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| Wavefield extrapolation in pseudodepth domain | |
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The Sampling of the
axis should be small enough to avoid wavefield aliasing in the
domain, for example
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(25) |
where
is the minimum velocity in the model and
is the maximum frequency of the wave. Accordingly, the number of samples representing the
axis should be chosen to cover the largest expected
value,
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(26) |
The mapping velocity
is often chosen as a slightly smoothed version of true velocity
. This is because the
domain wave equation involves a differentiation
of
, for example the first equation in 15.
For second-order wave equations, the operators on the right-hand side can become significantly complicated in the
domain, such as Equation 23.
Thus, it is more convenient to code up its first-order form 21. For consistency, we will extrapolate the wavefields using the first-order form for all the examples in this paper.
Thus, the time derivatives in these equations are approximated by central differences,
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(27) |
and the spatial derivatives are approximated using the Fourier pseudospectral approuch (Carcione et al., 2002; Gazdag, 1981), as follows
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(28) |
where superscript
indicate time steps,
is the spatial Fourier transform in the
direction.
The change of the vertical axis from
to
does not affect the stability condition.
For both isotropic and VTI extrapolations, the same time-step is used in both the Cartesian and
domains.
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| Wavefield extrapolation in pseudodepth domain | |
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Next: Examples
Up: pseudodepth domain wave equation
Previous: Anisotropic extrapolation
2013-04-02