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Elastic modelling on a grid with vertically varying spacing1
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AbstractWe present a discrete modelling scheme which solves the elastic wave equation on a grid with vertically varying grid spacings. Spatial derivatives are computed by finite‐difference operators on a staggered grid. The time integration is performed by the rapid expansion method. The use of variable grid spacings adds flexibility and improves the efficiency since different spatial sampling intervals can be used in regions with different material properties. In the case of large velocity contrasts, the use of a non‐uniform grid avoids spatial oversampling in regions with high velocities. The modelling scheme allows accurate modelling up to a spatial sampling rate of approximately 2.5 gridpoints per shortest wavelength. However, due to the staggering of the material parameters, a smoothing of the material parameters has to be applied at internal interfaces aligned with the numerical grid to avoid amplitude errors and timing inaccuracies. The best results are obtained by smoothing based on slowness averaging. To reduce errors in the implementation of the free‐surface boundary condition introduced by the staggering of the stress components, we reduce the grid spacing in the vertical direction in the vicinity of the free surface to approximately 10 gridpoints per shortest wavelength. Using this technique we obtain accurate results for surface waves in transversely isotropic media.
Title: Elastic modelling on a grid with vertically varying spacing1
Description:
AbstractWe present a discrete modelling scheme which solves the elastic wave equation on a grid with vertically varying grid spacings.
Spatial derivatives are computed by finite‐difference operators on a staggered grid.
The time integration is performed by the rapid expansion method.
The use of variable grid spacings adds flexibility and improves the efficiency since different spatial sampling intervals can be used in regions with different material properties.
In the case of large velocity contrasts, the use of a non‐uniform grid avoids spatial oversampling in regions with high velocities.
The modelling scheme allows accurate modelling up to a spatial sampling rate of approximately 2.
5 gridpoints per shortest wavelength.
However, due to the staggering of the material parameters, a smoothing of the material parameters has to be applied at internal interfaces aligned with the numerical grid to avoid amplitude errors and timing inaccuracies.
The best results are obtained by smoothing based on slowness averaging.
To reduce errors in the implementation of the free‐surface boundary condition introduced by the staggering of the stress components, we reduce the grid spacing in the vertical direction in the vicinity of the free surface to approximately 10 gridpoints per shortest wavelength.
Using this technique we obtain accurate results for surface waves in transversely isotropic media.
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