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The mixing transition in Rayleigh-Taylor instability

Author
COOK, Andrew W1 ; CABOT, William1 ; MILLER, Paul L1
[1] Lawrence Livermore National Laboratory, Livermore, CA 94550, United States
Source

Journal of Fluid Mechanics. 2004, Vol 511, pp 333-362, 30 p ; ref : 26 ref

CODEN
JFLSA7
ISSN
0022-1120
Scientific domain
Mechanics acoustics
Publisher
Cambridge University Press, Cambridge
Publication country
United Kingdom
Document type
Article
Language
English
Keyword (fr)
Couche mélange Déplacement miscible Echelle grande Fluide incompressible Instabilité Rayleigh Taylor Modélisation Méthode sous maille Simulation numérique Structure turbulence Vorticité
Keyword (en)
Mixing layer Miscible-phase displacement Large scale Incompressible fluid Rayleigh-Taylor instability Modelling Subgrid scale method Digital simulation Turbulence structure Vorticity
Keyword (es)
Capa mezcladura Escala grande Fluido incompresible Metodo submalla Estructura turbulencia
Classification
Pascal
001 Exact sciences and technology / 001B Physics / 001B40 Fundamental areas of phenomenology (including applications) / 001B40G Fluid dynamics / 001B40G20 Hydrodynamic stability / 001B40G20B Buoyancy-driven instability

Pascal
001 Exact sciences and technology / 001B Physics / 001B40 Fundamental areas of phenomenology (including applications) / 001B40G Fluid dynamics / 001B40G27 Turbulent flows, convection, and heat transfer / 001B40G27E Turbulence simulation and modeling

Pacs
4720B Buoyancy-driven instability

Pacs
4727E Turbulence simulation and modeling

Discipline
Physics : fluid mechanics
Origin
Inist-CNRS
Database
PASCAL
INIST identifier
15995774

Sauf mention contraire ci-dessus, le contenu de cette notice bibliographique peut être utilisé dans le cadre d’une licence CC BY 4.0 Inist-CNRS / Unless otherwise stated above, the content of this bibliographic record may be used under a CC BY 4.0 licence by Inist-CNRS / A menos que se haya señalado antes, el contenido de este registro bibliográfico puede ser utilizado al amparo de una licencia CC BY 4.0 Inist-CNRS

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