Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/111122
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dc.contributorDepartment of Civil and Environmental Engineeringen_US
dc.creatorSong, SYen_US
dc.creatorWang, XKen_US
dc.creatorDuan, HFen_US
dc.creatorStocchino, Aen_US
dc.creatorYan, XFen_US
dc.date.accessioned2025-02-17T01:37:30Z-
dc.date.available2025-02-17T01:37:30Z-
dc.identifier.issn1070-6631en_US
dc.identifier.urihttp://hdl.handle.net/10397/111122-
dc.language.isoenen_US
dc.publisherAIP Publishing LLCen_US
dc.rights© 2024 Author(s). Published under an exclusive license by AIP Publishing.en_US
dc.rightsThis article may be downloaded for personal use only. Any other use requires prior permission of the author and AIP Publishing. This article appeared in Si-Yuan Song, Xie-Kang Wang, Huan-Feng Duan, Alessandro Stocchino, Xu-Feng Yan; Numerical investigation of a three-dimensional flow structure influenced by the lateral expansion of a partially distributed submerged canopy. Physics of Fluids 1 August 2024; 36 (8): 085164 and may be found at https://doi.org/10.1063/5.0221723.en_US
dc.titleNumerical investigation of a three-dimensional flow structure influenced by the lateral expansion of a partially distributed submerged canopyen_US
dc.typeJournal/Magazine Articleen_US
dc.description.otherinformationAuthor name used in this publication: 宋思源en_US
dc.description.otherinformationAuthor name used in this publication: 王协康en_US
dc.description.otherinformationAuthor name used in this publication: 段焕丰en_US
dc.description.otherinformationAuthor name used in this publication: 闫旭峰en_US
dc.identifier.spage085164-1en_US
dc.identifier.epage085164-18en_US
dc.identifier.volume36en_US
dc.identifier.issue8en_US
dc.identifier.doi10.1063/5.0221723en_US
dcterms.abstractThis study employed numerical simulations to investigate the three-dimensional hydrodynamic structure of a channel obstructed by submerged rigid canopies. After validating the model using existing experimental data, a series of numerical experiments varying the canopy density and the blocking ratio were conducted. The results indicate that submerged canopy, different from emergent canopies, triggers the generation of three-dimensional coherent vortices. When canopies expand laterally, the scale, location, and evolution characteristics of cross-sectional secondary flows vary. The direction of secondary circulation at the canopy top of the fully covered vegetation channel is affected by the river width/depth ratio. Three-dimensional coherent vortices are jointly controlled by vertical and transverse Reynolds stresses. When the channel is seriously blocked, the degree of momentum exchange in the mixing layer does not change significantly. The boundary friction effect dominates the momentum exchange process near the wall. An equation coupling the drag length scale and blocking ratio with the vertical coherent vortex penetration length is proposed, indicating that the penetration length increases exponentially with both variables. Higher canopy density exhibits a stronger resistance to the vertical coherent vortex penetration length. In the process of canopy lateral expansion, the evolution time of the outer vortex to scale stability is longer than that of the inner vortex. The significance of research on the three-dimensional vortex structure of rigid submerged vegetation is established based on previous studies and existing conclusions.en_US
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationPhysics of fluids, Aug. 2024, v. 36, no. 8, 085164, p. 085164-1 - 085164-18en_US
dcterms.isPartOfPhysics of fluidsen_US
dcterms.issued2024-08-
dc.identifier.scopus2-s2.0-85201870476-
dc.identifier.eissn1089-7666en_US
dc.identifier.artn085164en_US
dc.description.validate202502 bcchen_US
dc.description.oaVersion of Recorden_US
dc.identifier.FolderNumberOA_Others-
dc.description.fundingSourceOthersen_US
dc.description.fundingTextNational Natural Science Foundation of China; National Natural Science Foundation of Joint Fund for Changjiang River Water Science Research; Sichuan Science and Technology Program; Open Research Fund of State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, the China Institute of Water Resources and Hydropower Research; State Key Laboratory of Hydraulics and Mountain River Engineering, Sichuan Universityen_US
dc.description.pubStatusPublisheden_US
dc.description.oaCategoryVoR alloweden_US
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