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Stability of Flow of a Variable-Viscosity Fluid Saturating a Differentially Heated Vertical Porous Layer

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Abstract

The effect of viscosity varying linearly with temperature and the Prandtl–Darcy number on the stability of buoyancy-driven convection in a vertical porous layer is investigated. The variation in viscosity causes a dramatic change in the base flow and thereby discards the analytical proof of stability even under the limit of an infinite Prandtl–Darcy number. The question about the stability/instability of the basic flow is thus examined by carrying out a numerical solution of the stability eigenvalue problem for infinite and finite values of the Prandtl–Darcy number. It is found that the linear temperature dependence of the viscosity does not activate the instability to small-amplitude disturbances.

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References

  • Barletta, A.: A proof that convection in a porous vertical slab may be unstable. J. Fluid Mech. 770, 273–288 (2015)

    Article  Google Scholar 

  • Barletta, A., Nield, D.A.: Variable viscosity effects on the dissipation instability in a porous layer with horizontal throughflow. Phys. Fluids 24, 104102 (2012)

    Article  Google Scholar 

  • Gill, A.E.: A proof that convection in a porous vertical slab is stable. J. Fluid Mech. 35, 545–547 (1969)

    Article  Google Scholar 

  • Honda, S., Iwase, Y.: Comparison of the dynamic and parameterized models of mantle convection including core cooling. Earth Planet. Sci. Lett. 139, 133–145 (1996)

    Article  Google Scholar 

  • Kwok, L.P., Chen, C.F.: Stability of thermal convection in a vertical porous layer. J. Heat Transf. 109, 889–893 (1987)

    Article  Google Scholar 

  • Nield, D.A., Bejan, A.: Convection in Porous Media, 5th edn. Springer, New York (2017)

    Book  Google Scholar 

  • Rees, D.A.S.: The stability of Prandtl–Darcy convection in a vertical porous layer. Int. J. Heat Mass Transf. 31, 1529–1534 (1988)

    Article  Google Scholar 

  • Rees, D.A.S.: The effect of local thermal nonequilibrium on the stability of convection in a vertical porous channel. Transp. Porous Med. 87, 459–464 (2011)

    Article  Google Scholar 

  • Rossby, H.T.: A study of Bénard convection with and without rotation. J. Fluid Mech. 36, 309–335 (1969)

    Article  Google Scholar 

  • Scott, N.L., Straughan, B.: A nonlinear stability analysis of convection in a porous vertical channel including local thermal nonequilibrium. J. Math. Fluid Mech. 15, 171–178 (2013)

    Article  Google Scholar 

  • Shankar, B.M., Shivakumara, I.S.: On the stability of natural convection in a porous vertical slab saturated with an Oldroyd-B fluid. Theor. Comput. Fluid Dyn. 31, 221–231 (2017)

    Article  Google Scholar 

  • Shankar, B.M., Shivakumara, I.S.: Gill’s stability problem may be unstable with horizontal heterogeneity in permeability. J. Fluid Mech. 943, A20 (2022)

    Article  Google Scholar 

  • Shankar, B.M., Kumar, J., Shivakumara, I.S.: Magnetohydrodynamic instability of mixed convection in a differentially heated vertical channel. Eur. Phys. J. Plus 134, 53 (2019)

    Article  Google Scholar 

  • Shankar, B.M., Naveen, S.B., Shivakumara, I.S.: Stability of double-diffusive natural convection in a vertical porous layer. Transp. Porous Med. 141, 87–105 (2022)

    Article  Google Scholar 

  • Straughan, B.: A nonlinear analysis of convection in a porous vertical slab. Geophys. Astrophys. Fluid Dyn. 42, 269–275 (1988)

    Article  Google Scholar 

  • Walzer, U., Hendel, R.: A new convection-fractionation model for the evolution of the principal geochemical reservoirs of the Earth’s mantle. Phys. Earth Planet. Inter. 112, 211–256 (1999)

    Article  Google Scholar 

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Acknowledgements

We are indebted to three anonymous referees for thoroughly reading the manuscript and for indicating several points which have led to substantial improvements in the work.

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Shankar, B.M., Nagamani, K.V. & Shivakumara, I.S. Stability of Flow of a Variable-Viscosity Fluid Saturating a Differentially Heated Vertical Porous Layer. Transp Porous Med 150, 1–14 (2023). https://doi.org/10.1007/s11242-023-01975-9

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