Physical Review E · 2005 · 11 citations · 13 references
EngineeringMaterials EngineeringMaterials ScienceComputational Materials ScienceSubsurface Fluid FlowTransport PhenomenaFluid-flow In Porous MediaPorous MaterialsPorous Media FlowTransport In Porous MediaTransport Property SimulationDiffusion Coefficient CalculationDiffusion CoefficientsFinite Difference SchemesLattice Boltzmann SimulationPorous MediaRandom Walk AlgorithmsTransport Phenomena In Porous MaterialsTransport Properties In Porous Media
Time-dependent diffusion simulations which can be measured by nuclear magnetic resonance (NMR) were numerically performed in consolidated reconstructed porous media saturated by two immobile fluids. The phase distributions were obtained by an immiscible lattice Boltzmann technique which incorporates interfacial tension and wetting. The apparent diffusion coefficient in each fluid was determined by a random walk algorithm. Permeability and conductivity tensors were calculated by finite-difference schemes. The major properties valid for a single phase could be generalized to two phases. First, the characteristic length Lambda introduced by Johnson et al.[Phys. Rev. Lett. 57, 2564 (1986)] is of the order of twice the phase volume to surface ratio. Second, the apparent diffusion coefficients for all porosities, saturations, and phases can be represented by a single dimensionless curve.
13
Grain reconstruction of porous media: Application to a low-porosity Fontainebleau sandstone
Jean‐François Thovert, F. Yousefian, P. Spanne et al. · Physical review. E, Statistical physics, plasmas, fluids, and related interdisciplinary topics · 2001 · 152 citations
Engineering, Earth Sciences, Geology +17