On natural convection in vertical porous enclosures due to prescribed fluxes of heat and mass at the vertical boundaries

Lua error in Module:PublicationMSCList at line 37: attempt to index local 'msc_result' (a nil value).

Related Items (14)

Numerical simulation of double-diffusion driven convective flow and rock alteration in three-dimensional fluid-saturated geological fault zones ⋮ Numerical simulation of three-dimensional double-diffusive natural convection in porous media by boundary element method ⋮ Magnetic field effect on Soret driving free convection in an inclined porous cavity saturated by a conducting binary mixture ⋮ Unicellular natural circulation in a shallow horizontal porous layer heated from below by a constant flux ⋮ Boundary domain integral method for the study of double diffusive natural convection in porous media ⋮ Onset of stationary and oscillatory convection in a tilted porous cavity saturated with a binary fluid: Linear stability analysis ⋮ Nonlinear doubly diffusive convection in vertical enclosures ⋮ Double diffusion-driven convective instability of three-dimensional fluid-saturated geological fault zones heated from below ⋮ Double diffusion natural convection in a rectangular enclosure filled with binary fluid saturated porous media: The effect of lateral aspect ratio ⋮ Thermo-Solutal Natural Convection in an Anisotropic Porous Enclosure Due to Non-Uniform Temperature and Concentration at Bottom Wall ⋮ Finite element modelling of flow, heat and mass transfer in fluid-saturated porous media ⋮ Analytical and numerical study of natural convection induced by a volumetric heat generation in inclined cavities asymmetrically cooled by heat fluxes ⋮ The Soret effect on convection in a horizontal porous domain under cross temperature and concentration gradients ⋮ Numerical modelling of double diffusion driven reactive flow transport in deformable fluid‐saturated porous media with particular consideration of temperature‐dependent chemical reaction rates

This page was built for publication: On natural convection in vertical porous enclosures due to prescribed fluxes of heat and mass at the vertical boundaries