| NUMERICAL MODELING OF THE SEABED MORPHOLOGY OF THE SUBAQUEOUS YELLOW RIVER DELTA |
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| 引用本文： | WANG Hou-jie1,YANG Zuo-sheng1,LI Rui-jie2,ZHANG Jun1,and CHANG Rui-fang1 1 Estuarine & Coastal Studies,Ocean University of Qingdao,Qingdao 266003,China 2 Traffic and Ocean Engineering College,Hohai University,Nanjing 210098,China corresponding. NUMERICAL MODELING OF THE SEABED MORPHOLOGY OF THE SUBAQUEOUS YELLOW RIVER DELTA[J]. 国际泥沙研究, 2001, 16(4) |
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| 作者姓名： | WANG Hou-jie1 YANG Zuo-sheng1 LI Rui-jie2 ZHANG Jun1 and CHANG Rui-fang1 1 Estuarine & Coastal Studies Ocean University of Qingdao Qingdao 266003 China 2 Traffic and Ocean Engineering College Hohai University Nanjing 210098 China corresponding |
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| 作者单位： | WANG Hou-jie1，YANG Zuo-sheng1，LI Rui-jie2，ZHANG Jun1，and CHANG Rui-fang1 1 Estuarine & Coastal Studies，Ocean University of Qingdao，Qingdao 266003，China 2 Traffic and Ocean Engineering College，Hohai University，Nanjing 210098，China corresponding |
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| 基金项目： | the 95 State Key Proect of China (Project No.96-922-03-02-02). |
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| 摘 要： | 1 wrsoorCnoxThe Yenow mver delta is ereated by the river transponing sediment bom the Loess Plateau to the shallOWBOhai Gulf during the paSt l45 years. lh recent years, the water discharge and sediment load enedg thesea have bein ched dramacaily The river end chann shital northeastWed hom QingshulgOuN to qngshulgou-Chah chaDnel in 1996, resulting in a new regfor of sedimenboon and erosion ofthe subaqucous delta.,A nUInerial model for river sediInen dispersion and seabed mOrPhofogy of t…
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NUMERICAL MODELING OF THE SEABED MORPHOLOGY OF THE SUBAQUEOUS YELLOW RIVER DELTA |
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| WANG Houjie,Yang Zuosheng,LI Rui-jie,ZHANG Jun,CHANG Ruifang. NUMERICAL MODELING OF THE SEABED MORPHOLOGY OF THE SUBAQUEOUS YELLOW RIVER DELTA[J]. International Journal of Sediment Research, 2001, 16(4) |
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| Authors: | WANG Houjie Yang Zuosheng LI Rui-jie ZHANG Jun CHANG Ruifang |
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| Abstract: | A horizontal 2-D model is employed to study the sediment dispersion and seabed morphology of the subaqueous Yellow River delta under the joint effect of tide, wind and river flow. The ending reach of the Yellow River channel was shifted from the Qingshuigou channel to the Qingshuigou-Chahe channel in 1996. The model is calibrated with the hydrographic, topographic and sediment data collected in 1998. Sediment deposits around the present river mouth, forming a lunate submerged nearshore ridge. The silty spit at the former river mouth is being eroded. The model is validated in tendency and magnitude of the seabed morphology from 1998 to 1999. It is used to predict the seabed morphology of the subaqueous delta under the action of estuarine hydrodynamics. |
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| Keywords: | Subaqueous Yellow River delta Hydrodynamics Numerical model Suspended sediment Seabed morphology |
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