中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Floc size asymmetry modulated by tidal dynamics drives net landward sediment transport in a man-made tidal channel

文献类型:期刊论文

作者Li, Wenjian1,2; Lee, Guan-hong1; Chang, Jongwi1; Ajama, Ojudoo Darius1; Wang, Zhenyan2
刊名MARINE GEOLOGY
出版日期2025-10-01
卷号488页码:16
关键词Tidal flat Floc size Shear velocity Tidal asymmetry Flocculation
ISSN号0025-3227
DOI10.1016/j.margeo.2025.107615
通讯作者Lee, Guan-hong(ghlee@inha.ac.kr)
英文摘要In natural aquatic systems, flocculation affects sediment transport by altering particle size and settling velocity. However, the asymmetry in floc size over tidal cycles and its influence on sediment transport, especially in turbid coastal regions affected by human activities, remains understudied. This study uses comprehensive observations from ADV, HR-ADCP, Signature ADCP, LISST, and CTD within a man-made tidal channel located on the west coast of the Korean Peninsula to elucidate the size-dependent sediment transport process. Our findings reveal a tidal asymmetry in bottom shear velocity and particle size distribution (PSD). During ebb tide, the bottom shear velocity was higher, but suspended sediment concentration (SSC), Total Volume Concentration (TVC), and mean size (Mz) were lower compared to flood tide. This suggests that advection transport, in addition to resuspension, is a significant source of particles during flood tide. These particles increased SSC, TVC, and landward sediment flux, while low shear velocity facilitated flocculation, resulting in higher Mz. Consequently, a higher proportion of microflocs and macroflocs occurred, leading to a higher settling flux from flood tide to high slack water. In contrast, weaker advection transport and low SSC during ebb tide led to lower seaward sediment flux, with stronger shear velocity and lower concentration resulting in weak flocculation and lower Mz. During ebb tide, flocculi (10-20 mu m diameter) exceeded microflocs and macroflocs, causing a lesser settling flux. This tidal asymmetry in floc size explains the trapping of larger particles during flood tide and high water levels, ultimately leading to net landward sediment flux in the channel over tidal cycles.
WOS关键词SETTLING VELOCITY ; SUSPENDED SEDIMENT ; PARTICLE-SIZE ; SHEAR-STRESS ; FLOCCULATION ; ESTUARY ; TURBULENCE ; MATTER ; FLATS ; MODEL
资助项目National Natural Science Foundation of China[42306059] ; Ministry of Oceans and Fisheries, Korea[20210607] ; China Postdoctoral Science Foundation[2020M682246] ; China Scholarship Council
WOS研究方向Geology ; Oceanography
语种英语
WOS记录号WOS:001533241700001
出版者ELSEVIER
源URL[http://ir.qdio.ac.cn/handle/337002/202592]  
专题海洋研究所_海洋地质与环境重点实验室
通讯作者Lee, Guan-hong
作者单位1.Inha Univ, Dept Oceanog, 100 Inharo, Incheon 22212, South Korea
2.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China
推荐引用方式
GB/T 7714
Li, Wenjian,Lee, Guan-hong,Chang, Jongwi,et al. Floc size asymmetry modulated by tidal dynamics drives net landward sediment transport in a man-made tidal channel[J]. MARINE GEOLOGY,2025,488:16.
APA Li, Wenjian,Lee, Guan-hong,Chang, Jongwi,Ajama, Ojudoo Darius,&Wang, Zhenyan.(2025).Floc size asymmetry modulated by tidal dynamics drives net landward sediment transport in a man-made tidal channel.MARINE GEOLOGY,488,16.
MLA Li, Wenjian,et al."Floc size asymmetry modulated by tidal dynamics drives net landward sediment transport in a man-made tidal channel".MARINE GEOLOGY 488(2025):16.

入库方式: OAI收割

来源:海洋研究所

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