Abstract
The Jiao (Ling) River is a typical mountainous macrotidal river. The tidal current and runoff jointly guide sediment gathering in a specific section to form the turbidity maximum zone and develop fluid mud. This plays an important role in riverbed evolution. The construction of sluice in the mainstream of the Jiang (Ling) River will greatly change the original flow and sediment movement characteristics of the river channel, forming siltation downstream sluice and producing a big influence on flood control and drainage and navigation. The flow and sediment movement characteristics of Jiang (Ling) River are analyzed and the influence of fine-grained cohesive sediment movement characteristics and salinity considered. A flow and sediment mathematical model for sluice construction in the Jiang (Ling) River is established to simulate the hydrodynamic change and the temporal and spatial distribution characteristics of sedimentation after the sluice construction. The research results show that the sluice construction has an influence on the entire channel downstream sluice. The closer to the sluice site, the bigger the influence will be. At the initial stage of sluice construction, sediment is mainly deposited in a deep trench of 10 km downstream sluice. The siltation downstream sluice will elevate the flood level and low water level, thus affecting flood control and drainage. It will also decrease the water depth of the channel, thus reducing the navigation capacity of the Jiao (Ling) River. The research results have improved the simulation accuracy of sediment transport mathematical model in the estuary with sluice constructed and provided reference for similar sluice construction in estuaries.
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References
Guo, L., & Chen, Z.-H. (2007). Remote sensing research on the distributed characteristics of suspended matter in Jiaojiang Estuary and Taizhou Gulf. Journal of Wuhan University of Technology, 49–52.
Liu, J., Cheng, H-F, Zhao De-Z., et al. (2013(11)). Spatial and temporal distribution of suspended sediment concentration in the Yangtze estuary 12.5 m deepwater channel. Port & Water Engineering, 49–54.
Sun, P.-F. (2006). Study on 2-D mathematical model of tidal flow and sediment in Jiaojiang Estuary. Hangzhou: Zhejiang University.
Wu, M.-Y., Xu J.-S., & Feng Y.-L. (2011(1)). Spacial-temporal distribution of suspended sediment concentration in Hangzhou Bay. Journal of Sediment Research, 33–37.
Zhao, L.-B., & Zhu Y.-K. (1991(4)). The preliminary analysis on the empirical relation of sediment transport capacity in Jiaojiang River Estuary. Journal of Sediment Research, 69–75.
Tanaka, H., & Sana, A. (1994). Numerical study on transition to turbulence in a wave boundary layer, In Sediment transport mechanism in coastal environments and rivers (pp. 14–25). Singapore: World Scientific.
Acknowledgements
The research work is supported by National Natural Science Foundation No. 51409163 and No. 51479122, National Key R&D Program of China (2017YFC0405402) and the National Natural Science Foundation of China (51479122).
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Zhang, X., Jiao, J., Dou, X., Zhao, X., Xia, W. (2020). Mathematical Model Research of the Siltation Downstream Estuary Floodgate Under the Effect of Float Mud. In: Nguyen, K., Guillou, S., Gourbesville, P., Thiébot, J. (eds) Estuaries and Coastal Zones in Times of Global Change. Springer Water. Springer, Singapore. https://doi.org/10.1007/978-981-15-2081-5_17
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DOI: https://doi.org/10.1007/978-981-15-2081-5_17
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