrossref
dc.subject.enForestry
dc.subject.enSeismology
dc.subject.enEpicentre
dc.subject.enField experiment
dc.subject.enField scale
dc.subject.enLocalised
dc.subject.enMaritime pines
dc.subject.enMechanical response
dc.subject.enRoot system
dc.subject.enSeismic event
dc.subject.enSeismic monitoring
dc.subject.enSystem failures
dc.title.enSeismic Monitoring of a Maritime Pine Root-System Failure During Its Overturn: A Field Experiment
dc.typeCommunication dans un congrès avec actesen_US
dc.identifier.doi10.3997/2214-4609.202120104en_US
dc.subject.halSciences de l'ingénieur [physics]/Mécanique [physics.med-ph]en_US
bordeaux.page1-5en_US
bordeaux.volume2021en_US
bordeaux.hal.laboratoriesInstitut de Mécanique et d’Ingénierie de Bordeaux (I2M) - UMR 5295en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionBordeaux INPen_US
bordeaux.institutionCNRSen_US
bordeaux.institutionINRAEen_US
bordeaux.institutionArts et Métiersen_US
bordeaux.conference.titleNear Surface Geoscience Conference and Exhibitionen_US
bordeaux.countryfren_US
bordeaux.title.proceeding27th European Meeting of Environmental and Engineering Geophysicsen_US
bordeaux.conference.cityVirtualen_US
bordeaux.peerReviewedouien_US
bordeaux.import.sourcedissemin
hal.identifierhal-03625033
hal.version1
hal.date.transferred2022-03-30T14:02:35Z
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.date=2021&rft.volume=2021&rft.spage=1-5&rft.epage=1-5&rft.au=ALLEGRE,%20Vincent&DENIS,%20Alain&COINTE,%20Alain&COUREAU,%20Jean-Luc&rft.genre=proceeding


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