2014
DOI: 10.1016/j.ultras.2014.02.022
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Scholte–Stoneley waves on an immersed solid dihedral: Generation, propagation and scattering effects

Abstract: Scholte-Stoneley wave propagation on a dihedral and more precisely the diffraction effects occurring at the corners, has since long been of high importance for nondestructive testing of materials and structures. Experimental investigations have been reported in the past. Simulations based on radiation mode theory have been published before, explaining the only situation for which the model is applicable namely rectangular corners. The current report describes an investigation applying finite element simulation… Show more

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Cited by 3 publications
(2 citation statements)
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“…VLF acoustic signals with strong penetrating power penetrate the sea bottom when propagating in the shallow sea. Thus, VLF acoustic energy leaks into the sea bottom and excites other sound field components that can propagate through the sea bottom or liquid-solid interface [10][11][12][13]. These components-such as the compression wave (Pwaves), the shear wave (S-waves), the normal mode waves, and the interface waves-are all important for understanding the conversion mechanism and spatial and temporal distribution of low-frequency sound waves [13][14][15][16].…”
Section: Introductionmentioning
confidence: 99%
See 1 more Smart Citation
“…VLF acoustic signals with strong penetrating power penetrate the sea bottom when propagating in the shallow sea. Thus, VLF acoustic energy leaks into the sea bottom and excites other sound field components that can propagate through the sea bottom or liquid-solid interface [10][11][12][13]. These components-such as the compression wave (Pwaves), the shear wave (S-waves), the normal mode waves, and the interface waves-are all important for understanding the conversion mechanism and spatial and temporal distribution of low-frequency sound waves [13][14][15][16].…”
Section: Introductionmentioning
confidence: 99%
“…Thus, VLF acoustic energy leaks into the sea bottom and excites other sound field components that can propagate through the sea bottom or liquid-solid interface [10][11][12][13]. These components-such as the compression wave (Pwaves), the shear wave (S-waves), the normal mode waves, and the interface waves-are all important for understanding the conversion mechanism and spatial and temporal distribution of low-frequency sound waves [13][14][15][16]. The systematic study of excitation, propagation, and detection of different components of low-frequency sound fields has essential application value in ocean acoustics and geophysics.…”
Section: Introductionmentioning
confidence: 99%