Convection in Fluids pp 85-132 | Cite as
The Bénard (1900, 1901) Convection Problem, Heated from below
In this chapter, we take into account the influence of a deformable free surface and, as a consequence, we revisit the mathematical formulation of the classical problem describing the Bénard instability of a horizontal layer of fluid, heated from below, and bounded by an upper deformable free surface. Because the deformation of the free surface, subject to a temperature-dependent surface tension, is taken into account in the full Bénard convection problem, heated from below, we have not specified this convection as being a ‘thermal convection’.
- (a)
the conduction adverse temperature gradient (Bénard) effect in motionless steady-state conduction temperature
- (b)
the temperature-dependent surface tension (Marangoni) effect
- (c)
the heat flux across the upper, free surface (Biot) effect
- (d)
the buoyancy (Archimedean—Boussinesq) effect arising from the volume (gravity) forces.
Keywords
Free Surface Liquid Layer Froude Number Biot Number Dimensionless TemperaturePreview
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