Page 79 - Acquisition and Processing of Marine Seismic Data
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70                            2. MARINE SEISMIC DATA ACQUISITION


































           FIG. 2.28  (A) Near- and far-field zones of a marine seismic source. Near-field signature is measured in the zone between
           the physical dimensions of the source array (d) and the dominant wavelength of the signal (λ) while the far-field signature is
           measured with a hydrophone located approximately 300 m below the source array. (B) Typical near-field signature. P is peak
           amplitude of initial pressure, B is amplitude of the first bubble effect, T is bubble period, and T R is the rise time. (C) Typical far-
           field signature. P-P is peak-to-peak amplitude of initial pressure.

           individual guns of a gun array interfere con-  acoustic pressure to maximum bubble pres-
           structively and arrive at a distant hydrophone  sure). Both parameters are measured from
           within one sampling interval (Dragoset, 2000).  zero-to-peak value for near-field signatures
           The far-field signature is measured with a   and peak-to-peak value for far-field signatures.
           hydrophone typically located 300 m below the  Near-field signatures have an initial high pres-
           array (Fig. 2.28a) so that the signal appears as  sure pulse, which then falls to negative pressure
           if it is emitted from a point source. If we locate  values below the hydrostatic pressure followed
           the hydrophone to the aft or side of a gun array,  by oscillating amplitudes due to the successive
           the signatures change from one location to   collapse and expansion of the air bubble
           another due to the array effect, so the far-field  (Fig. 2.28B). This initial pressure creates the
           hydrophone must be directly below the array  highest amplitude of the signature, which then
           so that the pressure pulses from each individual  gradually decreases with time. The effect of
           gun arrive at the hydrophone at the same time.  the source ghost is very small on the near-field
              Near- and far-field signatures are commonly  signature because of the location of the near-field
           used to delineate the source strength (maximum  hydrophone. The important parameters that can
           acoustic pressure radiated by the source) and  be obtained from the near-field signature are the
           peak-to-bubble ratio (the ratio of maximum   bubble period (T) and peak-to-bubble ratio (PBR),
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