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The influence of a layer of mud on the train of waves generated by a moving pressure distribution

โœ Scribed by J.-M. Vanden-Broeck; T. Miloh

Publisher
Springer
Year
1996
Tongue
English
Weight
544 KB
Volume
30
Category
Article
ISSN
0022-0833

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โœฆ Synopsis

Two-dimensional free surface flows generated by a moving distribution of pressure are considered. The bottom is assumed to be covered by a thin layer of mud. The mud is modelled as a viscous fluid. The problem is solved numerically by a boundary integral equation method. It is shown that the layer of mud produces a damping of the waves in the far field. Profiles of the free surface and of the surface of the mud are presented.

๐Ÿ“œ SIMILAR VOLUMES

Gravity capillary waves generated by a m
Gravity capillary waves generated by a moving pressure distribution in the presence of constant vorticity and dissipation
โœ Y. Kang; J.-M. Vanden-Broeck ๐Ÿ“‚ Article ๐Ÿ“… 2005 ๐Ÿ› Elsevier Science ๐ŸŒ English โš– 199 KB

Two-dimensional nonlinear free-surface flows due to a pressure distribution moving at a constant velocity at the surface of a fluid of infinite depth are considered. The effects of the gravity and of the surface tension are included in the dynamic boundary condition. The vorticity in the fluid is as