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Fluid mud transportation at water wedge in the Changjiang Estuary

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Abstract

In situ data show that fluid mud of the Changjiang Estuary consists of fine sediment ranging from 8 to 11.5 μm (median grain-size) including 28.8%-36.4% of clay. The composition of the clay is illite, chlorite, kaolinite and montmoillonite. The FM is a layer of high sediment concentration near the bed and results from flocculation under the environment of salt and fresh water mixing. Three kinds of FM have been identified under typical dynamic conditions: the first one is formed at slack water of ebb tide during the flood season, with the characteristics of extended area and low thickness; the second one is formed following a storm, characterized by large area and larger thickness; the third one is formed around the front of the saltwater wedge, characterized by small area but large thickness. In the dredged channel, the FM can be accumulated up to 1 m thick. In general, FM will change with the alternation from spring to neap tides, flood and dry seasons. Drastic change can happen during storms. At the same time, the change of FM is closely related to the erosion and growth of the mouth bar.

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Authors and Affiliations

  1. State Key Laboratory of Estuarine and Coastal Research, East China Normal University, 200062, Shanghai, China

    Jiufa Li, Qing He, Weihua Xiang, Xinning Wan & Huanting Shen

Authors
  1. Jiufa Li
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  2. Qing He
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  3. Weihua Xiang
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  4. Xinning Wan
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  5. Huanting Shen
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Li, J., He, Q., Xiang, W. et al. Fluid mud transportation at water wedge in the Changjiang Estuary. Sc. China Ser. B-Chem. 44 (Suppl 1), 47–56 (2001). https://doi.org/10.1007/BF02884808

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  • DOI: https://doi.org/10.1007/BF02884808

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