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dc.contributor.authorLiu, W.
dc.contributor.authorWang, B.
dc.contributor.authorGuo, Yakun
dc.date.accessioned2022-03-22T14:10:43Z
dc.date.accessioned2022-03-30T09:13:57Z
dc.date.available2022-03-22T14:10:43Z
dc.date.available2022-03-30T09:13:57Z
dc.date.issued2021-11
dc.date.issued2021-11
dc.identifier.citationLiu W, Wang B and Guo Y (2021) Numerical study of the dam-break waves and Favre waves down sloped wet rigid-bed at laboratory scale. Journal of Hydrology. 602: 126752.en_US
dc.identifier.urihttp://hdl.handle.net/10454/18823
dc.identifier.urihttp://hdl.handle.net/10454/18823
dc.descriptionYesen_US
dc.description.abstractThe bed slope and the tailwater depth are two important ones among the factors that affect the propagation of the dam-break flood and Favre waves. Most previous studies have only focused on the macroscopic characteristics of the dam-break flows or Favre waves under the condition of horizontal bed, rather than the internal movement characteristics in sloped channel. The present study applies two numerical models, namely, large eddy simulation (LES) and shallow water equations (SWEs) models embedded in the CFD software package FLOW-3D to analyze the internal movement characteristics of the dam-break flows and Favre waves, such as water level, the velocity distribution, the fluid particles acceleration and the bed shear stress, under the different bed slopes and water depth ratios. The results under the conditions considered in this study show that there is a flow state transition in the flow evolution for the steep bed slope even in water depth ratio α = 0.1 (α is the ratio of the tailwater depth to the reservoir water depth). The flow state transition shows that the wavefront changes from a breaking state to undular. Such flow transition is not observed for the horizontal slope and mild bed slope. The existence of the Favre waves leads to a significant increase of the vertical velocity and the vertical acceleration. In this situation, the SWEs model has poor prediction. Analysis reveals that the variation of the maximum bed shear stress is affected by both the bed slope and tailwater depth. Under the same bed slope (e.g., S0 = 0.02), the maximum bed shear stress position develops downstream of the dam when α = 0.1, while it develops towards the end of the reservoir when α = 0.7. For the same water depth ratio (e.g., α = 0.7), the maximum bed shear stress position always locates within the reservoir at S0 = 0.02, while it appears in the downstream of the dam for S0 = 0 and 0.003 after the flow evolves for a while. The comparison between the numerical simulation and experimental measurements shows that the LES model can predict the internal movement characteristics with satisfactory accuracy. This study improves the understanding of the effect of both the bed slope and the tailwater depth on the internal movement characteristics of the dam-break flows and Favre waves, which also provides a valuable reference for determining the flood embankment height and designing the channel bed anti-scouring facility.en_US
dc.description.sponsorshipNational Natural Science Foundation of China (Grant No: 51879179, 52079081), the Open Fund from the State Key Laboratory of Hydraulics and Mountain River Engineering, Sichuan University (SKHL1809) and the Sichuan Science and Technology Program (No. 2019JDTD0007)en_US
dc.language.isoenen_US
dc.rights© 2021 Elsevier. Reproduced in accordance with the publisher's self-archiving policy. This manuscript version is made available under the CC-BY-NC-ND 4.0 license.en_US
dc.subjectBed shear stressen_US
dc.subjectBed slopeen_US
dc.subjectDam-break flowen_US
dc.subjectLarge eddy simulationen_US
dc.subjectVelocity profileen_US
dc.subjectWet beden_US
dc.titleNumerical study of the dam-break waves and Favre waves down sloped wet rigid-bed at laboratory scaleen_US
dc.status.refereedYesen_US
dc.date.Accepted2021-07-25
dc.date.application2021-07-30
dc.typeArticleen_US
dc.type.versionAccepted manuscripten_US
dc.identifier.doihttps://doi.org/10.1016/j.jhydrol.2021.126752
dc.rights.licenseCC-BY-NC-NDen_US
dc.date.updated2022-03-22T14:10:53Z
refterms.dateFOA2022-03-30T09:20:15Z
dc.openaccess.statusopenAccessen_US


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