Research Article
Lattice Boltzmann Simulations of Fluid Flow in Continental Carbonate Reservoir Rocks and in Upscaled Rock Models Generated with Multiple-Point Geostatistics
Figure 16
Computer-generated models of a reed facies sample with different σ values, which controls the level of conditioning data used. (a) No conditioning data; (b) σ = 0.75; (c) σ = 0.50; and (d) the largest amount of conditioning data with σ = 0.25 (colors indicate connectivity). The more the conditioning data approaches the “truth,” the more the simulated permeability approaches the laboratory measured permeability.
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