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Explore the significance of wavelet in de-multiple and de-ghosting methods for seismic data processing. Discuss the Wavelet Estimation technique for improving wavefield prediction accuracy. Address the need for normal derivative in wavelet estimation. Present a new method to obtain wavelet with reduced singularity under the source. Analyze the effects of introducing perturbations and errors on wavelet estimation stability. Investigate the error analysis and weighting effects in wavelet estimation. Conclude with future testing plans and the impact on wave-theoretic demultiple methods.
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Wavelet Estimation Below Towed Streamers Zhiqiang Guo University of Houston and PGS M-OSRP Annual Meeting University of Houston March 31 – April 1, 2004
Why Do We Need the Wavelet? De-multiple, de-ghosting Wave equation based method needs wavelet
Why Do We Need the Wavelet? (cont.) Inverse scattering & sub-series image All events are assumed to be primaries
Wavelet Estimation (Weglein and Secrest, 1990 ) FS FS MS MS (1) ? Require: wavefield and its normal derivative
Wavefield prediction (H. Tan & A. Osen) F.S M.S (2) Require: wavefield and an extra receiver
Observation (H. Tan) when f<125Hz, z=6m
Amplitude of Predicted Wavefield Predicted Exact
Phase of Predicted Wavefield Predicted Exact
Amplitude of Predicted Derivative Predicted Exact
Phase of Predicted Derivative Predicted Exact
Problem FS MS We do need normal derivative under the source, in order to use Weglein&Secrest’s formula to obtain wavelet
New Method of Wavelet Estimation To avoid the singularity under the source, we include AG Is it perfect to take the derivative when and then substitute it into Weglein & Secrest formula ?
Alteration: add some perturbation on purpose No. Equation (1) is the same as equation (2) at M.S. (Weglein and Amundsen 2003) , in order to use both of them, we deliberately introduce some error, and it is valid for all x by altering the two equations so that they are independent. • Is it ok to take the derivative above M.S. instead of at M.S. ?
New Method of Wavelet Estimation (cont.) Weglein & Secrest
New Method of Wavelet Estimation (cont.) • How big is the error ? • Stable ? As • Take account of the effect of Green’s • Function under source
Model with three scatters Scatters: (-50,40), (0,40), (50,40) Free surface 2m 6m Measurement surface C0=1500m/s
Weighting F.S. Reflector =40m zb=100m Zb=500m Zb=1000m Zb=1500m
Weighting (cont.) W= 0.2 0.4 0.6 0.8 1 0.8 0.6 0.4 0.2 Zb=100m Zb=500m Zb=1000m Zb=1500m Zero offset: 100% Far offset(200m): 20% For all four estimation depths B W=0.2 0.4 0.6 0.8 1 0.8 0.6 0.4 0.2 Zero offset: 100% Far offset(200m): 20% For 1st depth 2ns: 80% of 1st 3rd : 70% of 1st 4th: 60 % of 1st C 80% 70% 60%
Conclusion & future work • Tests for different prediction depths and noise stability on synthetic data are encouraging • Further tests are planned for the impact on wave-theoretic demultiple methods based on energy minimization method for wavelet
Acknowledgements Dr. Weglein Dr. Tan M-OSRP