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SEISMIC SURVEYING 


sensors in the seismic streamers, as well as slanted cable configurations. In both cases, towing the cable at greater depth would allow for operation in rougher sea state conditions, although the corresponding increased variability of the sea-air reflection coefficient limits the effectiveness of the deghosting process. In addition, data dependent matched filtering is necessary to match the noisy geophone data to the hydrophone in the dual sensor case, while the slanted streamer approach requires some intricate data dependent processing to handle the variable ghost. Tis can only be done effectively poststack, which severely limits the use of prestack data for reservoir characterisation. Source deghosting through time and space staggering does show promising results, and can be used to good effect. New streamer deghosting techniques are therefore required to mitigate the afore mentioned drawback, and are subject of active research in the industry. Unfortunately, the increased patenting efforts by major players are limiting the ability to build on the current state of knowledge, and would seem to go far beyond the legitimate desire to justify R&D expenditure by protecting new inventions. An interesting view of the use of


wide bandwidth data was presented by Philip Fontana et al (SEG, 2011, San Antonio), in which he argued that deeper understanding of the target reservoirs is required. In many deeper targets, the earth spectrum has a limited bandwidth, and wide bandwidth acquisition will actually decrease the signal to noise ratio through the dispersion, absorption, and scattering of the higher frequencies in the seismic signal. An underestimated recent development is the emergence of new noise eliminating processing technologies (Fig. 1.), which do not have the disadvantages of conventional filtering approaches, which tended to smear the data and limit spatial resolution. As often, the need to drive down


acquisition cost has also resulted in elimination of unnecessary cost. A good example is the need for seismic infill, which traditionally can be as high as 20-30 per cent of the total acquisition. An understanding of the need for dense sampling at longer shooting offsets is emerging, initially through office based analysis of streamer spacing and possibilities to use fanned streamers. A more effective solution is offered by the recent introduction of Fresnel Zone Binning (Fig. 2.), which allows for a full analysis of target depth, seismic frequency dependency, and offsets, resulting in an optimised


Fig. 2. Dimensions of Fresnel Zones as a function of time and offset.


acquisition with real time analysis driving the streamer positioning. Further to cost reduction, a significant


effort is spent on simultaneous seismic acquisition, also called blended shooting. In particular the wide azimuth acquisition, both towed and ocean bottom, can benefit tremendously from simultaneous shooting. Tis has been demonstrated convincingly for exploration and development surveys, and the industry is now attempting to solve this for production monitoring surveys, which require a lower level of remnant deblending noise to achieve reliable analysis of the time- lapse signal. However, no matter how seismic acquisition technology improves, limitations remain in the acquisition of low frequencies. In onshore acquisition these are being solved through the use of sensors that record down to 0Hz, yielding startling improvements in the ability to create a correct earth model through the use of full waveform inversion rather than travel time inversion methods. Te inherent limitations in the acquisition


of low frequencies offshore however, require different geophysical methods. A first step towards acquiring these is


through the addition of a limited number of ocean bottom seismic sensors, yielding a significantly improved frequency spectrum, as shown by recent experiments in the Barents Sea. As these ocean bottom sensors can be deployed at relatively large spacing, this approach promises to be a very cost effective way to acquire better data. Te use of gravity/ gradiometry, magnetic, magneto telluric, and controlled source electromagnetic data offers great opportunities for improved definition of the earth model, and for derisking prospects by techniques complementary to seismic analysis. Te introduction of towed CSEM acquisition would be a step change, lowering the threshold for the acquisition of richer datasets. In conclusion, the drive to get more,


better, and cost-effective data is stronger than ever, and it is expected that, in addition to currently used technologies, some more radical changes will be needed. 


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Eric de Graaff is Chief Scientist, Fugro, Leidschendam, The Netherlands. www.fugro.com IHSS 12


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