Natural convection in partially porous media: a brief overview
From MaRDI portal
Publication:3113056
DOI10.1108/09615530810853682zbMath1231.76309OpenAlexW2067755328MaRDI QIDQ3113056
Publication date: 7 February 2012
Published in: International Journal of Numerical Methods for Heat & Fluid Flow (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1108/09615530810853682
Lua error in Module:PublicationMSCList at line 37: attempt to index local 'msc_result' (a nil value).
Related Items (3)
Flow currents and ventilation in Langstroth beehives due to brood thermoregulation efforts of honeybees ⋮ Сопряженный расчет течений в областях, содержащих пористое тело и свободный поток ⋮ Natural convection in fluid-superposed porous layers heated locally from below
Uses Software
Cites Work
- Linear stability of natural convection in superposed fluid and porous layers: influence of the interfacial modelling
- Convective heat and solute transfer in partially porous cavities
- Slip and no-slip velocity boundary conditions at interface of porous, plain media
- Momentum transfer at the boundary between a porous medium and a homogeneous fluid. I: Theoretical development. II: Comparison with experiment
- Analytical investigation of Couette flow in a composite channel partially filled with a porous medium and partially with a clear fluid
- A model for convection in the evolution of under-ice melt ponds
- Momentum transport at a fluid-porous interface.
- Non-Darcy effects in buoyancy driven flows in an enclosure filled with vertically layered porous media
- Flow at the interface of a model fibrous porous medium
- On the Boundary Condition at the Surface of a Porous Medium
- Viscosity renormalization in the Brinkman equation
- Stability of natural convection in superposed fluid and porous layers: Influence of the interfacial jump boundary condition
- The boundary correction for the Rayleigh-Darcy problem: limitations of the Brinkman equation
- Microscopic flow near the surface of two-dimensional porous media. Part 1. Axial flow
- Microscopic flow near the surface of two-dimensional porous media. Part 2. Transverse flow
- Natural convection in vertical enclosures containing simultaneously fluid and porous layers
- Viscosity of concentrated suspensions of aggregable particles
- Velocity measurements of a shear flow penetrating a porous medium
- On The Interface Boundary Condition of Beavers, Joseph, and Saffman
- Penetrative convection in a superposed porous-mediumfluid layer via internal heating
- Computer simulation study of the effective viscosity in Brinkman’s equation
- Sur une solution exacte de la convection naturelle en cavité partiellement remplie d'un milieu poreux
- Slow flow through stationary random beds and suspensions of spheres
- A model for the boundary condition of a porous material. Part 2
- A model for the boundary condition of a porous material. Part 1
- A calculation of the viscous force exerted by a flowing fluid on a dense swarm of particles
- Stability analysis of double-diffusive convection in superposed fluid and porous layers using a one-equation model.
This page was built for publication: Natural convection in partially porous media: a brief overview
