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• W72155197 abstract "This essay considers the physical phenomena that arise in the interaction of acoustic waves with fluid-loaded elastic (metal) plates (including a loading with different fluids on both sides), or with sediment layers covering the ocean floor. The fluid loading causes the appearance of fluid-borne (Scholte-Stoneley) waves propagating along the plate or layer, in addition to plate-borne, Rayleightype and Lamb-type waves as for the case of the free plate. All such plate wave types, excited acoustically or mechanically, re-radiate into the surrounding fluid in the form of head waves. Observing the latter by experimental methods of visualization, which will be described here, the properties of the plate waves can be obtained in this way. These properties may be understood via the action of multiple internal reflections that may lead to resonances, and it is pointed out that the resonances of submerged objects can be used for solving the inverse problem, i.e., the determination of the properties of a reflecting object from the observed return signal amplitude. This is illustrated here by considering the example of a layered ocean floor." @default.
• W72155197 created "2016-06-24" @default.
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• W72155197 date "2002-01-01" @default.
• W72155197 modified "2023-09-26" @default.
• W72155197 title "Elastic Surface Waves, Resonances, and Inverse Acoustic Scattering" @default.
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• W72155197 doi "https://doi.org/10.1007/978-1-4612-0095-6_1" @default.
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