An elongated finite-difference scheme for 2D acoustic and elastic wave simulations in the frequency domain

Geophysics ◽  
2019 ◽  
Vol 84 (2) ◽  
pp. T29-T45
Author(s):  
Junichi Takekawa ◽  
Hitoshi Mikada

We have developed a novel scheme to simulate acoustic and elastic wave propagation in the frequency-domain using a rectangular finite-difference (FD) stencil. One of the main problem of the frequency-domain modeling is its huge computational costs, i.e., the calculation time and memory usage. To overcome this problem, researchers have proposed many schemes to reduce the number of grid points in a wavelength. In general, high-accuracy schemes require large-sized stencils that cause increment in the bandwidth of the impedance matrix. It is, therefore, important to improve the accuracy of numerical schemes without increasing the bandwidth. We have applied an elongated stencil with different sampling ratio between horizontal and vertical directions to circumvent extra numerical bandwidth in the impedance matrix. Optimal FD coefficients and the aspect ratio of the grid cell are determined to minimize the error of the phase velocity. We investigate the dispersion property of the proposed scheme using plane-wave analysis. The dispersion analysis indicates that we could reduce the number of grid points in a wavelength by approximately 2.78 for acoustic wave modeling and by approximately 3.15 for elastic wave modeling so that the error of the phase velocity is less than 1%. We also conduct numerical simulations using homogeneous and inhomogeneous models to demonstrate the effectiveness of our scheme. The comparison of numerical accuracy and computational costs between our scheme and the conventional ones indicates that the computational costs (calculation time, memory usage) can be reduced with high numerical accuracy especially in elastic wave modeling. Because our technique is a simple and a powerful cost-efficient frequency-domain method, the elongated stencil can be an alternative scheme to the conventional ones for acoustic and elastic wave modeling.

Geophysics ◽  
2016 ◽  
Vol 81 (6) ◽  
pp. T339-T356 ◽  
Author(s):  
Jing-Bo Chen ◽  
Jian Cao

Based on an average-derivative method, we developed a new nine-point numerical scheme for a frequency-domain elastic-wave equation. Compared with the classic nine-point scheme, this scheme reduces the required number of grid points per wavelength for equal and unequal directional spacings. The reduction in the number of grid points increases as the Poisson’s ratio becomes larger. In particular, as the Poisson’s ratio reaches 0.5, the numerical S-wave phase velocity of this new scheme becomes zero, whereas the classical scheme produces spurious numerical S-wave phase velocity. Numerical examples demonstrate that this new scheme produces more accurate results than the classical scheme at approximately the same computational cost.


2013 ◽  
Author(s):  
Alan A. V. B. Souza ◽  
André Bulcão ◽  
Bruno Pereira Dias ◽  
Djalma M. Soares Filho ◽  
Fernanda F. Farias ◽  
...  

Geophysics ◽  
2018 ◽  
Vol 83 (4) ◽  
pp. T209-T234 ◽  
Author(s):  
Jing-Bo Chen ◽  
Jian Cao

Because of its high computational cost, we needed to develop an efficient numerical scheme for the frequency-domain 3D elastic wave equation. In addition, the numerical scheme should be applicable to media with a liquid-solid interface. To address these two issues, we have developed a new average-derivative optimal 27-point scheme with arbitrary directional grid intervals and a corresponding numerical dispersion analysis for the frequency-domain 3D elastic wave equation. The novelty of this scheme is that its optimal coefficients depend on the ratio of the directional grid intervals and Poisson’s ratio. In this way, this scheme can be applied to media with a liquid-solid interface and a computational grid with arbitrary directional grid intervals. For media with a variable Poisson’s ratio, we have developed an effective and stable interpolation method for optimization coefficients. Compared with the classic 19-point scheme, this new scheme reduces the required number of grid points per wavelength for equal and unequal directional grid intervals. The reduction of the number of grid points increases as the Poisson’s ratio becomes larger. In particular, the numerical S-wave phase velocity of this new scheme becomes zero, whereas the classic 19-point scheme produces a spurious numerical S-wave phase velocity, as Poisson’s ratio reaches 0.5. We have performed numerical examples to develop the theoretical analysis.


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