Page 297 - Acquisition and Processing of Marine Seismic Data
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288                                   5. PREPROCESSING






























           FIG. 5.50  (A) A raw shot gather with strong power-line harmonic noise interference between the channel numbers 48 and
           52. (B) Same shot after killing the traces containing the interference.



              Fig. 5.50 shows an example trace kill applica-  stack section after stacking. In two successive
           tion on a shot gather which has strong powerline  shot gathers in Fig. 5.51, the first six and last
           harmonic noise interference at six traces    three channels of the recording system are dead
           between channel numbers 48 and 52. Although  and are recording only noise. Fig. 5.51B shows
           these channels may have data as well, the inter-  the same shots after the dead channels are killed.
           ference is so strong that the reflection ampli-  Normally, the channel numbers of those dead
           tudes are concealed behind the noise. The    traces do not change for a specific survey; there-
           noise has monofrequency amplitudes appearing  fore, a regular channel number definition is gen-
           at 50 Hz and its multipliers; therefore it is neces-  erally sufficient to apply the trace kill to the
           sary to apply a notch filter to remove the inter-  whole seismic dataset, to remove the dead
           ference. However, applying a monofrequency   channels.
           notch filter is generally avoided because it pro-  As mentioned in Section 3.10.2, seismic data
           duces amplitude notches in the spectrum, which  may contain extremely high-amplitude tran-
           may ultimately cause issues during deconvolu-  sient noise bursts, or spikes, with amplitudes
           tion. Therefore, killing these traces is generally  distributed on almost all the available frequency
           the easiest and most convenient way to remove  band. Spikes may not be suppressed by simple
           powerline harmonic noise (Fig. 5.50B).       stacking because they may have extremely
              If one or more channels of the recording  higher amplitudes than those of primary reflec-
           instrument are nonfunctional, then the ampli-  tions. In some cases, such as seawater leakage
           tudes recorded at those traces cannot be used,  into the fluid-filled streamer sections, there
           since they may corrupt the quality of the final  may be several spikes randomly distributed
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