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Rayleigh–Bénard convection

In fluid thermodynamics, Rayleigh–Bénard convection is a type of natural convection, occurring in a planar horizontal layer of fluid heated from below, in which the fluid develops a regular pattern of convection cells known as Bénard cells. Such systems were first investigated by Joseph Valentin Boussinesq and Anton Oberbeck in the 19th century. This…

History, Physical processes & History and nomenclature

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Physical processes

Rayleigh–Bénard instability

Effects of surface tension

History and nomenclature

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Rayleigh–Bénard convection

Nodes44
Edges43
Triples19
Avg. degree1.95
Density0.045455
Components1

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Rayleigh–Bénard convection

Top relations

related to history · 18
Rayleigh–Bénard convection → Bénard, Davis, French, Henri Bénard, Henri Bénard's, In, Irish-Scottish, James Thomson, John Pearson, Koschmieder, Lord Kelvin, Lord Rayleigh, Marangoni, Nonetheless, Pearson, Rayleigh, This, Those
is a · 1
Rayleigh–Bénard convection → type of natural convection

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Important terminology

convection rayleigh cells bénard temperature layer surface isbn bottom liquid top tension pattern also horizontal patterns known fluid flow conditions

Entity relationships Subject–Predicate–Object triples

SubjectPredicateObjectConfidenceSrc
Rayleigh–Bénard convectionis atype of natural convection0.90text
Rayleigh–Bénard convectionrelated to historyIn0.60section
Rayleigh–Bénard convectionrelated to historyIrish-Scottish0.60section
Rayleigh–Bénard convectionrelated to historyJames Thomson0.60section
Rayleigh–Bénard convectionrelated to historyLord Kelvin0.60section
Rayleigh–Bénard convectionrelated to historyFrench0.60section
Rayleigh–Bénard convectionrelated to historyHenri Bénard0.60section
Rayleigh–Bénard convectionrelated to historyThis0.60section
Rayleigh–Bénard convectionrelated to historyLord Rayleigh0.60section
Rayleigh–Bénard convectionrelated to historyRayleigh0.60section
Rayleigh–Bénard convectionrelated to historyThose0.60section
Rayleigh–Bénard convectionrelated to historyHenri Bénard's0.60section

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