Three component 1D viscoelastic FDM for plane-wave oblique incidence

Arash Jafargandomi, Hiroshi Takenaka

Research output: Chapter in Book/Report/Conference proceedingChapter

1 Citation (Scopus)

Abstract

We propose a very efficient scheme for modeling three-component seismic plane waves in vertically heterogeneous attenuative media using the finitedifference (FD) method in the time domain. The scheme is able to represent P, SV, and SH waves incoming from different direction. The algorithm can also calculate the plane-wave responses of media for different incident angels. In the algorithm, neglecting lateral heterogeneity, the wave equation is rewritten for plane waves by applying a 2D Radon transform to the 3D general wave equation. QP and QS are incorporated via generalized Zener body rheological models for viscoelasticity to represent anelastic attenuation. Our FD scheme uses a 1D grid, which leads to a significant reduction in computation time and memory requirements as compared to the corresponding 3D or 2D computations. It may be an efficient tool for pre- or post-analysis of local structural effects including anelastic attenuation, before or after the large-scale seismic wave simulation. To demonstrate the ability and efficiency of the scheme, we calculate a synthetic vertical seismic profile (VSP) for a borehole with a highly heterogeneous velocity model and frequency dependent attenuation model in the Kanto area of Japan.

Original languageEnglish
Title of host publicationAdvances in Geosciences: Volume 20: Solid Earth (SE)
PublisherWorld Scientific Publishing Co.
Pages299-312
Number of pages14
ISBN (Electronic)9789812838186
ISBN (Print)9812838171, 9789812838179
DOIs
Publication statusPublished - Jan 1 2010
Externally publishedYes

Fingerprint

wave equation
Radon transform
vertical seismic profile
viscoelasticity
SH-wave
heterogeneous medium
seismic wave
P-wave
borehole
modeling
simulation
analysis
method
effect

ASJC Scopus subject areas

  • Earth and Planetary Sciences(all)

Cite this

Jafargandomi, A., & Takenaka, H. (2010). Three component 1D viscoelastic FDM for plane-wave oblique incidence. In Advances in Geosciences: Volume 20: Solid Earth (SE) (pp. 299-312). World Scientific Publishing Co.. https://doi.org/10.1142/9789812838186_0020

Three component 1D viscoelastic FDM for plane-wave oblique incidence. / Jafargandomi, Arash; Takenaka, Hiroshi.

Advances in Geosciences: Volume 20: Solid Earth (SE). World Scientific Publishing Co., 2010. p. 299-312.

Research output: Chapter in Book/Report/Conference proceedingChapter

Jafargandomi, A & Takenaka, H 2010, Three component 1D viscoelastic FDM for plane-wave oblique incidence. in Advances in Geosciences: Volume 20: Solid Earth (SE). World Scientific Publishing Co., pp. 299-312. https://doi.org/10.1142/9789812838186_0020
Jafargandomi A, Takenaka H. Three component 1D viscoelastic FDM for plane-wave oblique incidence. In Advances in Geosciences: Volume 20: Solid Earth (SE). World Scientific Publishing Co. 2010. p. 299-312 https://doi.org/10.1142/9789812838186_0020
Jafargandomi, Arash ; Takenaka, Hiroshi. / Three component 1D viscoelastic FDM for plane-wave oblique incidence. Advances in Geosciences: Volume 20: Solid Earth (SE). World Scientific Publishing Co., 2010. pp. 299-312
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