Two- and Three-Dimensional Absolute Instabilities in a Porous Medium with Inclined Temperature Gradient and Vertical Throughflow
Autor: | Leonardo S. de B. Alves, Mateus Schuabb, S. C. Hirata |
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Přispěvatelé: | Unité de Mécanique de Lille - ULR 7512 (UML), Université de Lille |
Rok vydání: | 2020 |
Předmět: |
Physics
Throughflow Work (thermodynamics) General Chemical Engineering 0208 environmental biotechnology 02 engineering and technology Mechanics Péclet number 010502 geochemistry & geophysics 01 natural sciences Instability Catalysis 020801 environmental engineering Temperature gradient symbols.namesake Convective instability Combined forced and natural convection Saddle point symbols [PHYS.MECA.MEFL]Physics [physics]/Mechanics [physics]/Fluid mechanics [physics.class-ph] ComputingMilieux_MISCELLANEOUS 0105 earth and related environmental sciences |
Zdroj: | Transport in Porous Media Transport in Porous Media, 2020, 132 (1), pp.135-155. ⟨10.1007/s11242-020-01383-3⟩ |
ISSN: | 1573-1634 0169-3913 |
Popis: | A linear stability analysis for the onset of mixed convection in a saturated porous medium through an absolute instability of both two- and three-dimensional disturbances is performed. Relevant control parameters associated with the inclined temperature gradient and the vertical throughflow are the vertical and horizontal Rayleigh numbers, $$R_{\mathrm{v}}$$ and $$R_{\mathrm{h}}$$, and the vertical Peclet number, $$Q_{\mathrm{v}}$$, respectively. This work extends previous studies on the very same problem in two fronts. For two-dimensional disturbances, the present results do not agree with the literature for a few of the parametric conditions reported. This is caused by the collision of the convectively unstable downstream propagating branch with multiple upstream propagating branches, which generates several saddle points and, hence, makes the identification of the correct pinching point more difficult. In other words, literature results are all saddle points but not always pinching points. For three-dimensional disturbances, this issue is not present and the current results agree with the literature. On the other hand, due to the inherent difficulties associated with a three-dimensional absolute instability analysis, literature results have only been able to report the group velocities at the onset of convective instability. When their real parts are zero, transition occurs directly from stable to absolutely unstable. Otherwise, transition occurs from stable to convectively unstable first and nothing can be said about the onset of absolute instability. In this work, a novel technique recently developed by the authors allowed the identification of the onset of absolute instability under all parametric conditions investigated in the literature, extending earlier results. Doing so confirmed the dichotomy already observed in these earlier studies, i.e., the onset of absolute instability for two- and three-dimensional longitudinal modes indeed differs. |
Databáze: | OpenAIRE |
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