会议专题

The Change Analyses of Seabed-clay Eroding-silting in the Yellow River Estuary after Flowing by Qingshuigou Course Since 1996

It has been ten years since the Yellow River changed its riverway from Diaokou Course to Qingshuigou Course in 1996. At Q-8 estuary, seabed landform has been remodeled largely as a result of seabed-sediment which come from the Yellow River depositing and fusing continuously. By dint of the analyses of the softwares (for example AutoCad, Surfer, etc.), the range of sediment depositing and the status of sediment eroding-depositing in different sections have been obtained.

seabed-sediment section surfer eroding-depositing

Yang Xiaoyang Guo Huimin Huang Jianjie He Min

Yellow River Estuary Research Institute, YRCC, Dongying, Shandong 257091 Investigation & Study Department of Dongying Municipal Government, Dongying, Shandong 257091

国际会议

第三届黄河国际论坛(The 3rd International Yellow River Forum on Sustainable Water Resources Management and Delta Ecosystem Maintenance)

山东东营

英文

359-365

2007-10-16(万方平台首次上网日期,不代表论文的发表时间)