http://www.cnr.it/ontology/cnr/individuo/prodotto/ID285639
Horizontal thermal convection in a shallow cavity: oscillatory regimes and transition to chaos (Articolo in rivista)
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- Label
- Horizontal thermal convection in a shallow cavity: oscillatory regimes and transition to chaos (Articolo in rivista) (literal)
- Anno
- 2000-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1108/09615530010312338 (literal)
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- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Bucchignani, E; Mansutti, D (literal)
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- Scopus (literal)
- ISI Web of Science (WOS) (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- Ctr Italiano Ric Aerospaziali; Consiglio Nazionale delle Ricerche (CNR) (literal)
- Titolo
- Horizontal thermal convection in a shallow cavity: oscillatory regimes and transition to chaos (literal)
- Abstract
- We develop a numerical analysis of the buoyancy driven natural convection of a fluid in a three dimensional shallow cavity (4.1.1) with a horizontal gradient of temperature along the larger dimension. The fluid is a liquid metal (Prandtl number equal to 0.015) while the Grashof number (Gr) varies in the range 100,000-300,000. The Navier-Stokes equations in vorticity-velocity formulation have been integrated by means of a linearized fully implicit scheme. The evaluation of fractal dimension of the attractors in the phase space has allowed the detection of the chaotic regime. The Ruelle-Takens bifurcation sequence has been observed as mechanism for the transition to chaos: the quasi periodic regime with three incommensurate frequencies is the instability mechanism responsible for the transition to chaos. Physical experiments confirm the existence of this scenario. (literal)
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