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dc.rights.licenseopenen_US
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorDEFONTAINE, Sophie
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorJALON ROJAS, Isabel
ORCID: 0000-0003-4254-4084
IDREF: 160580730
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorSOTTOLICHIO, Aldo
IDREF: 158099699
dc.contributor.authorGRATIOT, Nicolas
dc.contributor.authorLEGOUT, Cédric
dc.date.accessioned2024-01-22T11:09:35Z
dc.date.available2024-01-22T11:09:35Z
dc.date.issued2023-03-01
dc.identifier.issn0025-3227en_US
dc.identifier.urioai:crossref.org:10.1016/j.margeo.2023.106995
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/187367
dc.description.abstractEnAn optical settling column was used in the Garonne Tidal River to estimate the settling velocity of suspended matter in surface waters over a period characterized by contrasting hydrological conditions. A time and space variability of settling velocity was observed during this study. The settling velocities of surface suspended matter ranged from 0.018 to 0.268 mm:s�����1, and the median diameter of dispersed particles varied from 4.74 to 14.38 m. The data revealed the physical processes influencing the sediment settling dynamics throughout different time scales in a highly turbid tidal river. On tidal and fortnightly time scales, resuspension, deposition and advection mechanisms were the major drivers of the settling velocity variability, while it is likely that the estuarine turbidity maxima (ETM) was responsible for seasonal variations. The findings of this work suggest that in tidal rivers, salinity is too low to promote flocculation, whereas ETM can play a key role in enhancing this process. The stronger variability in settling velocity occurs on a tidal timescale, with median values up to four times higher at the end of the ebb tide than at high water. These variations cannot be correlated to salinity or sediment concentration. On a seasonal timescale, flocculation appears to be strongly correlated with the presence of the ETM and associated fluid mud layer. A simple correlation based on tidal variations seems to be a better predictor than the relationships based on the sediment concentration.
dc.language.isoENen_US
dc.sourcecrossref
dc.subject.ensediment dynamics
dc.subject.ensettling velocity
dc.subject.encohesive sediment
dc.subject.enETM
dc.subject.enSCAF
dc.subject.entidal river
dc.title.enSettling dynamics of cohesive sediments in a highly turbid tidal river
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.margeo.2023.106995en_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalMarine Geologyen_US
bordeaux.page106995en_US
bordeaux.volume457en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamMETHYSen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcedissemin
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exportfalse
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=Marine%20Geology&rft.date=2023-03-01&rft.volume=457&rft.spage=106995&rft.epage=106995&rft.eissn=0025-3227&rft.issn=0025-3227&rft.au=DEFONTAINE,%20Sophie&JALON%20ROJAS,%20Isabel&SOTTOLICHIO,%20Aldo&GRATIOT,%20Nicolas&LEGOUT,%20C%C3%A9dric&rft.genre=article


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