4.5 Article

Flocculation of suspended particles during estuarine mixing in the Changjiang estuary-East China Sea

Journal

JOURNAL OF MARINE SYSTEMS
Volume 233, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.jmarsys.2022.103766

Keywords

Changjiang (Yangtze) River Estuary; Estuarine mixing; Flocculation; Laser in situ scattering and transmissometry (LISST); SPM dynamics; Stable carbon isotopes(d(13)C)

Funding

  1. Science and Technology Commission of Shanghai Municipality [19230711900]
  2. National Natural Science Foundation of China [U2040216]
  3. fundamental research funds for the central universities of China

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Flocculation, an important process in estuarine mixing, plays a fundamental role in land-to-sea interactions. In this study, the use of LISST measurements and stable isotopic ratios of delta C-13 greatly improved our understanding of suspended particulate matter (SPM) dynamics in the Changjiang River Estuary. The results revealed that flocculation processes were influenced by phytoplankton blooms and involved the aggregation of smaller particles into larger ones.
Flocculation, triggered during estuarine mixing plays an important role in land-to-sea interactions and is a fundamental topic in near-shore oceanographic studies. Identifying in situ flocculation in large-river estuaries can be challenging due to the complex seawater circulation and heterogeneous suspended particulate matter (SPM) composition in these areas. In this study, three cruises were conducted in the Changjiang (Yangtze) River Estuary and the adjacent area in March, May, and July 2016. Vertical profiles of SPM total volume, mean size, and size spectra were determined using laser in situ scattering and transmissometry (LISST) measurements at 66-89 stations during the three cruises. Stable isotopic ratios of delta C-13 were also measured in the organic carbon contents of SPM collected at the surface, middle, and bottom layers of the sampling stations. LISST data were used to successfully identify the flocculation occurring in the field as well as to trace SPM size spectrum changes before and after the flocculation process. The delta C-13 values were utilized to study the response of biogeochemical parameters to the flocculation. Phytoplankton blooms occurring in May largely resulted in discontinuous variations in LISST parameters and delta C-13 from March to July. Although the pattern of SPM size spectra involved in flocculation differed among seasons, flocculation processes were always contributed by smaller particles with sizes of several tens of mu m aggregating into larger ones > 300 mu m. Using LISST and delta C-13 measurements combined greatly improved our understanding of SPM dynamics in estuarine and coastal areas where estuarine flocculation was a critical component.

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