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It is often convenient to arrange the calculation of a wave
to remove the effect of overall translation,
thereby making the wave appear to ``stand still.''
It is easy enough to introduce
the time shift t0 of a vertically propagating wave
in a hypothetical medium of velocity , namely,
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(67) |
Instead of solving equations in coordinates (t,x,z)
we could solve them in the so-called retarded coordinates
(t',x',z') where
t'=t-t0(z), x'=x and z'=z.
(For more details, see IEI sections 2.5-2.7.)
A time delay t0 in
the time domain corresponds to multiplication
by in the -domain.
Thus, the wave pressure P is related
to the time-shifted mathematical variable Q by
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(68) |
which is a generalization of equation (55)
to depth-variable velocity.
(Equations () and () apply in both x- and
kx-space).
Differentiating with respect to z gives
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(69) |
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Next, substitute () and ()
into Table .4
to obtain the retarded equations in Table .5.
Table:
Retarded form of phase-shift equations.
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general |
diffraction |
+ thin lens |
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Next: Lateral velocity variation again
Up: END OF CHAPTER FOR
Previous: END OF CHAPTER FOR
Stanford Exploration Project
12/26/2000