3次元多層地盤における地表面水平点加振の応答変位に対する表面波と実体波の寄与
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概要
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A numerical method is presented for computing ground surface displacements in radial and transverse directions that are induced by a harmonic horizontal point force acting on a three-dimensional layered elastic half-space. The contribution of the residue of the Rayleigh and Love poles and the branch line integrals, i. e., that of surface and body waves, to the ground displacements is computed for two-layered media. Its variation with the S-wave velocity ratio and Poisson's ratio of the media as well as the distance and frequency of the source is examined.
- 1996-03-30
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