SPE Journal
Volume 14, Number 4, December 2009, pp. 746-758

SPE-110771-PA

Downscaling Multiple Seismic Inversion Constraints to Fine-Scale Flow Models

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DOI  More information 10.2118/110771-PA http://dx.doi.org/10.2118/110771-PA

Citation

  • Kalla, S., White, C.D., Gunning, J., and Glinsky, M.E. 2009. Downscaling Multiple Seismic Inversion Constraints to Fine-Scale Flow Models. SPE J.  14 (4): 746-758. SPE-110771-PA. doi: 10.2118/110771-PA.

Discipline Categories

  • 6.1.5 Geologic Modeling
  • 6.5.5 Evaluation of Uncertainties
  • 6.5.2 Construction of Static Models
  • 6.7.4 Probabilistic Methods

Summary

Well data reveal reservoir layering with high vertical resolution but are areally sparse, whereas seismic data have low vertical resolution but are areally dense. Improved reservoir models can be constructed by integrating these data. The proposed method combines stochastic seismic inversion results, finer-scale well data, and geologic continuity models to build ensembles of flow models.

Stochastic seismic inversions operating at the mesoscale generate rock property estimates, such as porosity, that are consistent with regional rock physics and true-amplitude imaged seismic data. These can be used in a cascading workflow to generate ensembles of fine-scale reservoir models wherein each realization from the Bayesian seismic inversion is treated as an exact constraint for a subensemble of fine-scale models. Exact constraints ensure that relevant interproperty and interzone correlations implied by rock physics and seismic data are preserved in the downscaled models. Uncertainty in the rock physics and seismic response is included by using multiple stochastic inversions in a cascading workflow. In contrast, inexact constraints generally do not preserve these correlations. We use two-point covariance at the fine scale to provide prior model thickness and porosity distributions of multiple facies. A Bayesian formulation uses the kriged data as the prior with the coarse constraints as the likelihood, and this posterior is sampled using a Markov Chain Monte Carlo (MCMC) method in a sequential simulation framework.

These methods generate rich pinchout behavior and flexible spatial connectivities in the fine-scale model. These flow models are easily represented on a cornerpoint grid. 2D examples illustrate the interactions of prior and constraint data, and 3D examples demonstrate algorithm performance and the effects of stratigraphic variability on flow behavior.

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History

  • Original manuscript received: 2 August 2007
  • Meeting paper published: 11 November 2007
  • Revised manuscript received: 19 June 2009
  • Manuscript approved: 16 July 2009
  • Published online: 24 September 2009
  • Version of record: 22 December 2009