All Days 2012
DOI: 10.2118/154503-ms
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Assisted Seismic History Matching in Different Domains: What Seismic Data Should We Compare?

Abstract: Time-lapse (4D) seismic data can be integrated into history matching by comparing predicted and observed data in various domains. These include the time domain (time traces), seismic attributes, or petro-elastic properties such as acoustic impedance. Each domain requires different modelling methods and assumptions as well as data handling workflows. The aim of this work is to investigate the degree to which the choice of domain influences theoutcome of history matching on the choice of best model and associate… Show more

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Cited by 5 publications
(2 citation statements)
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“…The petro-elastic model uses pressure, saturation and static reservoir properties to calculate density and velocity for each grid cell (Sagitov et al 2012). The most used approaches to generate seismic data are direct methods, which approximate the geological model on a numerical mesh.…”
Section: Petro-elastic Model (Pem)mentioning
confidence: 99%
“…The petro-elastic model uses pressure, saturation and static reservoir properties to calculate density and velocity for each grid cell (Sagitov et al 2012). The most used approaches to generate seismic data are direct methods, which approximate the geological model on a numerical mesh.…”
Section: Petro-elastic Model (Pem)mentioning
confidence: 99%
“…Thus, from an engineering perspective, data integration on this domain would be the first choice. Then information can be directly applied without any domain conversion or issues associated with global objective functions involving production data and maps derived from seismic data (Sagitov and Stephen, 2012). However from a geophysics perspective, this domain is the most complex as it requires two inversions that involve compounding errors and non-uniqueness issues Yet the ability to distinguish between pressure and saturation effects relies on the 4D amplitude versus offset (AVO) response of the reservoir (Tura and Lumley, 2000;Landrø et al, 2003), and uncertainties in the rock physics models remain (Johnston, 2013).…”
Section: Introductionmentioning
confidence: 99%