Numerical simulation on the process of saltwater intrusion and its impact on the suspended sediment concentration in the Changjiang (Yangtze) estuary
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Numerical simulation on the process of saltwater intrusion and its impact on the suspended sediment concentration in the Changjiang (Yangtze) estuary
Numerical simulation on the process of saltwater intrusion and its impact on the suspended sediment concentration in the Changjiang (Yangtze) estuary
海洋湖沼学报(英文)2010年28卷第3期 页码:609-619
Affiliations:
1. Institute of Oceanology Chinese Academy of Sciences
2. Shanghai Institute of Waterways
3. Graduate School of Chinese Academy of Sciences
Author bio:
Funds:
Supported by the National Natural Science Foundation of China (No. 40406025), the National High Technology Research and Development Program of China (863 Program) (No. 2006AA09Z157)
Numerical simulation on the process of saltwater intrusion and its impact on the suspended sediment concentration in the Changjiang (Yangtze) estuary[J]. 海洋湖沼学报(英文), 2010,28(3):609-619.
Pang, C., Zhao, E. & Yang, Y. Numerical simulation on the process of saltwater intrusion and its impact on the suspended sediment concentration in the Changjiang (Yangtze) estuary., Chin. J. Ocean. Limnol. 28, 609–619 (2010). https://doi.org/10.1007/s00343-010-9254-4
Numerical simulation on the process of saltwater intrusion and its impact on the suspended sediment concentration in the Changjiang (Yangtze) estuary[J]. 海洋湖沼学报(英文), 2010,28(3):609-619. DOI: 10.1007/s00343-010-9254-4.
Pang, C., Zhao, E. & Yang, Y. Numerical simulation on the process of saltwater intrusion and its impact on the suspended sediment concentration in the Changjiang (Yangtze) estuary., Chin. J. Ocean. Limnol. 28, 609–619 (2010). https://doi.org/10.1007/s00343-010-9254-4DOI:
Numerical simulation on the process of saltwater intrusion and its impact on the suspended sediment concentration in the Changjiang (Yangtze) estuary
摘要
Abstract
To study the relationship between sediment transportation and saltwater intrusion in the Changjiang (Yangtze) estuary
a three-dimensional numerical model for temperature
salinity
velocity field
and suspended sediment concentration was established based on the ECOMSED model. Using this model
sediment transportation in the flood season of 2005 was simulated for the Changjiang estuary. A comparison between simulated results and observation data for the tidal level
flow velocity and direction
salinity and suspended sediment concentration indicated that they were consistent in overall. Based on model verification
the simulation of saltwater intrusion and its effect on sediment in the Changjiang estuary was analyzed in detail. The saltwater intrusion in the estuary including the formation
evolution
and disappearance of saltwater wedge and the induced vertical circulation were reproduced
and the crucial impact of the wedge on cohesive and non-cohesive suspended sediment distribution and transportation were successfully simulated. The result shows that near the salinity front
the simulated concentrations of both cohesive and non-cohesive suspended sediment at the surface layer had a strong relationship with the simulated velocity
especially when considering a 1-hour lag. However
in the bottom layer
there was no obvious correlation between them
because the saltwater wedge and its inducing vertical circulation may have resuspended loose sediment on the bed
thus forming a high-concentration area near the bottom even if the velocity near the bottom was very low during the transition phase from flood to ebb.
关键词
Keywords
references
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