Single-phase flow through porous channels: A review of flow models and channel entry conditions
From MaRDI portal
Publication:1332373
DOI10.1016/0096-3003(94)90083-3zbMath0806.76090OpenAlexW1976962530MaRDI QIDQ1332373
Publication date: 16 February 1995
Published in: Applied Mathematics and Computation (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1016/0096-3003(94)90083-3
Related Items (6)
Single-phase flow through porous channels. II: Flow models, critical length, and viscous separation ⋮ Effect of magnetic field on the viscous fluid flow in a channel filled with porous medium of variable permeability ⋮ Analytical approach to the Darcy-Lapwood-Brinkman equation ⋮ Upstream boundary conditions for flows in porous channels ⋮ An alternative approach to exact solutions of a special class of Navier-Stokes flows ⋮ Fully developed flow through a porous channel bounded by flat plates
Cites Work
- Unnamed Item
- Unnamed Item
- Unnamed Item
- Unnamed Item
- The nondarcy regime for vertical boundary layer natural convection in a porous medium
- On macroscopic equations governing multiphase flow with diffusion and chemical reactions in porous media
- Universal formulations and comprehensive correlations for non-Darcy natural convection and mixed convection in porous media
- Thermal dispersion in a porous medium
- The Brinkman model for natural convection about a semi-infinite vertical flat plate in a porous medium
- New mathematical models of porous flow
- Boundary and inertia effects on flow and heat transfer in porous media
- Fluid flow through porous macromolecular systems
- Systems of differential equations of heat and mass transfer in capillary-porous bodies. (Review.)
- THE RANDOM-WALK MODEL WITH AUTOCORRELATION OF FLOW THROUGH POROUS MEDIA
- Study of nonlinear convection in a sparsely packed porous medium using spectral analysis
- Convective and Radiative Heat Transfer in Porous Media
- The boundary correction for the Rayleigh-Darcy problem: limitations of the Brinkman equation
- Convective flow and heat transfer in variable-porosity media
- Modelling of porous media by renormalization of the Stokes equations
- Gradient destruction in flow through a rigid matrix
- Analysis of the Brinkman equation as a model for flow in porous media
- A periodic grain consolidation model of porous media
- Finite-amplitude cellular convection in a fluidsaturated porous layer
- Drag due to the motion of a Newtonian fluid through a sparse random array of small fixed rigid objects
- A boundary-layer model of flow in a porous medium at high Rayleigh number
- Constitutive equations for flow of an incompressible viscous fluid through a porous medium
- The drag on a cloud of spherical particles in low Reynolds number flow
- Slow flow through stationary random beds and suspensions of spheres
- Non-Darcy flow behavior in liquid-saturated porous media
- A calculation of the viscous force exerted by a flowing fluid on a dense swarm of particles
This page was built for publication: Single-phase flow through porous channels: A review of flow models and channel entry conditions
