2005
DOI: 10.2118/84571-pa
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Quantitative Use of 4D Seismic Data for Reservoir Description

Abstract: The major contribution of this paper is the description of an efficient, gradient-based method for incorporating time-lapse seismic impedance data in an automatic history-matching procedure. We use a finite-difference, black-oil reservoir simulator, with rock physics included, to predict seismic impedance as a function of saturation and pressure. The adjoint method is used to compute the derivatives of seismic impedance change in each gridblock with respect to porosity, permeability, pressure, and phase satura… Show more

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Cited by 44 publications
(20 citation statements)
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References 26 publications
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“…Liu and Oliver [108] used a quasi-Newton method to adjust geologic facies boundaries to match pressure data. Dong and Oliver [45] applied a quasiNewton method to history matching of 4D seismic (pwave impedance) data. Because of the large amount of data, this problem would be nearly impossible with Gauss-Newton.…”
Section: Gradient (Downhill) Methodsmentioning
confidence: 99%
“…Liu and Oliver [108] used a quasi-Newton method to adjust geologic facies boundaries to match pressure data. Dong and Oliver [45] applied a quasiNewton method to history matching of 4D seismic (pwave impedance) data. Because of the large amount of data, this problem would be nearly impossible with Gauss-Newton.…”
Section: Gradient (Downhill) Methodsmentioning
confidence: 99%
“…Two alternatives can be envisioned. The first approach encompasses a time-to-depth conversion applied to the reference seismic attributes and a comparison in depth domain (Dong and Oliver, 2005;Stephen et al, 2006;Roggero et al, 2007). With this approach, the conversion is made once and for all before the history matching process.…”
Section: Time-to-depth Conversionmentioning
confidence: 99%
“…Heterogeneous porosity and shaliness distributions are assigned to both the channel and nonchannel facies with prescribed variograms. The acoustic impedance and Poison's ratio are calculated using the same rock physics model used in [10]. The generated synthetic seismic attributes are shown in Fig.…”
Section: Examplementioning
confidence: 99%