Pages that link to "Item:Q1811691"
From MaRDI portal
The following pages link to On the stability of thermally driven shear flow of an Oldroyd-B fluid heated from below (Q1811691):
Displaying 6 items.
- Stability of thermal convection of an Oldroyd-B fluid in a porous medium with Newtonian heating (Q418597) (← links)
- Convective flow in a horizontal channel with non-Newtonian surface rheology under time-dependent longitudinal temperature gradient (Q893527) (← links)
- Stability of an oscillatory shear flow in a differentially heated vertical channel (Q978319) (← links)
- Linear and weakly nonlinear analysis of a ferrofluid layer for an LTNE model with variable gravity and internal heat source (Q2212097) (← links)
- Bio‐thermal convection caused by combined effects of swimming of oxytactic bacteria and inclined temperature gradient in a shallow fluid layer (Q3113102) (← links)
- Linear and nonlinear stability analyses of thermal convection for Oldroyd-B fluids in porous media heated from below (Q5304099) (← links)
