Title: Convective Instability in quasi 2D foams
1Convective Instabilityin quasi 2D foams
Eric Janiaud, Stefan Hutzler, Denis
Weaire. Trinity College, Dublin
janiaude_at_tcd.ie
2Convection in (3d) foams
- Add liquid on top of a foam
- if Qgt Threshold plastic flow of bubbles.
L. Alonso
3Analogy with Thermal convection
???
Damping
4Difference with Thermal convection
- Heat diffusion
- Gaussian
- continuous media
- Newtonian liquid
- Liquid diffusion
- non linear(chemistry)
- Discrete network
- Yield stressdilatency
Ra FArchimede/ Fviscosity
Nu Qconvection /Qno convection
?
Pr Dmvt / Dheat
Pe Tdiffusion / Tconvection
5Issues
- Mix Rheology and drainage
- Onset
- dilatency, surfactants, bubble size, ?
gradient... - After the onset
- Shear bands, efficiency on liquid transport,
size sorting...
6From 3D to 2D...
Film
Vertex decorated
Pseudo Plateau Border
Drainage is possible !
No liquid flow between vertex
7Quasi 2D foams in Hele-Shaw cell
8What is the Volume fraction?
- Wetting Plateau border
- VR2L
- Film
- VL2e
- Perpendicular
- Plateau border
- VR2d
- Vertices
- VR3
Cox
Needs experiments and Evolver Simulations
9Hele-Shaw Cell setup
- Sensitive to the wetting film
- Bidisperse foam
- Area 90 and 130 pixel
Q
Projector
10Steady state Drainage
- Injection point
- Uniform free convection
- Local forced convection
What is the caracteristic length for roll?
What is the solution to the drainage equation?
11Local injection
Q
12Vertical Velocity
3 pictures
Velocity (pi/s)
Horizontal coordinate (pi)
Smooth profile No shear Band
13Non uniform liquid Fraction
How to measure the volume fraction?
14Image Analysis Vertices
Velocity tracking bubbles T1 neighbourhood
relations Local Volume fraction ration of
Pixel Stress/Strain field Vertex
position Capillary pressure curvature measurement
15Plugin for ImageJ
- Public/free Java software
- developed by the NIH
- Object oriented
- easy implementation
- Already rich
- Multiplatform
16Perspectives
- Forced 2D convection
- impose and measure ?
- measure the velocity field
- Free 2D convection
- homogenous liquid input !!!
- boundary conditions !!!
- destabilisation length?
- Back to 3D convection