Page 58 - Acquisition and Processing of Marine Seismic Data
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2.1 COMPONENTS OF MARINE SEISMIC ACQUISITION               49






















           FIG. 2.9  Photos of (A) fluid-filled digital, (B) solid digital streamers.

           kerosene, to enable cable buoyancy in the seawa-  streamer skin. Axial vibrations of the streamer
           ter. Although fluid-filled streamers are outdated  travel along the cable as pressure fluctuations
           today, they are still in use, especially along with  resulting in the streamer jacket contracting and
           small-scale seismic systems used by academia  bulging out. The bulge waves induce noise into
           and with the single-channel acquisitions for site  the hydrophones of the fluid-filled streamers.
           surveys. This kind of streamers suffers from  Moreover, these streamers are also quite sen-
           several significant issues. One of the most  sitive to the ripples at the surface of the ocean.
           important  problems   with  the  fluid-filled  High-amplitude acoustic noise at the low-
           streamers is safety, since the kerosene is toxic  frequency band originating from the ocean sur-
           and easily flammable, which may cause envi-  face ripples radiates along the fluid filling the
           ronmental hazards and safety or health issues  streamer, which ultimately means that the
           onboard in case of possible damage in the jacket  fluid-filled streamers must be towed at relatively
           of the streamer encountered during the tow and  higher depths to avoid the ocean surface noise.
           deployment. Furthermore, such damage to the  This situation, however, adversely affects the
           skin results in salty seawater intrusion into the  seismicdataresolution,resultinginthecollection
           housing, which may result in serious issues with  of seismic data with much narrower frequency
           the electronic components of the streamer and  band, since the depth of the streamer is an impor-
           typically results in a spike-like noise appearing  tant parameter directly affecting the resolution
           as extreme amplitude bursts distributed ran-  of the seismic data due to the ghost signal inter-
           domly along the channels within the damaged  ference (Section 2.5.1.2).
           streamer   sections.  Therefore,  fluid-filled  An approach to overcoming the aforemen-
           streamers require frequent maintenance, which  tioned shortcomings of the fluid-filled streamers
           may ultimately cause downtimes during the    is to use a soft and flexible gel material produced
           acquisition.                                 from polyurethane to fill in the streamer housing.
              Fluid-filled streamers also suffer from noise  Gel-filled streamers have several advantages as
           originated by bulge waves, which are formed  compared to fluid-filled streamers. First of all,
           by the interactions among the members in the  they are more durable than fluid-filled streamers
           streamer housing, such as kerosene itself, wiring,  and they do not induce environmental, safety
           buoyancy spacers, or strength members, and the  and health issues. Since the gel is not liquid, no
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