North Sea Oil and Gas Reservoirs — III 1994
DOI: 10.1007/978-94-011-0896-6_18
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What Reservoir Characterisation is Required for Predicting Waterflood Performance in a High Net-to-Gross Fluvial Environment?

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Cited by 34 publications
(43 citation statements)
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“…Alternations of parallel, continuous layers of different lithologic and physical properties are a ubiquitous type of geologic heterogeneity observed at many different length scales, including lamination (millimeter-thick layers), bedding (centimeter-to meter-thick layers) and laterally extensive genetic and stratigraphic units that may correspond to flow zones in groundwater aquifers and hydrocarbon reservoirs, typically several meters to tens of meters in thickness (e.g., Campbell 1967;Ringrose et al 1993a, b;Jones et al 1994Jones et al , 1995Koltermann and Gorelick 1996;Marsily et al 1998;White and Barton 1999;Li and White 2003;Jackson et al 2003;Deveugle et al 2011). Understanding multiphase flow in layered porous media is therefore important for accurate prediction of many subsurface processes; examples include geologic carbon storage, migration of non-aqueous phase liquids (NAPLs) in contaminated aquifers and hydrocarbon production.…”
Section: Introductionmentioning
confidence: 99%
“…Alternations of parallel, continuous layers of different lithologic and physical properties are a ubiquitous type of geologic heterogeneity observed at many different length scales, including lamination (millimeter-thick layers), bedding (centimeter-to meter-thick layers) and laterally extensive genetic and stratigraphic units that may correspond to flow zones in groundwater aquifers and hydrocarbon reservoirs, typically several meters to tens of meters in thickness (e.g., Campbell 1967;Ringrose et al 1993a, b;Jones et al 1994Jones et al , 1995Koltermann and Gorelick 1996;Marsily et al 1998;White and Barton 1999;Li and White 2003;Jackson et al 2003;Deveugle et al 2011). Understanding multiphase flow in layered porous media is therefore important for accurate prediction of many subsurface processes; examples include geologic carbon storage, migration of non-aqueous phase liquids (NAPLs) in contaminated aquifers and hydrocarbon production.…”
Section: Introductionmentioning
confidence: 99%
“…1, none of the coarse-grid lines of the uniform 10 × 4 model (case [1]) coincides with the lens boundary, which makes it a bad model for upscaling. However, it is possible to reduce homogenization error by adjusting grid lines of case [1] (without changing its dimension) in order to align (all or some of) them with lens boundaries. Definitely, case [2] which covers all permeability variation boundaries is a perfect model with no homogenization error.…”
Section: Lens Modelmentioning
confidence: 98%
“…For case (1), since there is no flow in the region, then flow calculations are not necessary by the flow simulator and a coarse grid would suffice. If case (2) exits, then we have a homogeneous region and this area can be coarsened.…”
Section: Application To Irrotational Flowsmentioning
confidence: 99%
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