Skip to main content
Log in

Instability of fully developed mixed convection with viscous dissipation in a vertical porous channel

  • Published:
Transport in Porous Media Aims and scope Submit manuscript

Abstract

Flow driven by an externally imposed pressure gradient in a vertical porous channel is analysed. The combined effects of viscous dissipation and thermal buoyancy are taken into account. These effects yield a basic mixed convection regime given by dual flow branches. Duality of flow emerges for a given vertical pressure gradient. In the case of downward pressure gradient, i.e. upward mean flow, dual solutions coincide when the intensity of the downward pressure gradient attains a maximum. Above this maximum no stationary and parallel flow solution exists. A nonlinear stability analysis of the dual solution branches is carried out limited to parallel flow perturbations. This analysis is sufficient to prove that one of the dual solution branches is unstable. The evolution in time of a solution in the unstable branch is also studied by a direct numerical solution of the governing equation.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7

Similar content being viewed by others

References

  • Barletta, A., Miklavčič, M.: On fully developed mixed convection with viscous dissipation in a vertical channel and its stability. Z. Angew. Math. Mech. 96, 1457–1466 (2016)

    Article  Google Scholar 

  • Barletta, A., Magyari, E., Keller, B.: Dual mixed convection flows in a vertical channel. Int. J. Heat Mass Transf. 48, 4835–4845 (2005)

    Article  Google Scholar 

  • Barletta, A., Magyari, E., Pop, I., Storesletten, L.: Mixed convection with viscous dissipation in a vertical channel filled with a porous medium. Acta Mech. 194, 123–140 (2007)

    Article  Google Scholar 

  • Barletta, A., Lazzari, S., Magyari, E.: Buoyant Poiseuille–Couette flow with viscous dissipation in a vertical channel. Z. Angew. Math. Physik 59, 1039–1056 (2008)

    Article  Google Scholar 

  • Barletta, A.: Local energy balance, specific heats and the Oberbeck–Boussinesq approximation. Int. J. Heat Mass Transf. 52, 5266–5270 (2009)

    Article  Google Scholar 

  • Barletta, A.: On the thermal instability induced by viscous dissipation. Int. J. Therm. Sci. 88, 238–247 (2015)

    Article  Google Scholar 

  • Barletta, A., Rees, D.A.S.: Stability analysis of dual adiabatic flows in a horizontal porous layer. Int. J. Heat Mass Transf. 52, 2300–2310 (2009)

    Article  Google Scholar 

  • Barletta, A., Zanchini, E.: On the choice of the reference temperature for fully-developed mixed convection in a vertical channel. Int. J. Heat Mass Transf. 42, 3169–3181 (1999)

    Article  Google Scholar 

  • Celli, M., Alves, L.S. de B., Barletta, A.: Nonlinear stability analysis of Darcy’s flow with viscous heating. Proc. R. Soc. A 472, 20160036 (2016)

  • Henry, D.: Geometric Theory of Semilinear Parabolic Equations. Springer, Berlin (1981)

    Book  Google Scholar 

  • Joseph, D.D.: Variable viscosity effects on the flow and stability of flow in channels and pipes. Phys. Fluids 7, 1761–1771 (1964)

    Article  Google Scholar 

  • Joseph, D.D.: Stability of frictionally-heated flow. Phys. Fluids 8, 2195–2200 (1965)

    Article  Google Scholar 

  • Miklavčič, M.: Applied Functional Analysis and Partial Differential Equations. World Scientific Publishing Co., Inc., River Edge (1998)

    Google Scholar 

  • Miklavčič, M.: Stability analysis of some fully developed mixed convection flows in a vertical channel. Z. Angew. Math. Mech. 95, 982–986 (2015)

    Article  Google Scholar 

  • Miklavčič, M., Wang, C.Y.: Completely passive natural convection. Z. Angew. Math. Mech. 91, 601–606 (2011)

    Article  Google Scholar 

  • Nield, D.A., Barletta, A., Celli, M.: The effect of viscous dissipation on the onset of convection in an inclined porous layer. J. Fluid Mech. 679, 544–558 (2011)

    Article  Google Scholar 

  • Nield, D.A., Bejan, A.: Convection in Porous Media, 4th edn. Springer, New York (2013)

    Book  Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to A. Barletta.

Appendix

Appendix

If we multiply Eq. (8a) by \(T'\) and integrate, we obtain

$$\begin{aligned} \frac{1}{2}\left( \frac{\mathrm{d}T}{\mathrm{d}y} \right) ^2 + \frac{1}{3}\left( T-T_m-P \right) ^3= \frac{1}{3}\left[ T(0)-T_m-P \right] ^3, \end{aligned}$$
(17)

after noting that \(T'(0)=0\). If we use Eq. (17) and scale with \(T(0)-T_m-P\), we obtain two branches.

When \(T(0)-T_m-P>0\), one can describe T parametrically as follows:

$$\begin{aligned} T(y)=6s^2[\varphi (s)^2-\varphi (s|y|)^2], \end{aligned}$$
(18)

where \(0\le s<s_\mathrm{max}=\int _0^\infty (3-3x^2+x^4)^{-1/2}\mathrm{d}x=2.103\) and \(\varphi \) is defined on \([0,s_\mathrm{max})\) by

$$\begin{aligned} \varphi '=\sqrt{3-3\varphi ^2+\varphi ^4},\quad \varphi (0)=0. \end{aligned}$$
(19)

In this case

$$\begin{aligned} T(0)= & {} 6s^2\varphi (s)^2,\quad P=-6s^2+6s\int _0^s \varphi (x)^2\,\mathrm{d}x,\nonumber \\ T_m= & {} 6s^2\varphi (s)^2-6s\int _0^s \varphi (x)^2\,\mathrm{d}x. \end{aligned}$$
(20)

These solutions make up the entire upper branch in Fig. 1 and the piece between C and A on the lower branch.

When \(T(0)-T_m-P<0\) one can describe T parametrically as follows:

$$\begin{aligned} T(y)=6s^2[\psi (s)^2-\psi (s|y|)^2], \end{aligned}$$
(21)

where \(0\le s<z_\mathrm{max}=\int _0^\infty (3+3x^2+x^4)^{-1/2}\mathrm{d}x=1.214\) and \(\psi \) is defined on \([0,z_\mathrm{max})\) by

$$\begin{aligned} \psi '=\sqrt{3+3\psi ^2+\psi ^4},\quad \psi (0)=0. \end{aligned}$$
(22)

In this case

$$\begin{aligned} T(0)= & {} 6s^2\psi (s)^2,\nonumber \\ P= & {} 6s^2+6s\int _0^s \psi (x)^2\,\mathrm{d}x,\nonumber \\ T_m= & {} 6s^2\psi (s)^2-6s\int _0^s \psi (x)^2\,\mathrm{d}x. \end{aligned}$$
(23)

These solutions make up the lower branch in Fig. 1 without the piece between C and A.

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Barletta, A., Miklavčič, M. Instability of fully developed mixed convection with viscous dissipation in a vertical porous channel. Transp Porous Med 117, 337–347 (2017). https://doi.org/10.1007/s11242-017-0836-x

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s11242-017-0836-x

Keywords

Navigation