Local Erosion–Deposition Changes and Their Relationships with the Hydro-Sedimentary Environment in the Nearshore Radial Sand-Ridge Area off Dongtai, Northern Jiangsu

The radial sand-ridge field off the Jiangsu coast is a distinctive landform in a strongly tide-dominated environment, where sediment supply and geomorphic patterns have been profoundly altered by Yellow River course changes, reduced Yangtze-derived sediment, and large-scale reclamation. Focusing on a typical nearshore sector off Dongtai, this study integrates multi-source data from 1979 to 2025, including historical nautical charts, high-precision engineering bathymetry, full-tide hydro-sediment observations, and surficial sediment samples, to quantify seabed erosion–deposition over 46 years and clarify linkages among tidal currents, suspended-sediment transport, and surface grain-size patterns. Surficial sediments from Maozhusha to Jiangjiasha channel systematically fine from north to south: sand-ridge crests are dominated by sandy silt, whereas tidal channels and transition zones are characterized by silty sand and clayey silt. From 1979 to 2025, Zhugensha and its outer flank underwent multi-meter accretion and a marked accretion belt formed between Gaoni and Tiaozini, while the Jiangjiasha channel and adjacent deep troughs experienced persistent scour (local mean rates up to ~0.25 m/a), forming a striped “ridge accretion–trough erosion” pattern. Residual and potential maximum currents in the main channels enhance scour and offshore export of fines, whereas relatively strong depth-averaged flow and near-bed shear on inner sand-ridge flanks favor frequent mobilization and short-range trapping of coarser particles. Suspended-sediment concentration and median grain size are generally positively correlated, with suspension coarsening in high-energy channels but dominated by fine grains on nearshore flats and in deep troughs. These findings refine understanding of muddy-coast geomorphology under strong tides and may inform offshore wind-farm foundation design, navigation-channel maintenance, and coastal-zone management.

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Journal
Journal of Marine Science and Engineering
Published
2026-01-20
DOI
https://doi.org/10.3390/jmse14020205
Primary Topic
Geological formations and processes
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article
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article

Local Erosion–Deposition Changes and Their Relationships with the Hydro-Sedimentary Environment in the Nearshore Radial Sand-Ridge Area off Dongtai, Northern Jiangsu

Yanxia Liu, Nan Zhuang, Xiaohui Wang, Jiyang Jiang et al.
Journal of Marine Science and Engineering
Geological formations and processes
article

Local Erosion–Deposition Changes and Their Relationships with the Hydro-Sedimentary Environment in the Nearshore Radial Sand-Ridge Area off Dongtai, Northern Jiangsu

Yanxia Liu, Nan Zhuang, Xiaohui Wang, Jiyang Jiang, Jingyuan Cao, Liwen Yan
article en

Abstract

The radial sand-ridge field off the Jiangsu coast is a distinctive landform in a strongly tide-dominated environment, where sediment supply and geomorphic patterns have been profoundly altered by Yellow River course changes, reduced Yangtze-derived sediment, and large-scale reclamation. Focusing on a typical nearshore sector off Dongtai, this study integrates multi-source data from 1979 to 2025, including historical nautical charts, high-precision engineering bathymetry, full-tide hydro-sediment observations, and surficial sediment samples, to quantify seabed erosion–deposition over 46 years and clarify linkages among tidal currents, suspended-sediment transport, and surface grain-size patterns. Surficial sediments from Maozhusha to Jiangjiasha channel systematically fine from north to south: sand-ridge crests are dominated by sandy silt, whereas tidal channels and transition zones are characterized by silty sand and clayey silt. From 1979 to 2025, Zhugensha and its outer flank underwent multi-meter accretion and a marked accretion belt formed between Gaoni and Tiaozini, while the Jiangjiasha channel and adjacent deep troughs experienced persistent scour (local mean rates up to ~0.25 m/a), forming a striped “ridge accretion–trough erosion” pattern. Residual and potential maximum currents in the main channels enhance scour and offshore export of fines, whereas relatively strong depth-averaged flow and near-bed shear on inner sand-ridge flanks favor frequent mobilization and short-range trapping of coarser particles. Suspended-sediment concentration and median grain size are generally positively correlated, with suspension coarsening in high-energy channels but dominated by fine grains on nearshore flats and in deep troughs. These findings refine understanding of muddy-coast geomorphology under strong tides and may inform offshore wind-farm foundation design, navigation-channel maintenance, and coastal-zone management.

Journal of Marine Science and EngineeringVol. 14(2)
China Electric Equipment Group (China) (CN), Institute of Oceanology (CN), China Design Group (China) (CN), China Power Engineering Consulting Group (China) (CN), University of Chinese Academy of Sciences (CN), Shandong University of Science and Technology (CN)
Life below water
Openalex Percentile: Top 86%
Geological formations and processes
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