Abstract
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.
| Original language | English |
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| Pages (from-to) | 387-400 |
| Number of pages | 14 |
| Journal | Journal of Engineering Mathematics |
| Volume | 30 |
| Issue number | 3 |
| DOIs | |
| State | Published - 1996 |