scholarly journals Hybrid of surface shear waves at the contact interface between piezoelectric and electrically conductive half-spaces

2021 ◽  
Vol 74 (3) ◽  
pp. 53-61
Author(s):  
A.S. Avetisyan ◽  
A.V. Gevorgyan ◽  
L.V. Avetisyan
Keyword(s):  
Shear Waves ◽  
Contact Interface ◽  
Surface Shear ◽  
Electrically Conductive

Magnetoelastic surface shear waves in a regularly layered medium

1987 ◽  
Vol 23 (3) ◽  
pp. 207-211
Author(s):  
V. V. Levchenko ◽  
N. A. Shul'ga
Keyword(s):  
Layered Medium ◽  
Shear Waves ◽  
Surface Shear ◽  
Magnetoelastic Surface

Closure to “Surface Shear Waves”

1976 ◽  
Vol 102 (3) ◽  
pp. 413-414
Author(s):  
D. Howell Peregrine
Keyword(s):  
Shear Waves ◽  
Surface Shear

The propagation of surface shear waves

1979 ◽  
Vol 70 (2) ◽  
pp. 375-382 ◽  
Author(s):  
J.A de Feijter ◽  
J Benjamins
Keyword(s):  
Shear Waves ◽  
Surface Shear

Discussion of “Surface Shear Waves”

1975 ◽  
Vol 101 (7) ◽  
pp. 1032-1034
Author(s):  
Edward H. Wilson
Keyword(s):  
Shear Waves ◽  
Surface Shear

Surface Shear Waves

1974 ◽  
Vol 100 (9) ◽  
pp. 1215-1227
Author(s):  
D. Howell Peregrine
Keyword(s):  
Shear Waves ◽  
Surface Shear

scholarly journals Surface Shear Waves in a Half-Plane with Depth-Variant Structure

2019 ◽  
Vol 184 (1) ◽  
pp. 21-42 ◽  
Author(s):  
Andrey Sarychev ◽  
Alexander Shuvalov ◽  
Marco Spadini
Keyword(s):  
Half Plane ◽  
Shear Waves ◽  
Surface Shear ◽  
Variant Structure

scholarly journals Analysis of Phase Velocity of Love Waves in Rigid and Soft Mountain Surfaces: Exponential Law Model

Complexity ◽  
2021 ◽  
Vol 2021 ◽  
pp. 1-12
Author(s):  
Uma Bharti ◽  
Pramod Kumar Vaishnav ◽  
S.M. Abo-Dahab ◽  
Jamel Bouslimi ◽  
K.H. Mahmoud
Keyword(s):  
Phase Velocity ◽  
Saturated Porous Medium ◽  
Shear Waves ◽  
Superficial Layer ◽  
Contact Interface ◽  
Rigid Model ◽  
Fluid Saturated Porous Medium ◽  
Cartesian Coordinate ◽  
The Time Domain ◽  
Energy Equations

Irregularity may occur on the earth’s surface in the form of mountains due to the imperfection of the earth’s crust. To explore the influence of horizontally polarized shear waves on mountains, we considered the fluid-saturated porous medium (superficial layer) over an orthotropic semi-infinite medium with rigid (Model-I) and soft (Model-II) mountain surfaces for wave propagation. The mountain surface is defined mathematically as a periodic function of the time domain. The physical interpretation of materials’ structure has been explained in rectangular Cartesian coordinate system originated at the contact interface of layer and half-space. The displacement of the mountains has been derived by solving energy equations analytically. The influence of rigid and soft mountain surfaces on the phase velocity of shear waves has been demonstrated graphically (we used MATLAB software for graphical representations).

The existence of surface shear waves in a finitely conducting magneto-elastic half-space

1999 ◽  
Vol 10 (5) ◽  
pp. 381-389
Author(s):  
Manidipa Chattopadhyay ◽  
S.K. Chakraborty ◽  
Sarbani Chakraborty
Keyword(s):  
Half Space ◽  
Shear Waves ◽  
Elastic Half Space ◽  
Surface Shear
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