GfsSourceTension
From Gerris
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| Revision as of 00:32, 8 August 2008 GeordieMcBain (Talk | contribs) (new page, just with <examples/> autotag) ← Previous diff |
Current revision Popinet (Talk | contribs) |
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| + | GfsSourceTension adds a surface-tension term to the momentum equations, associated with an interface defined by its volume fraction and curvature. | ||
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| + | The syntax in parameter files is: | ||
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| + | [ [[GfsSourceVelocity]] ] TRACER SIGMA KAPPA | ||
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| + | with | ||
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| + | ;<code>TRACER</code>: the name of the variable holding the volume fraction defining the interface (typically a [[GfsVariableTracerVOF]]), | ||
| + | ;<code>SIGMA</code>: the (constant) value of the surface tension coefficient, | ||
| + | ;<code>KAPPA</code>: the name of the variable holding the curvature of the interface (typically a [[GfsVariableCurvature]]). | ||
| + | |||
| <examples/> | <examples/> | ||
Current revision
GfsSourceTension adds a surface-tension term to the momentum equations, associated with an interface defined by its volume fraction and curvature.
The syntax in parameter files is:
[ GfsSourceVelocity ] TRACER SIGMA KAPPA
with
TRACER- the name of the variable holding the volume fraction defining the interface (typically a GfsVariableTracerVOF),
SIGMA- the (constant) value of the surface tension coefficient,
KAPPA- the name of the variable holding the curvature of the interface (typically a GfsVariableCurvature).
Examples
- Savart--Plateau--Rayleigh instability of a water column
- Atomisation of a pulsed liquid jet
- Air-water flow around a Series 60 cargo ship
- Circular droplet in equilibrium
- Axisymmetric spherical droplet in equilibrium
- Planar capillary waves
- Air-Water capillary wave
- Fluids of different densities
- Pure gravity wave
- Shape oscillation of an inviscid droplet
- Scalings for Plateau--Rayleigh pinchoff
- Sessile drop
- Equilibrium of a droplet suspended in an electric field
SourceTension T 1 K
SourceTension T 0.00003 K
SourceTension T -3.*(1. - RATIO) Z
SourceTension T 1 K
SourceTension T 1 K
SourceTension T 1 K
SourceTension T 1 K
SourceTension T 1 K
SourceTension {} T 45 Y
SourceTension T 1. K
SourceTension T 1. K
SourceTension T 1. K
SourceTension T 1 K

