Search results for "porous media"

showing 10 items of 25 documents

Modeling mass transfer in fracture flows with the time domain-random walk method

2019

The time domain-random walk method was developed further for simulating mass transfer in fracture flows together with matrix diffusion in surrounding porous media. Specifically, a time domain-random walk scheme was developed for numerically approximating solutions of the advection-diffusion equation when the diffusion coefficient exhibits significant spatial variation or even discontinuities. The proposed scheme relies on second-order accurate, central-difference approximations of the advective and diffusive fluxes. The scheme was verified by comparing simulated results against analytical solutions in flow configurations involving a rectangular channel connected on one side with a porous ma…

1171 GeosciencesvirtauslaskentaPOROUS-MEDIAadvection116 Chemical sciencesPorous media010103 numerical & computational mathematicsClassification of discontinuitiesPORE114 Physical scienceskulkeutuminen01 natural scienceshuokoisuusMatrix (mathematics)porous mediadiffuusio (fysikaaliset ilmiöt)Mass transfersimulointiPERMEABILITYTime domainBreakthrough curve0101 mathematicsComputers in Earth SciencesDiffusion (business)matrix diffusionPhysicsHETEROGENEOUS ROCK MATRIXHYDRODYNAMIC TRANSPORTPOROSITYSolute transportMechanicssimulationRandom walkDIFFUSIONComputer Science ApplicationsComputational MathematicsComputational Theory and MathematicsFlow (mathematics)solute transportSIMULATIONAdvectionMatrix diffusionbreakthrough curvePorous mediumComputational Geosciences
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Onset of Convection in an Inclined Anisotropic Porous Layer with Internal Heat Generation

2019

The onset of convection in an inclined porous layer which is heated internally by a uniform distribution of heat sources is considered. We investigate the combined effects of inclination, anisotropy and internal heat generation on the linear instability of the basic parallel flow. When the Rayleigh number is sufficiently large, instability occurs and a convective motion is set up. It turns out that the preferred motion at convection onset depends quite strongly on the anisotropy ratio, &xi

ConvectioninclinationMaterials scienceonsetComputingMethodologies_IMAGEPROCESSINGANDCOMPUTERVISION02 engineering and technologyanisotropylcsh:Thermodynamics01 natural sciencesInstability010305 fluids & plasmasPhysics::Fluid Dynamicsporous media0203 mechanical engineeringlcsh:QC310.15-3190103 physical sciencesAstrophysics::Solar and Stellar Astrophysicsheat generationAnisotropyconvectionlcsh:QC120-168.85Fluid Flow and Transfer ProcessesMechanical EngineeringMechanicsRayleigh numberCondensed Matter PhysicsVDP::Matematikk og Naturvitenskap: 400::Matematikk: 410Transverse plane020303 mechanical engineering & transportsTheoryofComputation_MATHEMATICALLOGICANDFORMALLANGUAGESHeat generationComputer Science::Programming Languageslcsh:Descriptive and experimental mechanicsAstrophysics::Earth and Planetary AstrophysicsInternal heatingPorous mediumFluids
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The MAST-FV/FE scheme for the simulation of thermohaline processes in variable density saturated porous media

2009

A novel methodology for the simulation of 2D thermohaline double diffusive processes, driven by heterogeneous temperature and concentration fields in variable-density satu- rated porous media, is presented. The stream function is used to describe the flow field and it is defined in terms of mass flux. The partial differential equations governing system is given by the mass conservation equation of the fluid phase written in terms of the mass- based stream function, as well as by the advection–diffusion transport equations of the contaminant concentration and of the heat. The unknown variables are the stream func- tion, the contaminant concentration and the temperature. The governing equatio…

Density driven flowFinite element methodStream functionFinite volume methodPorous mediaThermohaline processDensity driven flows thermohaline process finite volume method finite element method porous media stream functionSettore ICAR/01 - Idraulica
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The MAST-FV/FEM scheme for the simulation of thermohaline processes in density-variable saturated porous media

2008

Density driven flows thermohaline process finite volume method finite element method porous media stream function
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Simulations of single-fluid flow in porous media

1998

Several results of lattice-gas and lattice-Boltzmann simulations of single-fluid flow in 2D and 3D porous media are discussed. Simulation results for the tortuosity, effective porosity and permeability of a 2D random porous medium are reported. A modified Kozeny–Carman law is suggested, which includes the concept of effective porosity. This law is found to fit well the simulated 2D permeabilities. The results for fluid flow through large 3D random fibre webs are also presented. The simulated permeabilities of these webs are found to be in good agreement with experimental data. The simulations also confirm that, for this kind of materials, permeability depends exponentially on porosity over…

Materials sciencePoromechanicsGeneral Physics and AstronomyStatistical and Nonlinear Physicsporous mediumMechanicsTortuosityEffective porosityComputer Science ApplicationsPermeability (earth sciences)effective porosityComputational Theory and MathematicsFluid dynamicsNuclear magnetic resonance in porous mediapermeabilitytortuosityPorosityPorous mediumMathematical PhysicsInternational Journal of Modern Physics C
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Iterative momentum relaxation for fast lattice-Boltzmann simulations

2001

Abstract Lattice-Boltzmann simulations are often used for studying steady-state hydrodynamics. In these simulations, however, the complete time evolution starting from some initial condition is redundantly computed due to the transient nature of the scheme. In this article we present a refinement of body-force driven lattice-Boltzmann simulations that may reduce the simulation time significantly. This new technique is based on an iterative adjustment of the local body-force. We validate this technique on three test cases, namely fluid flow around a spherical obstacle, flow in random fiber mats and flow in a static mixer reactor.

Mathematical optimizationComputer Networks and CommunicationsComputer scienceLattice Boltzmann methodsTime evolutionPorous mediaRelaxation (iterative method)Fluid mechanicsMechanicsStatic mixerlaw.inventionMomentumFlow (mathematics)Hardware and ArchitecturelawLattice-Boltzmann methodFluid dynamicsInitial value problemFluid mechanicsPorous mediumSoftware
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Monotonic solution of flow and transport problems in heterogeneous media using Delaunay unstructured triangular meshes

2013

Transport problems occurring in porous media and including convection, diffusion and chemical reactions, can be well represented by systems of Partial Differential Equations. In this paper, a numerical procedure is proposed for the fast and robust solution of flow and transport problems in 2D heterogeneous saturated media. The governing equations are spatially discretized with unstructured triangular meshes that must satisfy the Delaunay condition. The solution of the flow problem is split from the solution of the transport problem and it is obtained with an approach similar to the Mixed Hybrid Finite Elements method, that always guarantees the M-property of the resulting linear system. The…

Mathematical optimizationFinite volume methodDiscretizationTransport problem porous media anisotropic diffusion tensor heterogeneous medium M-matrix Delaunay mesh edge swap numerical methods finite elementsDelaunay triangulationAnisotropic diffusionLinear systemMonotonic functionFinite element methodSettore ICAR/01 - IdraulicaApplied mathematicsPolygon meshWater Science and TechnologyMathematics
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A mechanical picture of fractional-order Darcy equation

2015

Abstract In this paper the authors show that fractional-order force-flux relations are obtained considering the flux of a viscous fluid across an elastic porous media. Indeed the one-dimensional fluid mass transport in an unbounded porous media with power-law variation of geometrical and physical properties yields a fractional-order relation among the ingoing flux and the applied pressure to the control section. As a power-law decay of the physical properties from the control section is considered, then the flux is related to a Caputo fractional derivative of the pressure of order 0 ⩽ β ≤ 1 . If, instead, the physical properties of the media show a power-law increase from the control sectio…

Numerical AnalysisAnomalous diffusionApplied MathematicsVolumetric fluxMass flowAnomalous diffusion; Anomalous scaling; Darcy equation; Fractional derivatives; Porous mediaMathematical analysisPorous mediaAnomalous diffusionFluxFractional derivativeViscous liquidDarcy–Weisbach equationFractional calculusModeling and SimulationDarcy equationSettore ICAR/08 - Scienza Delle CostruzioniPorous mediumAnomalous scalingMathematicsCommunications in Nonlinear Science and Numerical Simulation
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Calculation of heat and moisture distribution in the porous media layer

2007

In this paper we study the problem of the diffusion of one substance through the pores of a porous material which may absorb and immobilize some of the diffusing substances with the evolution or absorption of heat. The transfer of moisture and the heat are described by the model. The system of two partial differential equations (PDEs) is derived, one equation expresses the rate of change of concentration of water vapour in the air spaces and the other the rate of change of temperature. The obtained initial‐boundary value problem is approximated by using the finite volume method. This procedure allows us to reduce the 2D transfer problem described by a system of PDEs to initial value problem…

Partial differential equationFinite volume methodMoistureMathematical analysisModeling and SimulationOrdinary differential equationQA1-939Initial value problemDiffusion (business)Porous mediumPorosityFinite‐volume methodmathematical modelsMathematicsAnalysisporous media flowsMathematicsMathematical Modelling and Analysis
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Adiabatic eigenflows in a vertical porous channel

2014

AbstractThe existence of an infinite class of buoyant flows in a vertical porous channel with adiabatic and impermeable boundary walls, called adiabatic eigenflows, is discussed. A uniform heat source within the saturated medium is assumed, so that a stationary state is possible with a net vertical through-flow convecting away the excess heat. The simple isothermal flow with uniform velocity profile is a special adiabatic eigenflow if the power supplied by the heat source is zero. The linear stability analysis of the adiabatic eigenflows is carried out analytically. It is shown that these basic flows are unstable. The only exception, when the power supplied by the heat source is zero, is th…

PhysicsMechanical EngineeringIsothermal flowBoundary (topology)Bénard convectionMechanicsCondensed Matter PhysicsPhysics::Fluid DynamicsMechanics of MaterialsCombined forced and natural convectionconvection in porous mediaAdiabatic processbuoyancy-driven instabilityStationary stateCommunication channelRayleigh–Bénard convectionConvection cell
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