Rayleigh–Bénard convection

E350921

Rayleigh–Bénard convection is a fluid dynamics phenomenon in which a horizontal fluid layer heated from below develops organized convection cells due to buoyancy-driven instability.

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All labels observed (3)

Statements (49)

Predicate Object
instanceOf fluid dynamics phenomenon
hydrodynamic instability
thermal convection
applicationArea astrophysical convection
atmospheric convection
industrial heat transfer
mantle convection
assumes Boussinesq approximation
canBecome turbulent convection
characterizedBy buoyancy-driven instability
cellular flow patterns
organized convection cells
pattern formation
dependsOn fluid viscosity
gravity
layer thickness
thermal diffusivity
thermal expansion coefficient
drivenBy buoyancy forces
temperature gradient
exhibits hexagonal patterns
roll patterns
spiral defect chaos
governedBy Navier–Stokes equations
heat equation
hasAlternativeName Rayleigh–Bénard convection
surface form: Bénard convection

Rayleigh–Bénard convection
surface form: Rayleigh-Bénard convection
hasCriticalRayleighNumber approximately 1708 for free-free boundaries in a simple model
hasParameter Nusselt number
Prandtl number
Rayleigh number
isExampleOf dissipative structure
far-from-equilibrium thermodynamics
spontaneous symmetry breaking
leadsTo heat transport enhancement
transition from conduction to convection
lowerBoundary hotter plate
namedAfter Henri Bénard
Lord Rayleigh
occursIn finite layer between two horizontal plates
horizontal fluid layer
viscous fluid
onsetCondition Rayleigh number exceeds critical value
requires cooling from above
heating from below
studiedIn nonlinear dynamics
pattern formation theory
turbulence research
upperBoundary cooler plate

Referenced by (3)

Full triples — surface form annotated when it differs from this entity's canonical label.

Schwarzschild criterion relatedTo Rayleigh–Bénard convection
Rayleigh–Bénard convection hasAlternativeName Rayleigh–Bénard convection
this entity surface form: Bénard convection
Rayleigh–Bénard convection hasAlternativeName Rayleigh–Bénard convection
this entity surface form: Rayleigh-Bénard convection