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Spatial variation of and the factors influencing the floc size distribution in the North Yellow Sea during the winter season
Li, Wenjian1; Wang, Zhenyan1,2,3,4; Lee, Guan-hong5; Figueroa, Steven Miguel5; Huang, Haijun1,3,4
2021-12-01
发表期刊MARINE GEOLOGY
ISSN0025-3227
卷号442页码:14
通讯作者Wang, Zhenyan(zywang@qdio.ac.cn)
摘要Suspended particulate matter (SPM) usually exists in the ocean as floc, the behavior of which is believed to be significant for the source to sink sedimentary systems. However, the spatial variation of floc size distributions on the shelf scale is not fully understood. In this study, the SPM floc size distribution and the corresponding hydrological conditions in the North Yellow Sea are delineated to examine the spatial variation of floc size and the influencing factors based on a comprehensive investigation conducted during January 2017. The results indicate that the fine primary particles and microflocs display high volume concentration (C-v) around the tip of the Shandong Peninsula both in surface and bottom layers, while the macroflocs dominate the western North Yellow Sea. The primary particles (<4.48 mu m) and micmflocs (4.48-219 mu m) are mainly inorganic particles, whereas the macroflocs (>219 mu m) are dominated by phytoplankton and mucus-bound organic aggregates. The higher C-v of primary particles and microflocs around the tip of Shandong Peninsula mainly results from the resuspension of bottom sediments. Temperature fronts limit the spread of SPM from the coastal area to the offshore area in surface layer, while the bottom sediments tend to cross the temperature front and spread seaward. In the western North Yellow Sea, flocculation is enhanced by plankton which accounts for the dominance of macroflocs, especially in surface layer. The Yellow Sea Warm Current may transport sediments that cross the temperature front in the bottom layer back to the central North Yellow Sea or South Yellow Sea in the winter season. Until the summer season, the deposition of macroflocs may contribute to the formation of mud deposits in the Yellow Sea.
关键词North Yellow Sea Suspended particulate matter Hoc size distribution LISST Temperature front
DOI10.1016/j.margeo.2021.106660
收录类别SCI
语种英语
资助项目Strategic Priority Research Program of the Chinese Academy of Sciences[XDA19060401] ; Strategic Priority Research Program of the Chinese Academy of Sciences[XDB42010203] ; Strategic Priority Research Program of the Chinese Academy of Sciences[XDA23050503] ; National Natural Science Foundation Project[41476045] ; China Post-doctoral Science Foundation[2020M682246] ; Post-doctoral Applied Research Project of Qingdao ; Yellow Sea ocean observation and research station OMORN ; NSFC Open Research Cruise - Shiptime Sharing Project of the NSFC[NORC2016-01]
WOS研究方向Geology ; Oceanography
WOS类目Geosciences, Multidisciplinary ; Oceanography
WOS记录号WOS:000706525800015
出版者ELSEVIER
引用统计
被引频次:1[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.qdio.ac.cn/handle/337002/176688
专题海洋地质与环境重点实验室
通讯作者Wang, Zhenyan
作者单位1.Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China
2.Pilot Natl Lab Marine Sci & Technol, Lab Marine Mineral Resources, Qingdao 266071, Peoples R China
3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
4.Chinese Acad Sci, Ctr Ocean Megasci, Qingdao 266071, Peoples R China
5.Inha Univ, Dept Oceanog, 100 Inharo, Incheon 22212, South Korea
第一作者单位中国科学院海洋研究所
通讯作者单位中国科学院海洋研究所;  中国科学院海洋大科学研究中心
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GB/T 7714
Li, Wenjian,Wang, Zhenyan,Lee, Guan-hong,et al. Spatial variation of and the factors influencing the floc size distribution in the North Yellow Sea during the winter season[J]. MARINE GEOLOGY,2021,442:14.
APA Li, Wenjian,Wang, Zhenyan,Lee, Guan-hong,Figueroa, Steven Miguel,&Huang, Haijun.(2021).Spatial variation of and the factors influencing the floc size distribution in the North Yellow Sea during the winter season.MARINE GEOLOGY,442,14.
MLA Li, Wenjian,et al."Spatial variation of and the factors influencing the floc size distribution in the North Yellow Sea during the winter season".MARINE GEOLOGY 442(2021):14.
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