Elastic wave‐propagation simulation in heterogeneous media by the spectral moments method

Geophysics ◽  
1996 ◽  
Vol 61 (5) ◽  
pp. 1269-1281 ◽  
Author(s):  
Valérie Rousseau ◽  
Claude Benoit ◽  
Roger Bayer ◽  
Michel Cuer ◽  
Gérard Poussigue

The second‐order elastic wave propagation equations are solved using the spectral moments method. This numerical method, previously developed in condensed matter physics, allows the computation of Green’s functions for very large systems. The elastic wave equations are transformed in the Fourier domain for time derivatives, and the partial derivatives in space are computed by second‐order finite differencing. The dynamic matrix of the discretized system is built from the medium parameters and the boundary conditions. The Green’s function, calculated for a given source‐receiver couple, is developed as a continued fraction whose coefficients are related to the moments and calculated from the dynamic matrix. The continued fraction coefficients and the moments are computed using a very simple algorithm. We show that the precise estimation of the waveform for the successive waves arriving at the receiver depends on the number of moments used. For long recording times, more moments are needed for an accurate solution. Efficiency and accuracy of the method is illustrated by modeling wave propagation in 1-D acoustic and 2-D elastic media and by comparing the results obtained by the spectral moments method to analytical solutions and classical finite‐difference methods.

2003 ◽  
Vol 2003.78 (0) ◽  
pp. _5-51_-_5-52_
Author(s):  
Masatoshi YAMASHITA ◽  
Akihiro NAKATANI ◽  
Yoshikazu HIGA ◽  
Hiroshi KITAGAWA

2011 ◽  
Vol 129 (4) ◽  
pp. 2611-2611 ◽  
Author(s):  
Kamyar Firouzi ◽  
Benjamin Cox ◽  
Bradley Treeby ◽  
Nader Saffari

2004 ◽  
Vol 12 (02) ◽  
pp. 257-276 ◽  
Author(s):  
M. TADI

This paper is concerned with the numerical modeling of elastic wave propagation in layered media. It considers two isotropic homogeneous elastic solids in perfect contact. The interface is parallel to the free surface. Two finite difference methods are developed. The usefulness of the methods are investigated for long time simulations and the accuracy of the results are compared with the response from an approximate model.


Geophysics ◽  
1991 ◽  
Vol 56 (2) ◽  
pp. 168-181 ◽  
Author(s):  
J. S. Sochacki ◽  
J. H. George ◽  
R. E. Ewing ◽  
S. B. Smithson

The divergence theorem is used to handle the physics required at interfaces for acoustic and elastic wave propagation in heterogeneous media. The physics required at regular and irregular interfaces is incorporated into numerical schemes by integrating across the interface. The technique, which can be used with many numerical schemes, is applied to finite differences. A derivation of the acoustic wave equation, which is readily handled by this integration scheme, is outlined. Since this form of the equation is equivalent to the scalar SH wave equation, the scheme can be applied to this equation also. Each component of the elastic P‐SV equation is presented in divergence form to apply this integration scheme, naturally incorporating the continuity of the normal and tangential stresses required at regular and irregular interfaces.


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