scholarly journals Effect of a viscous liquid loading on Love wave propagation

2012 ◽  
Vol 49 (17) ◽  
pp. 2314-2319 ◽  
Author(s):  
P. Kiełczyński ◽  
M. Szalewski ◽  
A. Balcerzak
1999 ◽  
Vol 07 (01) ◽  
pp. 59-70 ◽  
Author(s):  
VICTOR V. KRYLOV

The theory of antisymmetric localized elastic modes propagating along edges of immersed wedge-like structures is developed using the geometrical-acoustics approach to the description of flexural waves in elastic plates of variable thickness. The velocities of these modes, often called wedge acoustic waves, are calculated using solutions of the dispersion equation of the Bohr-Sommerfeld type following from the geometrical-acoustics description of localized wedge modes. In a subsonic regime of wave propagation, i.e. for wedge modes slower than sound in liquid, the influence of liquid loading results in significant decrease of wedge wave velocities in comparison with their values in vacuum. This decrease is a nonlinear function of a wedge apex angle θ and is more pronounced for small values of θ. In a supersonic regime of wedge wave propagation, a smaller decrease in velocities takes place and the waves travel with the attenuation due to radiation of sound into the surrounding liquid. The comparison is given with the recent experimental investigations of wedge waves carried out by independent researchers.


2003 ◽  
Vol 2003 (0) ◽  
pp. 49
Author(s):  
Hiroaki YAMAMOTO ◽  
Tsuyoshi YASHIMA ◽  
Tsutomu SAITO ◽  
Kazuyoshi TAKAYAMA

Geophysics ◽  
1983 ◽  
Vol 48 (7) ◽  
pp. 833-853 ◽  
Author(s):  
K. R. Kelly

Love wave propagation is studied by investigating numerical modeling results for several examples of geologic interest. The modal characteristics of the results are clarified by the use of narrow band‐pass filters and two‐dimensional Fourier transforms in range and time. Such processing makes it possible to study changes in phase and group velocity for the various modes and to locate points of reflection. This permits one to gain insight into changes in the physical properties of the surface channel supporting the waves.


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