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Propagation of a compressional pulse in a layered solid
Author(s) -
Pekeris C. L.,
Alterman Z.,
Abramovici F.,
Jarosch H.
Publication year - 1965
Publication title -
reviews of geophysics
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 8.087
H-Index - 156
eISSN - 1944-9208
pISSN - 8755-1209
DOI - 10.1029/rg003i001p00025
Subject(s) - seismogram , sawtooth wave , pulse (music) , half space , physics , displacement (psychology) , point source , point (geometry) , geometry , optics , computational physics , mathematical analysis , geology , mathematics , seismology , psychology , detector , computer science , computer vision , psychotherapist
In this investigation we solve the problem of propagation of a compressional pulse in a solid half‐space which is overlain by a solid layer of different properties. The point source is situated at the depth ½ H , H denoting the thickness of the layer. Theoretical seismograms of the vertical displacement w at the surface are evaluated out to ranges r = 20 H . The solution is obtained by the exact ray theory. The displacement W o due to the source was assumed to have a shape which at large distances reduces to a sawtooth. The once‐reflected waves from the interface, PP and PS , are strongly marked. The Rayleigh wave is already recognizable at r = 5 H and is fully developed at r = 20 H . The method of ‘ray theory’ was applied here far into the region where the normal mode theory converges well. The theoretical seismograms are illustrated. The properties assumed for the layer (1) and for the half‐space (2) are λ 1 = μ 1 μ 2 = 2μ 1 c s2 ≡ c 2 = 1.1 c s1 ≡ 1.1 c 1 c p2 > c p1 > c 2 > c 1