1989
DOI: 10.1016/0165-2125(89)90028-0
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Scattering of elastic waves by three-dimensional surface topographies

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Cited by 37 publications
(17 citation statements)
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“…They also state that their presented method also may be extended to consider alluvial valleys. Diffraction of plane harmonic waves by three-dimensional surface irregularities was investigated, by Mossessian and Dravinski [8], with use of the indirect boundary integral method. The irregular shapes are arbitrary and embedded in the half-space.…”
Section: Literature Reviewmentioning
confidence: 99%
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“…They also state that their presented method also may be extended to consider alluvial valleys. Diffraction of plane harmonic waves by three-dimensional surface irregularities was investigated, by Mossessian and Dravinski [8], with use of the indirect boundary integral method. The irregular shapes are arbitrary and embedded in the half-space.…”
Section: Literature Reviewmentioning
confidence: 99%
“…The RMS-value of displacements from a steady-state analysis is determined as (8) where is the RMS-value of displacements, is the magnitude of the frequency dependent displacement and n is the number of frequencies in the interval.…”
Section: Structural Dynamicsmentioning
confidence: 99%
“…Following an indirect boundary integral equation approach (Dravinski and Mossessian, 1987a;Mossessian and Dravinski, 1989) the scattered field is assumed to be generated from distribution of unknown tractions f(y) on an auxiliary surface Sa inside the surface B. Hence the scattered displacement field in the half-space can be written in the form (15) where G is a half-space displacement Green's function tensor (Aki and Richards, 1980).…”
Section: Boundary Integral Equation Analysismentioning
confidence: 99%
“…The element Gij(x, y) corresponds to the i-th component of the displacement vector at x due to a unit harmonic force at y acting in the j-th direction. Theoretical development of these Green's functions is rather involved and their complete explicit forms can be found in the article by Mossessian and Dravinski (1989). Choosing f(y) to be concentrated at discrete points of the surface Sa, it can be shown (Mossessian, 1989;Mossessian and Dravinski, 1989) that the total wave field takes the following form:…”
Section: Boundary Integral Equation Analysismentioning
confidence: 99%
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