Author(s): L. H. Huang
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Keywords: No Keywords
Abstract: A finite thickness porous wavemaker is located in an infinite one dimensional water channel as shown in Fig. 1. The vertical wavemaker performs a small amplitude oscillation along the channel. Linear water waves are generated in the channel, while the equations derived from the simplified Biot's theory of poroelasticity are used within the porous wavemaker. Regular perturbation expansions, with a small parameter R, are applied. The flow-efficiency parameter, R, represents the easiness of water flow relative to the skeleton inside the porous wavemaker, and it is usually very small. The larger R is, the greater inertial reaction and the less viscous damping will be. The increase of inertial reaction is greater than the decrease of viscous damping as R increases. It is also found that the thickness of the porous wavemaker is a significant factor to the hydrodynamic pressure on the porous wavemaker when the thickness is small, but it is not a significant factor to wave profile.
Year: 1989