| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 1719835 | Applied Ocean Research | 2016 | 15 Pages |
•3D hydroelastic model for surface gravity wave motion with elastic bottom in finite water depth is presented.•The progressive wave characteristics in flexural mode for various parameters are discussed.•Three-dimensional Green's function and Fourier-type expansion formula are derived.•Forced and free oscillations in a closed and semi-infinite channel are discussed and cut-off frequencies are determined.•Effect of elastic bottom on reflection wave amplitude and wave oscillations are studied.
A general three-dimensional hydroelastic model is developed to study the effect of elastic bottom on surface gravity wave motion in three-dimensions under the action of uniform compressive force based on linearized theory of water wave in finite water depth. The elastic bottom bed is modeled as a thin plate theory. The progressive wave characteristics in different wave modes are analyzed in both the cases of deep and shallow water waves. Further, the linearized long wave equation under shallow water approximation in a direct manner is derived and compared the results obtained based on the small amplitude wave theory. Three-dimensional Green's function associated with surface gravity wave motion with elastic bed is derived using the fundamental source potentials. Fourier-type expansion formula and corresponding orthogonal mode-coupling relations are derived in finite depth and finite/semi-infinite width in three-dimensions. Utilizing the expansion formula, two classical problems (i) forced motion and (ii) wave reflection by a rigid wall in a channel of finite width and finite/semi-infinite length are illustrated which will play significant role in the analysis of wave-structure interaction problems arising in ocean engineering.The effects of elastic bottom on surface gravity waves are analyzed by presenting several numerical results on reflection wave amplitudes in different cases. Further, the behavior of free motions and oscillations in a basin of finite width and finite/semi-infinite length with elastic bed under the action of uniform compressive force are discussed.
