Practical considerations

From SEG Wiki
Jump to: navigation, search
Seismic Data Analysis
Series Investigations in Geophysics
Author Öz Yilmaz
ISBN ISBN 978-1-56080-094-1
Store SEG Online Store

Figure 6.4-4 shows the modeled CMP gather before and after t2-stretching. Note that the hyperbolas in Figure 6.4-4a are replaced with parabolas in Figure 6.4-4b. The t2-transformation causes compression on data before 1 s and stretching on data after 1 s. As mentioned earlier, a nice property of the parabolic moveout is that it is invariant along the axis t′ = t2 for a specific value of velocity (equation 12). The sampling rate along the t2-axis was set equal to t′/nt, where nt is the number of samples along the t-axis. There can be a potential problem of aliasing near t = 0, causing frequency distortion for shallow events. This problem can be avoided by finer sampling along the t′-axis.

By using the singular-value decomposition procedure described in Section F.3, we obtain the Radon transform represented by the velocity-stack gather in the stretched coordinates as shown in Figure 6.4-4c. Finally, we undo the stretching to get the Radon transform represented by the velocity-stack gather in Figure 6.4-4c. Compare this with the conventional velocity-stack gather in Figure 6.4-2d. Note the significant reduction of amplitude smearing and enhancement of velocity resolution in the velocity-stack gather based on the Radon transform. In particular, multiples and primaries now are clearly distinguishable. Nevertheless, there is some frequency distortion of the wavelet associated with the shallowest event in the Radon transform (Figure 6.4-4d), primarily because of stretching and unstretching.

By using the Radon transform (Figure 6.4-5a), the CMP gather can be faithfully reconstructed (Figure 6.4-5b). Compare the panels in Figure 6.4-5 with those in Figure 6.4-3. Note that, unlike the conventional velocity-stack gather, repeated application of the Radon transformation always reproduces the CMP gather with minimal amplitude distortion (Figures 6.4-5b and 6.4-5d), with the exception of frequency distortion at the very early times.

To summarize the construction of velocity-stack gathers using the conventional procedure defined by equation (10a) and the Radon transform based on equation (16), we refer to Figures 6.4-6 and 6.4-7. Starting with the synthetic CMP gather (Figure 6.4-6a), we use equation (10a) to get the conventional velocity-stack gather (Figure 6.4-6b), and the reconstructed gather from it (Figure 6.5-6c) using equation (10b). Again, starting with the same synthetic CMP gather (Figure 6.4-7a), we obtain the velocity-stack gather based on the Radon transform (Figure 6.4-7b) defined by equation (16), and the reconstructed gather from it (Figure 6.4-7c) using equation (10b). It is important to note that the reconstruction procedure using equation (10b) to obtain the modeled CMP gather is the same in both Figures 6.4-6 and 6.4-7. The difference lies in the way the velocity-stack gather is created — the conventional approach causes amplitude smearing along the velocity axis (Figure 6.4-6c), and the procedure based on the Radon transform reduces this smearing and thus increases the resolution along the velocity axis (Figure 6.4-7c).

Now we examine the performance of the Radon transform in the presence of random noise. Consider the CMP gather in Figure 6.4-8a after the addition of band-limited random noise that is uncorrelated from trace to trace (Figure 6.4-8b). Figure 6.4-8c shows the conventional velocity-stack gather constructed by using equation (10a), and Figure 6.4-8d shows the velocity-stack gather constructed by using the Radon transform based on equation (16). When the data are contaminated by noise, choice of the damping factor β to stabilize the solution represented by equation (16) has a significant impact on the quality of the velocity-stack gather. It is important to emphasize that for the velocity-stack construction using the hyperbolic discrete Radon transform, noise is anything but hyperbolic events.

The β factor is equivalent to the prewhitening factor in Wiener-Levinson deconvolution. In this regard, the optimum β factor depends significantly upon the noise level in the data. Figure 6.4-9 shows estimates of the velocity-stack gathers using four different values of the β factor. For the noise-free case (Figure 6.4-7), theoretically, the best choice of β should be zero; however, to avoid exaggeration of numerical roundoff errors, β should be chosen to be a very small number. A practical rule of thumb is that stability in the SVD procedure does not improve further for β factors beyond a certain value (compare Figures 6.4-9c and d). For field data, a value of 1% of the largest eigenvalue of the matrix LT*L of equation (16) often yields adequate results (Section F.3).

Since the elements of the matrix L in equation (16) depends on the geometry of the CMP gather under consideration, estimation of the Radon transform u would normally require singular-value decomposition (equation F-22) for each individual gather. To circumvent the repeated application of the singular-value decomposition — a numerically intensive scheme, the Radon transform estimation procedure can be made efficient by implementing a two-staged computation. First, the part of the Radon transform associated with the operator LT* in equation 16) can be computed using the actual offset distribution of the input CMP gather. Second, the part of the Radon transform associated with the operator (LT*L)-1 is computed by the singular-value decomposition only once for the entire data set using an offset distribution that may be considered an acceptable average of the actual offset distributions of the CMP gathers along the line traverse.

Finally, we examine the ability of the Radon transform in separating hyperbolic events from band-limited random noise. Consider the same noisy gather as in Figure 6.4-8b. Reconstruct this CMP gather as shown in Figure 6.4-10a using the velocity-stack gather shown in Figure 6.4-8d, and subtract the result from the original noisy CMP gather (Figure 6.4-8b). This difference gather is shown in Figure 6.4-10b, and it represents the least-squares error e defined as the difference between the actual CMP gather d and the modeled CMP gather d′ defined by equation (15). Ideally, it should contain anything but hyperbolic events. Nevertheless, the missing high-frequency components in the shallowest part of the reconstructed CMP gather have leaked into the difference gather (Figure 6.4-10d). The actual random noise added to the original CMP gather (Figure 6.4-8a) is shown in Figure 6.4-10c. Compare the extracted noise (Figure 6.4-10b) with the actual noise (Figure 6.4-10c) and note that the difference between the two (Figure 6.4-10d) contains negligibly small residual amplitudes aside from some remnants of the hyperbolic events.







See also

External links

find literature about
Practical considerations
SEG button search.png Datapages button.png GeoScienceWorld button.png OnePetro button.png Schlumberger button.png Google button.png AGI button.png