| WANG Hong,FAN Wei,YUN Caixing. 2004. Indicators and impact analysis of sediment from the Changjiang Estuary and East China Sea to the Hangzhou Bay. Acta Oceanologica Sinica, (2):297－308 |
| Indicators and impact analysis of sediment from the Changjiang Estuary and East China Sea to the Hangzhou Bay |
| Indicators and impact analysis of sediment from the Changjiang Estuary and East China Sea to the Hangzhou Bay |
| Received:January 03, 2004 Revised:April 02, 2004 |
| DOI： |
| Key words:Changjiang Estuary Hangzhou Bay sediment transport |
| 中文关键词: Changjiang Estuary Hangzhou Bay sediment transport |
| 基金项目: |
|
| Hits: 902 |
| Download times: 633 |
| Abstract: |
| Based on the historical evolution of the Hangzhou Bay, by making use of the conclusions made by the previous research workers and the integration of concrete data, five distinct impact indicators of the sediment from the Changjiang Estuary and the East China Sea to the Hangzhou Bay are summarized. Numerical calculation and analysis indicate that the scouring and deposition of seabed in the Hangzhou Bay are subject to the direct impact of the evolution of the Changjiang Estuary, and the growth and decline and the direction of the sandy bar at Nanhuizui give traces to the sediment transport between the Changjiang Estuary and the Hangzhou Bay. The transport of sediment from the Changjiang Estuary to the Hangzhou Bay occurs mainly in winter and spring seasons and the increase of the Changjiang River runoff and the decrease of sediment charge have caused scouring in the northern coast of the Hangzhou Bay and the seabed erosion along the frontal margin of the Changjiang River Delta. |
| 中文摘要: |
| Based on the historical evolution of the Hangzhou Bay, by making use of the conclusions made by the previous research workers and the integration of concrete data, five distinct impact indicators of the sediment from the Changjiang Estuary and the East China Sea to the Hangzhou Bay are summarized. Numerical calculation and analysis indicate that the scouring and deposition of seabed in the Hangzhou Bay are subject to the direct impact of the evolution of the Changjiang Estuary, and the growth and decline and the direction of the sandy bar at Nanhuizui give traces to the sediment transport between the Changjiang Estuary and the Hangzhou Bay. The transport of sediment from the Changjiang Estuary to the Hangzhou Bay occurs mainly in winter and spring seasons and the increase of the Changjiang River runoff and the decrease of sediment charge have caused scouring in the northern coast of the Hangzhou Bay and the seabed erosion along the frontal margin of the Changjiang River Delta. |
|
HTML
View Full Text
View/Add Comment Download reader |
| Close |
