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Wen Mingzheng, Tian Lizhu, Zhang Shaotong, Yang Peng, Li Yong, Wang Fu, Wang Zhenhao. 2025. Distribution of suspended sediments and action of nearshore currents in Xiangyun Island, Laoting County, Hebei Province[J]. Geology in China, 52(2): 747−758. DOI: 10.12029/gc20210326006
Citation: Wen Mingzheng, Tian Lizhu, Zhang Shaotong, Yang Peng, Li Yong, Wang Fu, Wang Zhenhao. 2025. Distribution of suspended sediments and action of nearshore currents in Xiangyun Island, Laoting County, Hebei Province[J]. Geology in China, 52(2): 747−758. DOI: 10.12029/gc20210326006

Distribution of suspended sediments and action of nearshore currents in Xiangyun Island, Laoting County, Hebei Province

Funds: Supported by the projects of China Geological Survey (No. DD20211301, No.121201006000182401).
More Information
  • Author Bio:

    WEN Mingzheng, male, born in 1988, doctor candidate, mainly engaged in marine environmental geology; E-mail: wmingzheng@mail.cgs.gov.cn

  • Corresponding author:

    WANG Fu, male, born in 1979, researcher, mainly engaged in modern sediment dating and coastal geological environment research; E-mail: wfu@cgs.cn.

  • Received Date: March 25, 2021
  • Revised Date: May 20, 2021
  • Available Online: March 31, 2025
  • This paper is the result of marine geological survey engineering.

    Objective 

    There are high−quality natural fine sand distributed along the coast of Xiangyun Island in Hebei, which is a famous coastal tourist island. Simultaneous investigation and research on the concentration of suspended sediments and nearshore current in this area is of great significance to the ecological environment of Xiangyun Island and its nearshore engineering.

    Methods 

    The current velocity and flow direction of the sea area were continuously profiled by ship−borne Acoustic Doppler Current Profiler (ADCP), and the distribution of suspended sediments in the sea area was qualitatively discussed according to the backscatter intensity recorded by the instrument.

    Results 

    The survey results show that: (1) The current in Xiangyun bay is mainly parallel to the coastline, which has obvious reciprocation. The magnitude of flood current was obviously larger than ebb current, the flood current was gradually weakened along the shore direction, however the ebb current in the southwest of Xiangyun bay increased along the shore direction; (2) During the transition from flat tide to ebb tide in Xiangyun Island sea area, the current turning starts from the bottom water, and the current turning and tide level change have certain lag; (3) The data of backscatter intensity shows that: there was a high concentration layer in Xiangyun bay coastal area, and the concentration increases along the shore direction, and the concentration of suspended sediment gradually decreases from northeast to southwest.

    Conclusions 

    Xiangyun Island coastal waters under the action of the tidal current, suspended sediment along Xiangyun Island shoreline from northeast to southwest, is the main reason for the Xiangyun Island in the northeast section erosion and the southwest section deposition.

    Highlights
    The synchronous measurement of current velocity, direction, and suspended sediment concentration was carried out using ship-borne ADCP, elucidating the distribution characteristics of suspended sediment in the Xiangyun Island sea area and the action of nearshore currents.
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