Coupling between physical processes and biogeochemistry of suspended particles over the inner shelf mud in the East China Sea Article Swipe
James T. Liu
,
Jay Lee
,
Rick J. Yang
,
Xiaoqin Du
,
Anchun Li
,
Yu‐Shih Lin
,
Chih‐Chieh Su
,
Shuqin Tao
·
YOU?
·
· 2021
· Open Access
·
· DOI: https://doi.org/10.1016/j.margeo.2021.106657
YOU?
·
· 2021
· Open Access
·
· DOI: https://doi.org/10.1016/j.margeo.2021.106657
This study examines how geochemical signals regarding the source and transformation in suspended particles are transported in the marine portion of the sediment dispersal system. In the source-to-sink sedimentary continuum of a world major river, the Changjiang (Yangtze) River, is used to demonstrate the close coupling between the marine physical processes and the geochemical signals carried by suspended particles. A sediment trap mooring configured with a non-sequential sediment trap, a downward-looking ADCP, CTD, LISST-100× were deployed for 29 days in the winter of 2014 off the coast of Zhejiang Province, China in water depth of 22.5 m. The mooring rendered two types of data. Physical processes included temporal changes of water depth, currents at 11 depths, temperature at two depths, and salinity at one depth. There was 15-cm accumulation of captured particles in the trap, which rendered the total mass flux of 233.3 g/cm2/day. The trap material was analyzed for grain-size composition, total 210Pb, minerals including mica/illite, kaolinite, chlorite, k-feldspar, plagioclase, quartz, and dolomite. Organic material (TOC, TN) and carbon isotope δ13C were also measured. The range of terrestrial fraction (Ft) of the trap material was between 45–60%. EOF analysis was used to examine the covariability in both data sets. For the physical data set, 37 variables were used in the analysis. For the sediment trap material, 15 variables were used. The EOF results of the physical processes indicate the tidal flow was the most important physical forcing for the transport of suspended particles and water masses that carried marine- and terrestrial-sourced particles. Wave and current combined resuspension entrained reworked sediment off the seabed, which was then transported landward or seaward. The most important covariability of the particle properties in the sediment trap was caused by hydrodynamic sorting that separated the clay from silt and sand sizes. Geochemical signals of the particles were carried by clay and the particle mass (dry weight) was associated with silt and sand. The temporal characteristics of the sorting show the spring-neap tidal cycle. The next major distinction was the contrast between terrestrial- and marine-sourced materials. The EOF analysis further distinguish contributions from the distal Changjiang River and proximal small rivers at the tertiary level of the covariability. The coverabilities in both data sets show close correspondence. Our findings give firm evidence to show marine processes dominated the transport of land-derived fluvial sediment and the incorporation of marine-sourced particles into the dispersal system. There is complexity in both physical processes and geochemical signals of suspended particles. However, our study points out the close coupling between the two.
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Metadata
- Type
- article
- Language
- en
- Landing Page
- https://doi.org/10.1016/j.margeo.2021.106657
- OA Status
- hybrid
- Cited By
- 15
- References
- 140
- Related Works
- 10
- OpenAlex ID
- https://openalex.org/W3203101864
All OpenAlex metadata
Raw OpenAlex JSON
- OpenAlex ID
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https://openalex.org/W3203101864Canonical identifier for this work in OpenAlex
- DOI
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https://doi.org/10.1016/j.margeo.2021.106657Digital Object Identifier
- Title
-
Coupling between physical processes and biogeochemistry of suspended particles over the inner shelf mud in the East China SeaWork title
- Type
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articleOpenAlex work type
- Language
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enPrimary language
- Publication year
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2021Year of publication
- Publication date
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2021-10-01Full publication date if available
- Authors
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James T. Liu, Jay Lee, Rick J. Yang, Xiaoqin Du, Anchun Li, Yu‐Shih Lin, Chih‐Chieh Su, Shuqin TaoList of authors in order
- Landing page
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https://doi.org/10.1016/j.margeo.2021.106657Publisher landing page
- Open access
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YesWhether a free full text is available
- OA status
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hybridOpen access status per OpenAlex
- OA URL
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https://doi.org/10.1016/j.margeo.2021.106657Direct OA link when available
- Concepts
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Geology, Oceanography, Sediment trap, Feldspar, Sediment, Plagioclase, Illite, Mineralogy, Geochemistry, Water column, Quartz, Clay minerals, Geomorphology, PaleontologyTop concepts (fields/topics) attached by OpenAlex
- Cited by
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15Total citation count in OpenAlex
- Citations by year (recent)
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2025: 4, 2024: 3, 2023: 5, 2022: 2, 2021: 1Per-year citation counts (last 5 years)
- References (count)
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140Number of works referenced by this work
- Related works (count)
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10Other works algorithmically related by OpenAlex
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