Pages that link to "Item:Q1315784"

The following pages link to The Brinkman model for natural convection in a porous layer: Effects of nonuniform thermal gradient (Q1315784):

Displaying 14 items.

• Onset of convection in a couple-stress fluid-saturated porous medium: effects of non-uniform temperature gradients (Q363158) (← links)
• Exact solutions for equations of flow and heat transfer in fluid saturated porous media (Q497028) (← links)
• Natural convection in a shallow porous cavity - The Brinkman model (Q581153) (← links)
• Porous media convection between vertical walls: continuum of solutions from capped to open ends (Q954242) (← links)
• The Brinkman model for natural convection about a semi-infinite vertical flat plate in a porous medium (Q1064933) (← links)
• The effect of thermal stratification on natural convection in a vertical porous insulation layer (Q1276656) (← links)
• A bifurcation study of natural convection in porous media with internal heat sources: The non-Darcy effects (Q1287833) (← links)
• The onset of Darcy-Brinkman convection in a porous layer: An asymptotic analysis (Q1614553) (← links)
• Thermal convection in an inclined porous layer with Brinkman law (Q1623078) (← links)
• Convection induced by the selective absorption of radiation for the Brinkman model (Q1876031) (← links)
• The effect of a nonuniform basic temperature gradient on the convective instability of a fluid-saturated porous layer with general velocity and thermal conditions (Q1977058) (← links)
• Importance of Darcy or Brinkman laws upon resonance in thermal convection (Q2374344) (← links)
• Linear stability of natural convection in a multilayer system of fluid and porous layers with internal heat sources (Q2393316) (← links)
• The effect of non-uniform basic temperature gradient on the convective instability of a fluid layer sandwiched between two porous layers with general velocity and thermal conditions (Q2730890) (← links)