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KONG Lingshuang,CAO Zude,WANG Wei,QI Dingman.Sediment movement characteristics of coast and analysis of seabed evolution[J].Acta Oceanologica Sinica,2011,(5):101-107
Sediment movement characteristics of coast and analysis of seabed evolution
Sediment movement characteristics of coast and analysis of seabed evolution
投稿时间:2011-01-11  修订日期:2011-06-14
DOI:10.1007/s13131-011-0152-1
中文关键词:  sediment movement  periodic alternating current  sediment numerical simulation  equilibrium sediment concentration  seabed erosion-sedimentation index
英文关键词:sediment movement  periodic alternating current  sediment numerical simulation  equilibrium sediment concentration  seabed erosion-sedimentation index
基金项目:The Public Science and Technology Research Funds Projects of Ocean under contract Nos 200905001 and 201005019; UNESCO-IHE Partnership Research Fund (UPaRF) under contract No. 60038881; the National Natural Science Foundation of China under contract No. 50939003.
作者单位E-mail
KONG Lingshuang Shanghai Estuary and Coastal Science Research Center, Shanghai 201201, China Kong_lsh@sina.com 
CAO Zude Tianjin Research Institute for Water Transport Engineering, Ministry of Transport, Tianjin 300456, China  
WANG Wei Shanghai Estuary and Coastal Science Research Center, Shanghai 201201, China  
QI Dingman Shanghai Estuary and Coastal Science Research Center, Shanghai 201201, China  
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中文摘要:
      The rotary ring flume is used to study the silty sand movement in a periodic alternating current. Characteristics of sediment movement of different coasts in the tidal current are summarized. More detailed analysis of erosion-sedimentation function in a numerical simulation is made. The equilibrium sediment concentration is advanced. Based on the equilibrium sediment concentration, the seabed erosion-sedimentation index is derived and the seabed erosion-sedimentation calculation is analyzed. The seabed erosion-sedimentation index is used to calculate the seabed evolution of Yangshan sea area and a good agreement with field measurements is obtained.
英文摘要:
      The rotary ring flume is used to study the silty sand movement in a periodic alternating current. Characteristics of sediment movement of different coasts in the tidal current are summarized. More detailed analysis of erosion-sedimentation function in a numerical simulation is made. The equilibrium sediment concentration is advanced. Based on the equilibrium sediment concentration, the seabed erosion-sedimentation index is derived and the seabed erosion-sedimentation calculation is analyzed. The seabed erosion-sedimentation index is used to calculate the seabed evolution of Yangshan sea area and a good agreement with field measurements is obtained.
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