Characteristics and controlling factors of suspended sediment transportation in summer spring tide in Funing Bay

YI Zhaohan; HU Rijun; LI Yi; CHEN Xiaoci; CHEN Juanjuan; MENG Lingpeng; ZHU Longhai; ZHANG Xiaodong

doi:10.16562/j.cnki.0256-1492.2021040401

2021 Vol. 41, No. 6

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Article navigation > Marine Geology & Quaternary Geology > 2021 > 41(6): 53-66

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YI Zhaohan, HU Rijun, LI Yi, CHEN Xiaoci, CHEN Juanjuan, MENG Lingpeng, ZHU Longhai, ZHANG Xiaodong. Characteristics and controlling factors of suspended sediment transportation in summer spring tide in Funing Bay[J]. Marine Geology & Quaternary Geology, 2021, 41(6): 53-66. doi: 10.16562/j.cnki.0256-1492.2021040401

Citation:

YI Zhaohan, HU Rijun, LI Yi, CHEN Xiaoci, CHEN Juanjuan, MENG Lingpeng, ZHU Longhai, ZHANG Xiaodong. Characteristics and controlling factors of suspended sediment transportation in summer spring tide in Funing Bay[J]. Marine Geology & Quaternary Geology, 2021, 41(6): 53-66. doi: 10.16562/j.cnki.0256-1492.2021040401

Characteristics and controlling factors of suspended sediment transportation in summer spring tide in Funing Bay

1.
College of Marine Geosciences, Ocean University of China, Qingdao 266100, China
2.
Key Lab of Submarine Geosciences and Prospecting Techniques, Ministry of Education, Ocean University of China, Qingdao 266100, China
3.
Huaneng Xiapu Nuclear Power Co., Ltd., Ningde 352000, China
4.
School of Ocean and Earth Science, Tongji University, Shanghai 200082, China

More Information

Corresponding author: HU Rijun, hrj@ouc.edu.cn

Received Date: 01 April 2021

Revised Date: 07 June 2021

Publish Date: 28 December 2021

Abstract

Abstract

Using the measured hydrological and sediment data in the summer Funing Bay, the variation characteristics of suspended sediment concentrations are analyzed, the transport mechanism of suspended sediment studied, and the controlling factors of suspended sediment transportation discussed in this paper. The results show that the suspended sediment concentration decreases from the inside to the outside of the bay in plane view. Vertically, the average sediment concentration of each station decreases from the bottom layer to the surface layer. Suspended sediment is transported landward within the bay, and moves southwestward in the mouth and outside the bay, and advection transport dominates the transport of suspended sediment. Under normal weather, the net transport direction of suspended sediment in the study area in summer is basically consistent with the residual flow direction. Under the southwest strong wind weather, however, the concentration of suspended sediment in the study area increases, and the transport direction turns to northeast. The Min-Zhe coastal current is weak in summer and has little effect on the transportation of suspended sediment in the study area.
- suspended sediment /
- change in time and space /
- transport mechanism /
- control factors /
- Funing Bay

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References

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