Abstract
Time-harmonic surface waves in a half-space (x 3 ≥ 0) and plate waves in a layer (-h ≤ x 3 ≤ h) of a homogeneous transversely isotropic linearly elastic solid, where the x 1 x 2 -plane is the plane of transverse isotropy, have been reconsidered. The displacement components are expressed in terms of a carrier wave which defines the propagation in the x 1 x 2 -plane, and which supports the sub-surface motion in the half-space and the thickness motion of the plate. The carrier wave can be any solution of the reduced wave equation for a membrane.
Original language | English (US) |
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Pages (from-to) | 89-97 |
Number of pages | 9 |
Journal | Wave Motion |
Volume | 28 |
Issue number | 1 |
DOIs | |
State | Published - Jul 1998 |
ASJC Scopus subject areas
- Modeling and Simulation
- Physics and Astronomy(all)
- Computational Mathematics
- Applied Mathematics