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Features of velocity distribution and secondary flow in compound channel with vegetation
  • +4
  • Zhi-Peng Zhu,
  • * Fei-Dong,
  • Wang Weijie,
  • Han-Qing Zhao,
  • Jin-Jin Li,
  • Qing Feng- Meng,
  • Da-Cheng Li
Zhi-Peng Zhu
Power Construction Corporation of China Guiyang Engineering Corporation Limited
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* Fei-Dong
State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin

Corresponding Author:dongfei@iwhr.com

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Wang Weijie
State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin
Author Profile
Han-Qing Zhao
China Three Gorges Corporation
Author Profile
Jin-Jin Li
State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin
Author Profile
Qing Feng- Meng
Power Construction Corporation of China Guiyang Engineering Corporation Limited
Author Profile
Da-Cheng Li
Power Construction Corporation of China Guiyang Engineering Corporation Limited
Author Profile

Abstract

s: In riverine, marsh, coastal, and other environments, vegetation communities are widely distributed and interact with the flow system to produce more complicated flow structures. Four sets of indoor flume vegetation flow experiments were conducted using a typical Beach trough structure in the lower sections of the Yangtze River as an example. The compound channel was divided into the main channel zone, side slope zone, and side beach zone, and simulated vegetation such as reed, sedge, and dwarf grass was used. The emphasis was on the hydrodynamic properties under semi-covered submerged rigid vegetation and semi-covered non-submerged rigid vegetation. This research focuses on the Shiono and Knight equations (SKM model) to clarify the distribution characteristics of cross-section flow velocity and the ”equivalent diameter D” of gradual vegetation in water. We also propose a new secondary flow model using a genetic algorithm and investigate the relationship between the parameters of the vegetation the flow structure and the distribution pattern of the secondary flow coefficient values. Finally, it employs the Taylor method to demonstrate that the proposed ”equivalent diameter D” of the vegetation has some value within a reasonable threshold range. Eventually, the depth-averaged velocity of the compound channel was accurately predicted by combining the experimental data with the novel SKM model. The proposed model can provide technical support for river flooding.
Submitted to Hydrological Processes
Submission Checks Completed
Assigned to Editor
Reviewer(s) Assigned
10 Jul 2024Reviewer(s) Assigned
10 Jul 2024Reviewer(s) Assigned
07 Aug 2024Review(s) Completed, Editorial Evaluation Pending
08 Aug 2024Editorial Decision: Revise Minor
19 Sep 20241st Revision Received
20 Sep 2024Submission Checks Completed
20 Sep 2024Assigned to Editor
20 Sep 2024Reviewer(s) Assigned
20 Sep 2024Review(s) Completed, Editorial Evaluation Pending
22 Sep 2024Reviewer(s) Assigned
25 Sep 2024Editorial Decision: Revise Minor
09 Oct 20242nd Revision Received
17 Oct 2024Submission Checks Completed
17 Oct 2024Assigned to Editor
17 Oct 2024Reviewer(s) Assigned
17 Oct 2024Review(s) Completed, Editorial Evaluation Pending
20 Oct 2024Editorial Decision: Revise Minor
04 Nov 20243rd Revision Received
04 Nov 2024Submission Checks Completed
04 Nov 2024Assigned to Editor
04 Nov 2024Reviewer(s) Assigned
04 Nov 2024Review(s) Completed, Editorial Evaluation Pending
04 Nov 2024Editorial Decision: Accept