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The zero-offset waveform

The first comparison involves the zero-offset response of the three methods. A window that includes the first two primary reflections (both PP) was selected from the zero-offset trace of the vertical components for the three simulated wavefields. Figure [*] shows the three waveforms. Except for small differences in the amplitude and the precursor lobe, the waveforms generated by the propagator-matrix and dual-operator methods are very similar. The dispersion is minimal and the kinematics are in accordance with theoretical expectations. The dispersive character observed in the wavefield of the traditional finite-difference scheme becomes more clear in the selected window. As a result of the dispersion, the traveltime difference between the two reflections (using the central picks as the measuring criterion) is slightly larger than the theoretical value.

 
zeroresp
zeroresp
Figure 5
Zero offset response generated by the three schemes. The three curves correspond to a window selected from the first traces of Figures [*]-a, [*]-a, and [*]-a, which include the reflections from the first two interfaces of the model. The continuous line comes from the Haskell-Thomson scheme, the dotted-line comes from the dual-operator scheme, and the dashed-line comes from the traditional finite-difference scheme.
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The theoretical ratio between the amplitudes of the two reflections is given by

\begin{displaymath}
{\mbox{Amp}_2 \over \mbox{Amp}_1} = {R_2 \over R_1} \; (1-R_...
 ...[{t_1 v_1^2 \over (t_2 - t_1) v_2^2 + t_1 v_1^2} \right]^{1/2},\end{displaymath}

where the first term is the ratio between the normal incidence reflection coefficients, the second term is the two-way transmission coefficient, and the third term is the 2D-divergence relative correction. The value obtained from the propagator-matrix trace coincides with the predicted value, while the value from the dual-operator trace is 3.7 percent higher, and the value from the traditional finite-difference trace is 7.5 percent lower.


previous up next print clean
Next: Amplitude versus offset Up: DYNAMIC BEHAVIOR Previous: Reflection seismograms from a
Stanford Exploration Project
11/18/1997