1959
DOI: 10.1098/rspa.1959.0221
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Elastic waves in anisotropic media

Abstract: The displacements due to a radiating point source in an infinite anisotropic elastic medium are found in terms of Fourier integrals. The integrals are evaluated asymptotically, yielding explicit expressions for displacements at points far from the source. The relative amplitudes of waves from a point source are thus determined, and it is found that although in general the decay of wave amplitudes is proportional to the distance from the source, it is possible that in certain directions the decay is less than t… Show more

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Cited by 136 publications
(18 citation statements)
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“…For example, along certain directions there are three phase velocities for each mode giving rise to pulses which separate into distinct parts and which decay with distance according to r-5 / 6 for cuspidal edges of the group velocity surface or as r 1/2 along directions corresponding to conical points [6]. Such behaviour has been seen in numerical calculations [7].…”
Section: Discussionmentioning
confidence: 59%
See 1 more Smart Citation
“…For example, along certain directions there are three phase velocities for each mode giving rise to pulses which separate into distinct parts and which decay with distance according to r-5 / 6 for cuspidal edges of the group velocity surface or as r 1/2 along directions corresponding to conical points [6]. Such behaviour has been seen in numerical calculations [7].…”
Section: Discussionmentioning
confidence: 59%
“…(5) (6) These demonstrate that the processing works when the complications of anisotropic materials are absent.…”
Section: A(9tp)mentioning
confidence: 99%
“…Buckwald [83]. The good agreement shows that the axisymmetric finite element algo- The goal of all these techniques is to account for the con straining effect (stiffness) of the missing medium while preventing or minimizing the unwanted reflections at the artificial boundaries.…”
Section: Axisymmetric Formulationmentioning
confidence: 61%
“…This implies that only these two types of ma terials can possibly be modeled in an axisymmetric system. An explanation to this phenomenon is that the shear component (^^ -^^) is independent of the other displacements for isotropic and transversely isotropic materials [83], which is also the reason that the equation of the slowness surface for these two kinds of materials can be factorized. The separated wave front can be described by uq and is neglected in the axisymmetric geometry.…”
Section: Axisymmetric Formulationmentioning
confidence: 99%
“…Therefore, it follows from Eqs. ( 3 ) and ( 6 ) that stresses associated with P and SV waves are Y (7) It has also been shown that an SH wave travelling in a plane containing the zonal axis,z axis, of a transversely isotropic medium possesses a transverse displacement only, t h a t i s , f o r the coordinates i n Assume t h a t an SV wave i s incident on t h e plane boundary, the x-y plane i n Fig. 2 .…”
mentioning
confidence: 99%