The onset of convective instability in a vertical porous layer with open boundaries is analysed. The base flow is partly buoyancy-induced and partly caused by an imposed vertical pressure gradient. The linearised perturbation equations expressing the local mass and energy balances, as well as the momentum balance modelled according to Darcy-Forchheimer’s law, are solved numerically in terms of normal modes. The neutral stability curves and the critical Darcy-Rayleigh number are obtained versus the form-drag parameter.

Form-drag effects on unstable buoyant flow in a vertical porous layer with open boundaries / Barletta A.; Rees D.A.S.. - ELETTRONICO. - (2017), pp. 1525-1535. (Intervento presentato al convegno International Symposium on Advances in Computational Heat Transfer, CHT 2017 tenutosi a ita nel 2017) [10.1615/ichmt.2017.1600].

Form-drag effects on unstable buoyant flow in a vertical porous layer with open boundaries

Barletta A.;
2017

Abstract

The onset of convective instability in a vertical porous layer with open boundaries is analysed. The base flow is partly buoyancy-induced and partly caused by an imposed vertical pressure gradient. The linearised perturbation equations expressing the local mass and energy balances, as well as the momentum balance modelled according to Darcy-Forchheimer’s law, are solved numerically in terms of normal modes. The neutral stability curves and the critical Darcy-Rayleigh number are obtained versus the form-drag parameter.
2017
International Symposium on Advances in Computational Heat Transfer
1525
1535
Form-drag effects on unstable buoyant flow in a vertical porous layer with open boundaries / Barletta A.; Rees D.A.S.. - ELETTRONICO. - (2017), pp. 1525-1535. (Intervento presentato al convegno International Symposium on Advances in Computational Heat Transfer, CHT 2017 tenutosi a ita nel 2017) [10.1615/ichmt.2017.1600].
Barletta A.; Rees D.A.S.
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11585/873196
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