Onset of instability in Hadley–Prats flow in a weakly heterogeneous porous layer with viscous dissipation

2021 ◽  
Vol 33 (8) ◽  
pp. 084110
Author(s):  
Kamalika Roy
Keyword(s):  
Viscous Dissipation ◽  
Porous Layer

Darcy–Forchheimer Flow With Viscous Dissipation in a Horizontal Porous Layer: Onset of Convective Instabilities

2009 ◽  
Vol 131 (7) ◽  
Author(s):  
A. Barletta ◽  
M. Celli ◽  
D. A. S. Rees
Keyword(s):  
Boundary Condition ◽  
Viscous Dissipation ◽  
Porous Layer ◽  
Linear Equations ◽  
Orientation Angle ◽  
Base Flow ◽  
Neutral Stability ◽  
Governing Parameter ◽  
Bottom Boundary ◽  
Forchheimer Flow

Parallel Darcy–Forchheimer flow in a horizontal porous layer with an isothermal top boundary and a bottom boundary, which is subject to a third kind boundary condition, is discussed by taking into account the effect of viscous dissipation. This effect causes a nonlinear temperature profile within the layer. The linear stability of this nonisothermal base flow is then investigated with respect to the onset of convective rolls. The third kind boundary condition on the bottom boundary plane may imply adiabatic/isothermal conditions on this plane when the Biot number is either zero (adiabatic) or infinite (isothermal). The solution of the linear equations for the perturbation waves is determined by using a fourth order Runge–Kutta scheme in conjunction with a shooting technique. The neutral stability curve and the critical value of the governing parameter R=GePe2 are obtained, where Ge is the Gebhart number and Pe is the Péclet number. Different values of the orientation angle between the direction of the basic flow and the propagation axis of the disturbances are also considered.

scholarly journals Convective Roll Instabilities of Vertical Throughflow with Viscous Dissipation in a Horizontal Porous Layer

2009 ◽  
Vol 81 (3) ◽  
pp. 461-477 ◽  
Author(s):  
Antonio Barletta ◽  
Eugenia Rossi di Schio ◽  
Leiv Storesletten
Keyword(s):  
Viscous Dissipation ◽  
Porous Layer ◽  
Convective Roll ◽  
Vertical Throughflow
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