中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Flow-Sediment Interaction and Formation Mechanism of Sediment Longitudinal Streaky Structures in Rough Channel Flows

文献类型:期刊论文

作者Wang, Hao5; Kong, Xiangju5; Zhong, Qiang1,4; Yang, Feiqi5; Zhang, Chendi2,3; Wu, Wei5
刊名JOURNAL OF HYDRAULIC ENGINEERING
出版日期2025
卷号151期号:1页码:17
关键词Longitudinal sediment streaks Streamwise vortex Movement characteristic Bed structure Formation mechanism
ISSN号0733-9429
DOI10.1061/JHEND8.HYENG-13984
产权排序4
英文摘要Bed-load streaky structures are typical bed morphological features, yet its formation mechanism remains unclear. To fill this knowledge gap, flume experiments were conducted to quantitatively identify the characteristics of turbulent coherent structures, sediment particle movement, and bed surface structure. An innovative workflow was established that combines the particle tracking velocimetry method with the Kalman filter algorithm, specifically for identifying the trajectories of sediment particles on the bed surface. Feature matching velocity was applied to acquire the flow surface field and structure-from-motion (SFM) was used to reconstruct the three-dimensional bed topography. All the flow velocity, sediment movement, and bedforms show streaky features in the streamwise direction at 0. 0680.113. The instantaneous turbulence properties of turbulent flow and sediment movement in the spanwise direction disappear, and fixed time-averaged streaky structures are formed. The streaky structures have larger characteristic scales (width and spanwise distance) in the middle of the channel than those near the sidewalls. The spanwise distance between adjacent streaky structures remains about twice the whole flow depth. Finally, this study proposes a formation mechanism based on fluid-sediment interactions, offering innovative measurement and analysis methods that can significantly contribute to understanding these interactions.
WOS关键词CELLULAR SECONDARY CURRENTS ; VORTEX ORGANIZATION ; TURBULENCE ; BED ; REGION
资助项目Open Research Fund of Key Laboratory of Sediment Science and Northern River Training ; Ministry of Water Resources, China Institute of Water Resources and Hydropower Research[IWHR-SEDI-2022-09] ; Open Fund of the Zhejiang River and Port Institute[ZIHE21003] ; Natural Science Foundation of Fujian Province[2023J01406]
WOS研究方向Engineering ; Water Resources
语种英语
WOS记录号WOS:001365144800022
出版者ASCE-AMER SOC CIVIL ENGINEERS
资助机构Open Research Fund of Key Laboratory of Sediment Science and Northern River Training ; Ministry of Water Resources, China Institute of Water Resources and Hydropower Research ; Open Fund of the Zhejiang River and Port Institute ; Natural Science Foundation of Fujian Province
源URL[http://ir.igsnrr.ac.cn/handle/311030/211715]  
专题陆地表层格局与模拟院重点实验室_外文论文
通讯作者Zhong, Qiang
作者单位1.China Agr Univ, Coll Water Resources & Civil Engn, Beijing 100083, Peoples R China
2.Sichuan Univ, State Key Lab Hydraul & Mt River Engn, Chengdu 610065, Peoples R China
3.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Land Surface Pattern & Simulat, Beijing 100101, Peoples R China
4.Beijing Engn Res Ctr, Safety & Energy Saving Technol Water Supply Networ, Beijing 100083, Peoples R China
5.Fuzhou Univ, Coll Civil Engn, Fuzhou 350116, Peoples R China
推荐引用方式
GB/T 7714
Wang, Hao,Kong, Xiangju,Zhong, Qiang,et al. Flow-Sediment Interaction and Formation Mechanism of Sediment Longitudinal Streaky Structures in Rough Channel Flows[J]. JOURNAL OF HYDRAULIC ENGINEERING,2025,151(1):17.
APA Wang, Hao,Kong, Xiangju,Zhong, Qiang,Yang, Feiqi,Zhang, Chendi,&Wu, Wei.(2025).Flow-Sediment Interaction and Formation Mechanism of Sediment Longitudinal Streaky Structures in Rough Channel Flows.JOURNAL OF HYDRAULIC ENGINEERING,151(1),17.
MLA Wang, Hao,et al."Flow-Sediment Interaction and Formation Mechanism of Sediment Longitudinal Streaky Structures in Rough Channel Flows".JOURNAL OF HYDRAULIC ENGINEERING 151.1(2025):17.

入库方式: OAI收割

来源:地理科学与资源研究所

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