Abstract
The Qiantang Estuary is characterized by strong tidal bore, high sediment concentration, severe erosion/deposition and frequent human activities. The law of saltwater intrusion is different from other general tidal estuary. This chapter reveals the law of interaction among runoff, channel volume and salinity by means of the analysis of the long-term hydrological and measured salinity data of the Qiantang Estuary. Based on the concept of water, sand and salt mixture density, the muddy water control equations have been derived, and the mathematical model coupling with strong tidal bore-sediment-salinity has been developed as a result, and the model has also been verified, which shows that the result adopting movable-bed numerical simulation model in calculation agrees more with the actual condition.
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References
Bao, Y., Liu, J. B., Ren, J., et al. (2009). Research of law and dynamic mechanism for strong saline water intrusion in Modaomen waterway. China Science G, 39(10), 1527–1534.
Cun-hong, P., & Kun, X. (2006). Kinetic flux vector splitting scheme for solving 2-D shallow water equations with triangular mesh. Chinese Journal of Hydraulic Engineering, 37(7), 858–864.
Han, Z. C., Cheng, H. P., & Shi, Y. B. (2012). Long term forecast of salt water intrusion at the Qiantang Estuary. Chinese Journal of Hydraulic Engineering, 43(2), 232–240.
Han, Z. C., Dai, Z. H., & Li, G. B. (2003). Management and development of Qiantang Estuary. Beijing: China Water Resources and Hydropower Press.
Han, Z. C., Pan, C. H., & Shi, Y. B. (2002). Effects of human activities on saltwater intrusion in estuaries. Advances of Water Science, 13(3), 333–339.
MacCormack, R. W., Paullay, A. (1972). Computational efficiency achieved by time split ting of finite difference operators. AIAA Paper, 72–154.
Mao, H. L. (1964). Preliminary study on mixed tide of Hangzhou Bay. Oceanology ET Limnologia Sinica, 6(2).
Pan, C. H., Zhang, S. Y., Shi, Y. B., et al. (2014). Study on saltwater intrusion in Qiantang Estuary affected by tidal bore. Chinese Journal of Hydraulic Engineering, 45(11), 1301–1308.
Savenije, H. H. G. (2005). Salinity and tides in alluvial estuaries. Amsterdam: Elsevier Press.
Shen, F., Mao, Z., & Zhu, J. (2003). The saltwater intrusion of the Changjiang Estuary. Beijing: The Ocean Publish.
Shi, Y. B., Li, R. H., & Yao, G. H. (2015). 1D Movable bed numerical forecast model of salinity of the Qiantang Estuarine reach and its application. Advances of Water Science (chinese), 26(2), 212–220.
Shi, Y. B., Pan, C. H., Cheng, W. L., et al. (2012). Temporal spatial variation and numerical forecast model of salt water intrusion of the Qiantang Estuarine reach. Advances in Water Science (Chinese), 23(3), 419–428.
Smagorinsky, J. (1963). General circulation experiment with the primitive equations. Monthly Weather Review, 91(3), 99–164.
van Rijn, L. C., Walstra, D. J. R., Grasmeijer, B., et al. (2003). The predictability of cross-shore bed evolution of sandy beaches at the time scale of storms and season using process-based profile models. Coastal Engineering, 47, 295–327.
Acknowledgements
The research reported in this chapter was supported by the special Project of Zhejiang Province Scientific Research Institute (No. 2016F50018).
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Shi, Yb., Cheng, Wl. (2020). Law of Salt Tide Intrusion of the Qiantang Estuary and Its Numerical Simulation. 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_5
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