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dc.rights.licenseopenen_US
hal.structure.identifierGéoHydrosystèmes COntinentaux [GéHCO EA6293]
dc.contributor.authorDHIVERT, Elie
hal.structure.identifierGéoHydrosystèmes COntinentaux [GéHCO EA6293]
dc.contributor.authorGROSBOIS, Cécile
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorCOYNEL, Alexandra
hal.structure.identifierLaboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette] [LSCE]
hal.structure.identifierGéochimie Des Impacts [GEDI]
dc.contributor.authorLEFÈVRE, I.
hal.structure.identifierGéoHydrosystèmes COntinentaux [GéHCO EA6293]
dc.contributor.authorDESMET, Marc
dc.date.accessioned2024-05-15T08:08:19Z
dc.date.available2024-05-15T08:08:19Z
dc.date.issued2015-03
dc.identifier.issn0341-8162en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/199848
dc.description.abstractEnThe Villerest flood-control reservoir was built in the Upper Loire River (France) during the early 1980s, downstream from the most important industrial and coal-mining area of the basin. This reservoir has constituted an important trap for sediments and associated pollutants since its operation in 1984. A 154-cm-long core was recovered in 2010 in the deepest area of the reservoir and shows the influence of sedimentary infill processes on aggradation rates and selected chemical patterns. During dam operations, the lacustrine aggradation rate is not linear because of three turbiditic-like layers resulting from sediment-laden underflows during major flood events in 1996, 2003 and 2008. These three events contribute to 43% of the 151 kg·m−2 of accumulated sediments over the 1984–2010 period. Trace element solid sources are activated during these floods as selected metals present the highest enrichment factors, levels never reached during interflood periods. In addition, sedimentological and detrital geochemical signals during these events influence anthropogenic trace element signals by a variable dilution effect (maximumduring the increasing discharge stage). Hence, coupling sedimentological and geochemical approaches allows us to understand the sedimentary infill dynamics and, more specifically, to take into account the influence of floods on the temporal trajectories of pollutants.
dc.language.isoENen_US
dc.subject.enLoire basin
dc.subject.enSedimentary archive
dc.subject.enAge model
dc.subject.enFlood event
dc.subject.enDetrital trace elements
dc.subject.enVillerest Dam reservoir
dc.title.enInfluences of major flood sediment inputs on sedimentary and geochemical signals archived in a reservoir core (Upper Loire Basin, France)
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.catena.2014.10.030en_US
dc.subject.halPlanète et Univers [physics]/Océan, Atmosphèreen_US
dc.subject.halPlanète et Univers [physics]/Interfaces continentales, environnementen_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalCATENAen_US
bordeaux.page75 - 85en_US
bordeaux.volume126en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamTGMen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifierhal-01806672
hal.version1
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exportfalse
workflow.import.sourcehal
dc.rights.ccPas de Licence CCen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=CATENA&rft.date=2015-03&rft.volume=126&rft.spage=75%20-%2085&rft.epage=75%20-%2085&rft.eissn=0341-8162&rft.issn=0341-8162&rft.au=DHIVERT,%20Elie&GROSBOIS,%20C%C3%A9cile&COYNEL,%20Alexandra&LEF%C3%88VRE,%20I.&DESMET,%20Marc&rft.genre=article


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