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Numerical study on wave propagation over a fluid-mud layer with different bottom conditions

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Abstract

Wave decay over a muddy seabed has been widely reported. In previous studies, the fluid-mud layer is usually treated as a homogeneous layer with a certain thickness lying on the rigid bottom. However, the muddy seabed beneath a fluid-mud layer is usually movable in practice. This study aims to find out the influence of the movable seabed beneath a fluid-mud layer. For this purpose, a numerical model for wave propagation over a multilayered muddy seabed is developed, in which water is treated as a Newtonian fluid, and the rheology of mud is described by a visco-elastic–plastic model. The laboratory experiments of Sakakiyama and Bijker (J Waterw Port Coast Ocean Eng 115(5):614–633, 1989) are chosen to validate the numerical model. The model is then employed to investigate the movement of a fluid-mud layer with different conditions of the underlying mud layer and its influence on wave decay. It is found that the underlying mud layer plays a very important role in the wave–mud interaction and greatly affects the wave decay rate.

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Acknowledgments

The authors would like to acknowledge the support by the National Natural Science Foundation of China under the grant No. 51109119 and the Specialized Research Fund for the Doctoral Program of Higher Education of China under the grant No. 20110002120019.

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Correspondence to Xiaojing Niu.

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Responsible Editor: Qing He

This article is part of the Topical Collection on the 11th International Conference on Cohesive Sediment Transport

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Niu, X., Yu, X. Numerical study on wave propagation over a fluid-mud layer with different bottom conditions. Ocean Dynamics 64, 293–300 (2014). https://doi.org/10.1007/s10236-013-0686-1

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  • DOI: https://doi.org/10.1007/s10236-013-0686-1

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