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Flow dynamics and turbulent coherent structures around sediment reduction plates of a sewer system.
Li, Zhiwei; Wang, Bing; Wang, Feifei; Sun, Bin; Li, Liutao.
Afiliação
  • Li Z; School of Water Conservancy and Transportation, Zhengzhou University, Zhengzhou, 450001, China; Yellow River Laboratory, Zhengzhou University, Zhengzhou, 450001, China. Electronic address: zwli@zzu.edu.cn.
  • Wang B; School of Water Conservancy and Transportation, Zhengzhou University, Zhengzhou, 450001, China; Yellow River Laboratory, Zhengzhou University, Zhengzhou, 450001, China. Electronic address: wang2541883646@163.com.
  • Wang F; School of Water Conservancy and Transportation, Zhengzhou University, Zhengzhou, 450001, China; Yellow River Laboratory, Zhengzhou University, Zhengzhou, 450001, China. Electronic address: ffwang@zzu.edu.cn.
  • Sun B; School of Water Conservancy and Transportation, Zhengzhou University, Zhengzhou, 450001, China; Yellow River Laboratory, Zhengzhou University, Zhengzhou, 450001, China. Electronic address: sunbin@zzu.edu.cn.
  • Li L; School of Water Conservancy and Transportation, Zhengzhou University, Zhengzhou, 450001, China; Yellow River Laboratory, Zhengzhou University, Zhengzhou, 450001, China. Electronic address: 1399694635@qq.com.
J Environ Manage ; 366: 121594, 2024 Aug.
Article em En | MEDLINE | ID: mdl-38971061
ABSTRACT
In the management of urban drainage networks, great interest has been generated in the removal of sediments from sewer systems. The unsteady three-dimensional (3D) flow and turbulent coherent structures surrounding sediment reduction plates in a sewer system are investigated by means of the detached-eddy simulation (DES). Particular emphasis is given to detailing the instantaneous velocity and vorticity fields within the grooves, along with an examination of the three-dimensional, long-term, average flow structure at a Reynolds number of approximately 105. Velocity vectors demonstrate continuous flapping of the flow on the groove wall, periodically interacting with ejections of positive and negative vorticity originating from the grooves. The interaction between the three-dimensional groove flow and the shear flow leads to the downstream transport of patches of positive and negative vorticity, which significantly influence sediment transport. The high-velocity shear flows and strong vortices generated in undulating topography, as identified by the Q-criteria, are the key factors contributing to the efficient sediment reduction capabilities of the sediment reduction plates. The sediment reduction plates with partially enclosed structures exhibit low sedimentation rates in grooves on the plate, a broader acceleration region, and a lesser impact on the flow capacity. The results improve the understanding of the hydrodynamics and turbulent coherent structures surrounding the sediment reduction plates while elucidating the driving factors behind the enhancement of sediment scouring and suspension capacities. These results indicate that the redesign of the plates as partially enclosed structures contributes to further improving their sediment reduction performance.
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Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Assunto principal: Esgotos / Hidrodinâmica Idioma: En Revista: J Environ Manage Ano de publicação: 2024 Tipo de documento: Article

Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Assunto principal: Esgotos / Hidrodinâmica Idioma: En Revista: J Environ Manage Ano de publicação: 2024 Tipo de documento: Article