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dc.contributor.authorYang, L.
dc.contributor.authorHuai, W.
dc.contributor.authorGuo, Yakun
dc.date.accessioned2022-03-22T14:00:42Z
dc.date.accessioned2022-04-21T07:42:14Z
dc.date.available2022-03-22T14:00:42Z
dc.date.available2022-04-21T07:42:14Z
dc.date.issued2021-09-09
dc.identifier.citationYang L, Huai W and Guo Y (2021) Stochastic Simulation of the Suspended Sediment Deposition in the Channel With Vegetation and Its Relevance to Turbulent Kinetic Energy. Water Resources Research. 57(9): e2021WR030380.en_US
dc.identifier.urihttp://hdl.handle.net/10454/18911
dc.descriptionYesen_US
dc.description.abstractThe aquatic vegetation patch plays a significant role on sediment net deposition in the vegetated channels. Particularly, the flow is decelerated at the leading edge of a patch that tends to induce vertical updraft, that is, a diverging flow region, in which vegetation greatly affects the pattern of sediment net deposition. This study focuses on the simulation of the sediment net deposition in the whole vegetation patch region through an innovative random displacement model, a Lagrange method, with probability-based boundary conditions, instead of the reflection or sorption boundary at the channel bottom. The probability model of deposition and resuspension is proposed according to the flow field characteristics in the different regions of the vegetation patch. The variation of the sediment deposition and resuspension with the turbulent kinetic energy is analyzed to illustrate the effect of the turbulence induced by vegetation, represented by the dimensionless turbulent kinetic energy (ψ), on the sediment deposition and resuspension. The sediment deposition predicted by the proposed model agrees well with the experimental measurements. Results show that the effect of vegetation on the sediment deposition and resuspension motions begins to prevail when the vegetation-induced ψ is larger than its threshold, ψ *. The threshold of ψ is predicted to be within 6.8–10 according to the simulation results in this study. As the turbulent kinetic energy increases, the deposition probability decreases continuously when ψ > ψ *.en_US
dc.description.sponsorshipational Natural Science Foundation of China (NSFC). Grant Numbers: 52020105006, 11872285; UK Royal Society - International Exchanges Program. Grant Number: IES\R2\181122; Open Funding of State Key Laboratory of Water Resources and Hydropower Engineering Science (WRHES), Wuhan University. Grant Number: 2018HLG01en_US
dc.language.isoenen_US
dc.relation.isreferencedbyhttps://doi.org/10.1029/2021WR030380en_US
dc.rights(c) 2021 American Geophysical Union. Full-text reproduced in accordance with the publisher's self-archiving policy.en_US
dc.subjectDepositionen_US
dc.subjectResuspensionen_US
dc.subjectTurbulent kinetic energyen_US
dc.subjectRandom displacement modelen_US
dc.subjectVegetation patchen_US
dc.subjectProbability boundary conditionen_US
dc.titleStochastic Simulation of the Suspended Sediment Deposition in the Channel With Vegetation and Its Relevance to Turbulent Kinetic Energyen_US
dc.status.refereedYesen_US
dc.date.Accepted2021-08-26
dc.date.application2021-08-30
dc.typeArticleen_US
dc.type.versionPublished versionen_US
dc.rights.licenseUnspecifieden_US
dc.date.updated2022-03-22T14:00:44Z
refterms.dateFOA2022-04-21T07:43:18Z
dc.openaccess.statusopenAccessen_US


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