Page 290 - Acquisition and Processing of Marine Seismic Data
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5.6 GAIN RECOVERY                              281



































           FIG. 5.41  AGC gain corrections for different AGC scalar calculation methods on a marine shot gather. (A) Filtered shot
           with no gain, and its AGC corrected versions using 500 ms operator length calculated by using (B) mean, (C) RMS, and
           (D) median values of the amplitudes samples within the AGC window.



           Fig. 5.43 illustrates the effect of AGC operator  termed the shadow zone. In the case of using
           length on the efficiency of the application. AGC  AGC scalar applications on the central samples
           operation is much more effective for smaller  of the AGC window, there will be a low ampli-
           operator lengths, and the amplitudes of both in  tude “quiet” zone just before the seabed reflec-
           shallow and deeper parts of the data become  tion on the shot gathers, the length of which
           much more balanced. AGC application becomes  exactly equals half of the AGC operator length
           progressively ineffective as the operator length  (Δt/2) in the case of the application to the central
           increases. In practice, the suitable operator length  samples of the AGC window. If a smaller AGC
           is selected by considering the recording length of  operator is used, this quiet zone will be narrow.
           the input data. Operator lengths between 250 and  Above this zone is the shadow zone in the water
           1000 ms generally produce acceptable results;  column on the shot gathers. This quiet zone is
           however, depending on the record length, the  not only observed on shot gathers, but also evi-
           most suitable operator length can be determined  dent on the final stack sections if an AGC is
           by trying several different values and visually  applied after stacking (Fig. 5.44A). When there
           checking the results after each trial.       is a strong reflection on the stack data, there
              AGC blows up the noise in the water column  may be a low amplitude band of Δt/2 millisec-
           and produces a relatively high-amplitude noise  onds width just below the high amplitude reflec-
           zone just above the seabed (Fig. 5.43), which is  tion after AGC (Fig. 5.44B).
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