| Li Bogen,Yang Zhaoqing,Xie Qinchun.Suspended sediment transport of the Hangzhou Bay and its related hydrodynamic analyses[J].Acta Oceanologica Sinica,1993,(1):39-50 |
| Suspended sediment transport of the Hangzhou Bay and its related hydrodynamic analyses |
| Suspended sediment transport of the Hangzhou Bay and its related hydrodynamic analyses |
| 投稿时间：1992-02-23 修订日期：1992-06-01 |
| DOI： |
| 中文关键词: |
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| 基金项目:This project is supported by National Natural Science Foundation of China and the Zhejiang Provincial Natural Science Foundation. |
| 作者 | 单位 | | Li Bogen | Second Institute of Oceanography, State Oceanic Administration, P. O. Box 1207, Hangzhou 310012, China | | Yang Zhaoqing | Second Institute of Oceanography, State Oceanic Administration, P. O. Box 1207, Hangzhou 310012, China | | Xie Qinchun | Second Institute of Oceanography, State Oceanic Administration, P. O. Box 1207, Hangzhou 310012, China |
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| 中文摘要: |
| The 25-h measurements of current speed, flow direction, water depth, suspended sediment concentration and salinity were carried out at six anchored stations in the study area during spring and neap tides in winter of 1987 and summer of 1989. Caculations and analyses of the data obtained show that large amounts of suspended sediments are moved back and forth under the action of tidal current, and the net transport of sediment is small, with its predominance upstream in winter and downstream in summer. These calculations and analyses also suggest that the advective transport of sediment is dominant, while the vertical gravitational circulation of the suspended sediment comes next. Meantime, it is indicated that tidal currents play a major role in the suspended sediment transport, and residual flows have effect on the net transport of the suspended sediment, which is more remarkable during neap tide than during spring tide. |
| 英文摘要: |
| The 25-h measurements of current speed, flow direction, water depth, suspended sediment concentration and salinity were carried out at six anchored stations in the study area during spring and neap tides in winter of 1987 and summer of 1989. Caculations and analyses of the data obtained show that large amounts of suspended sediments are moved back and forth under the action of tidal current, and the net transport of sediment is small, with its predominance upstream in winter and downstream in summer. These calculations and analyses also suggest that the advective transport of sediment is dominant, while the vertical gravitational circulation of the suspended sediment comes next. Meantime, it is indicated that tidal currents play a major role in the suspended sediment transport, and residual flows have effect on the net transport of the suspended sediment, which is more remarkable during neap tide than during spring tide. |
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