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Houston Geological Society Bulletin

Abstract


Houston Geological Society Bulletin, Volume 40, No. 3, November 1997. Pages 8-8.

Abstract: The Future of 4-D Previous HitReservoirNext Hit Previous HitMonitoringNext Hit: Advances in Technology for Large Oil and Gas Fields

By

Roger N. Anderson
Lamont-Doherty Earth Observatory

Getting more oil out of old fields is the payout of 4-D Previous HitseismicNext Hit Previous HitreservoirNext Hit Previous HitmonitoringNext Hit. 4- D combines the analysis of Previous HitseismicNext Hit acoustic changes occurring over time with other borehole and surface measurements. 4-D analysis has the ability to track time-dependent changes such as pressure changes and production histories. The result is a coupled model of oil and gas drainage and a more accurate simulation of future production.

Evaluating the Subsurface over Time Using Time-Lapse Previous HitSeismicNext Hit

The tools and techniques required to interpret past acoustic changes that have occurred in oil and gas fields perform two essential tasks: 1) normalization of the Previous HitseismicNext Hit images between snapshots taken at different times, using different equipment and different geometries of acquisition and then processed differently at the computer center, and 2) interpretation of the similarities and differences in the acoustic signature of oil, gas, and water in the Previous HitreservoirNext Hit as they change over time.

More than twenty oil and gas fields from (fig. 1, 2) the Gulf of Mexico and the North Sea are the proving ground for new 4-D technology developments. These fields provide contrasts in acoustic response and Previous HitseismicNext Hit signal-to-noise, often between reservoirs within the same field, that point to important lessons for the planning of future 4-D Previous HitreservoirNext Hit Previous HitmonitoringNext Hit projects. Conclusions to date are 1) pressure history often affects Previous HitseismicNext Hit responses as significantly as oil/gas/water mix changes and 2) volumetric "region-growing" is a method to scan multiple 3-D data sets for changes at a fast enough computational rate to satisfy engineers in charge of production. Region-growing is a signal analysis technique developed for the detection of differences in MRIs, CAT and PET scans, and in anti-submarine warfare. Region-growing is also very useful for the isolation of 4-D Previous HitseismicNext Hit differences that are meaningful in reservoirs.

Better understanding of the pattern of drainage to the surface will allow for better planning and execution of recovery programs in the future. Four-D provides the "killer app" for impedance inversions, which are the most likely Previous HitseismicNext Hit attributes that can detect change over time in reservoirs. As we get better at 4-D Previous HitmonitoringNext Hit, more original oil-in-place will be extracted from producing reservoirs.

The 4-D Previous HitSeismicNext Hit Previous HitReservoirNext Hit Simulation Loop

Previous HitSeismicNext Hit inversions will be routinely used on time-lapse Previous HitseismicNext Hit data sets to produce impedance differences. These become geostatistical Previous HitreservoirNext Hit characterizations and Previous HitreservoirNext Hit simulator data to quantify the variations in fluid saturations with time. New 3-D finite element models will be developed to compute synthetic Previous HitseismicNext Hit responses to differences detected by the real observations. Previous HitSeismicTop-to-petrophysical iterations are added to the simulation loop. The continual updating of the loop forms a planning tool for predicting new drilling targets for recovery of bypassed oil and gas. Repeated looping of information leads to planning the time, spacing, types of receivers and borehole arrays that will be needed to successfully monitor the oil and gas fields of the future.

Figure 1. Production from a Gulf of Mexico well drilled after 4-D evaluation.

Figure 2. The field has added reserves after drilling wells based on 4-D.

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Cover photo. 3-D graphic illustration courtesy Roger Anderson, Lamont-Doherty Earth Observatory, New York.

 

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