1983
DOI: 10.1007/bf01236352
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Generation of SH-type waves due to non-uniformly moving stress-discontinuity in layered anisotropic elastic half-space

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Cited by 5 publications
(6 citation statements)
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“…For the above reasons, the stress discontinuity may be treated as a moving source either with uniform velocity or with non-uniform velocity. Relating to stress discontinuity, Pal (1983) has considered the problem of generation of SH-type waves due to non-uniformly moving stress discontinuity in a layered anisotropic elastic half-space. It is our intention in the present paper, to investigate the disturbance of SH-type waves at the free surface of a anisotropic soil layer due to an impulsive stress discontinuity moving with nonuniform velocity along the interface of isotropic homogeneous and inhomogeneous medium.…”
Section: Mandal Et Almentioning
confidence: 99%
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“…For the above reasons, the stress discontinuity may be treated as a moving source either with uniform velocity or with non-uniform velocity. Relating to stress discontinuity, Pal (1983) has considered the problem of generation of SH-type waves due to non-uniformly moving stress discontinuity in a layered anisotropic elastic half-space. It is our intention in the present paper, to investigate the disturbance of SH-type waves at the free surface of a anisotropic soil layer due to an impulsive stress discontinuity moving with nonuniform velocity along the interface of isotropic homogeneous and inhomogeneous medium.…”
Section: Mandal Et Almentioning
confidence: 99%
“…The problem can readily be solved by using the Laplace and Fourier transforms combined with the modified Cagniard-de Hoop (1960) technique and used by Pal (1983). The Laplace transform of a function v(x, z, t) with respect to t will be defined by…”
Section: Solution Of Problemmentioning
confidence: 99%
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“…In addition to initial stress, shearing stress discontinuity also plays a vital role in the study of seismic wave propagation. Pal [1983] considered the problem of generation and propagation of SH-type waves due to non-uniformly moving stress discontinuity in layered anisotropic elastic half-space using Garvin's [1956] techniques, which are a modification of Cagniard's [1939] technique. Pal and Kumar [2000] considered the generation of SH waves by a moving stress discontinuity in an anisotropic soil layer over an elastic half-space using the Cagniard-de Hoop special reduction technique [de Hoop 1960].…”
Section: Introductionmentioning
confidence: 99%
“…In addition to initial stress, shearing stress discontinuity also plays a vital role in the study of seismic wave propagation. Pal [1983] considered the problem of generation and propagation of SH-type waves due to non-uniformly moving stress Communicated by Holm Altenbach. MSC2010: 35L05, 74J15.…”
Section: Introductionmentioning
confidence: 99%