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Response of tidal dynamics to geomorphic evolution and depositional effects in the Huanghe River Delta
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Xuelei Gong1, Hongyu Ji1, Peng Li2, Shenliang Chen1, *
Haiyang Xuebao | 2024, 46(2) : 64 - 78
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Haiyang Xuebao | 2024, 46(2): 64-78
Response of tidal dynamics to geomorphic evolution and depositional effects in the Huanghe River Delta
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Xuelei Gong1, Hongyu Ji1, Peng Li2, Shenliang Chen1, *
Affiliations
  • 1. State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200241, China
  • 2. College of Harbour and Coastal Engineering, Jimei University, Xiamen 361021, China
Published: 2024-02-29 doi: 10.12284/hyxb2024021
Outline
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In recent years, natural processes and human activities have significantly altered the Huanghe River channel and the coastal geomorphic pattern, while the impact of the dramatic geomorphic evolution on the coastal hydrodynamics has not been fully studied. Based on series images captured by the Landsat satellites and bathymetric measurements, this paper analyzed the shorelines and topography changes of the Huanghe River Delta from 1992 to 2020. Several sets of numerical models covering the entire Bohai Sea were established by TELEMAC-2D to investigate the response of tidal dynamics to geomorphic evolution and its depositional effects in the Huanghe River Delta. The results show that the erosion and deposition had significant spatial and temporal heterogeneity, and there were multiple siltation and erosion centers. The erosion center outside the old Qingshuigou Estuary moved 9.6 km to the south during 2000–2020, and the one outside the Diaokou Estuary moved 6.4 km to the east during 1992–2015. The tidal dynamics were dominated by the coastline and terrain changes on the medium and long time scales. The tidal range of the Diaokou estuary decreased, while the old and the new estuary increased. And the tidal range at 5 m depth had a maximum variation of 0.27 m. The K1 tidal amplitude increased significantly, while the M2 tidal amplitude was considerably reduced, and the amphidromic point near Dongying port eastward migration of 3.8 km. The high velocity outside the Diaokou Estuary and the old estuary continued to weaken, and another high velocity area gradually developed outside the current estuary. The continuous and stable high velocity area caused the erosion of the subaqueous delta and the coarsening of sediment.

the Huanghe River Delta  /  numerical simulation  /  geomorphic evolution  /  tidal dynamics  /  depositional effects
Xuelei Gong, Hongyu Ji, Peng Li, Shenliang Chen. Response of tidal dynamics to geomorphic evolution and depositional effects in the Huanghe River Delta[J]. Haiyang Xuebao, 2024 , 46 (2) : 64 -78 . DOI: 10.12284/hyxb2024021
Year 2024 volume 46 Issue 2
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Article Info
doi: 10.12284/hyxb2024021
  • Receive Date:2023-11-13
  • Online Date:2025-11-25
  • Published:2024-02-29
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History
  • Received:2023-11-13
  • Revised:2024-01-13
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Affiliations
    1. State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200241, China
    2. College of Harbour and Coastal Engineering, Jimei University, Xiamen 361021, China
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表12种不同金属材料的力学参数

Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)

Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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