Application of a 'Radiation-type' boundary condition to the wave, porous bed problem.

The problem of a small-amplitude wave propagating over a flat porous bed is reanalyzed subject to a bottom boundary condition which is of the form of a 'radiation-type' condition commonly encountered in heat conduction problems. The important physical quantities (velocity, velocity potential, streamfunction, shear stress and energy dissipation) have been derived and are presented, subject to natural condition. The bottom boundary layer is represented by the linearized Navier-Stokes equations under the usual boundary layer approximation. It is found that the boundary layer velocity distribution and shear stress can be greatly altered from impermeable bed predictions. Theoretical results for energy dissipation and shear stress are compared to existing data and are found to agree very well. The predictions of classical small-amplitude wave theory are not appreciably modified away from the boundary. (A)