Abstract

Many maritime structures are made of submerged permeable rubble mound breakwaters. Most numerical models dealing with wave propagation on a porous bed linearize Forchheimer's equation through Lorentz's hypothesis of equivalent work. The friction coefficient f is found by iteration and always averaged on the structure volume. In this paper we write and solve the dispersion relationship for a friction coefficient that is variable on the water depth. It is shown that a constant friction coefficient is only valid for water depth hp and wavelength L with hp/L < 1/10. Above this threshold, the errors on the imaginary part of the wavenumber are not negligible and reach 20% of the peak value. Calculations with constant and depth-dependent friction coefficient produce a different decay of waveheight. Mots cles. Lit poreux, houle, relation de dispersion, bicouche, elements finis.

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