SPE Europec/Eage Annual Conference 2012
DOI: 10.2118/154392-ms
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Assisted History-Matching for the Characterization and Recovery Optimization of Fractured Reservoirs Using Connectivity Analysis

Abstract: An integrated optimization workflow was developed to characterize seismic and sub-seismic fault networks from history-matching. A fractal model of fault networks is optimized via the gradual deformation of stochastic realizations of fault density maps, fault spatial and length distributions. In order to facilitate the history-matching, connectivity analysis tools were developed for characterizing wells-reservoir and well-to-well connectivity. Indeed these connectivity properties usually depend on the fault net… Show more

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Cited by 14 publications
(4 citation statements)
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“…where c and b are constants and d is the distance between location x and the primary-fracture plane (Dershowitz 1993). The probability-density function of the location of induced fractures is defined by…”
Section: Methodsmentioning
confidence: 99%
“…where c and b are constants and d is the distance between location x and the primary-fracture plane (Dershowitz 1993). The probability-density function of the location of induced fractures is defined by…”
Section: Methodsmentioning
confidence: 99%
“…To reduce the high computational effort required by naturally fractured reservoirs, some works proposed the streamline-based approach (Vasco et al, 1997;Bahar et al, 2003) Similarly, De Lima et al (2009) proposed the application of connectivity analysis to characterize well-reservoir and well-to-well connectivity in fractured reservoirs. Again, the authors worked only on the simulation model while we use the geological and simulation models.…”
Section: Literature Reviewmentioning
confidence: 99%
“…They used the ratio of pore volume to transmissibility between neighboring grid cells as an edge weight, which is one of Hirsch and Schuette's suggestions. This edge weight can be also interpreted as the time needed to fill the given pore volume with a fluid of unit viscosity under a unit potential difference (De Lima et al, 2012). 1The subscript and $ are the indices of grid cells, % is pore volume, ∆" is the potential difference between grid cells i and j, # is the fluid viscosity, , is the transmissibility between grid cells and $.…”
Section: Connectivity Analysismentioning
confidence: 99%