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- W2364305965 abstract "The Fourier transform method was used to study the problem of wave scattering by an depositional valley for incident plane SV waves in time domain.The problem was firstly transformed into the frequency domain,and then the calculations were performed in the frequency domain using indirect boundary element method for the effective frequency components,finally the results were transformed back into the time domain by the inverse Fourier transform.The validity of the method is confirmed by comparing the results with published ones.Numerical results are given by taking the amplification of incident Ricker wave by an depositional valley in one layer over half-space as an example.The results show that the duration of vibration is prolonged due to the existence of the soil layer and the depositional valley,and there exist distinct differences between the wave amplification by an depositional valley in one later over half-space and that in homogeneous half-space.The reasons were investigated and the effects of the depth and stiffness of the soil layer on scattering were discussed." @default.
- W2364305965 created "2016-06-24" @default.
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- W2364305965 date "2011-01-01" @default.
- W2364305965 modified "2023-09-22" @default.
- W2364305965 title "Wave scattering of a depositional valley in layered half-space for incident plane SV waves:time domain solution" @default.
- W2364305965 hasPublicationYear "2011" @default.
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