Upload
niran
View
43
Download
0
Embed Size (px)
DESCRIPTION
Wetting as a Macroscopic and Microscropic Process. J.E. Sprittles (University of Birmingham / Oxford, U.K.) Y.D. Shikhmurzaev(University of Birmingham, U.K.) Seminar at KAUST, February 2012. ‘Impact’ . A few years after completing my PhD. Wetting: Statics. Wettable (Hydrophilic). - PowerPoint PPT Presentation
Citation preview
Wetting as a Macroscopic and Microscropic ProcessJ.E. Sprittles (University of Birmingham / Oxford, U.K.)Y.D. Shikhmurzaev (University of Birmingham, U.K.)
Seminar at KAUST, February 2012
‘Impact’ A few years after completing my PhD.....
Wetting: Statics
Non-Wettable (Hydrophobic)Wettable (Hydrophilic)e e
Wetting: Dynamics
( )h t
Capillary Rise
50nm x 900nm ChannelsHan et al 06
27mm Radius TubeStange et al 03
1 Million Orders of Magnitude!!
Polymer-Organic LED (P-OLED) Displays
Inkjet Printing of P-OLED Displays
Microdrop Impact & Spreading
Modelling: Why Bother?1 - Recover Hidden Information
2 - Map Regimes of Spreading
3 – Experiment
Millimetres in Milliseconds - Rioboo et al (2002)
Microns in Microseconds - Dong et al (2002)
Flow Inside Solids – Marston et al 2010
r
Pasandideh-Fard et al 1996
Dynamic Contact AngleRequired as a boundary condition for the free surface shape.
r
t
d( )d f t
d e
Speed-Angle Formulae
dθ = ( )f U
e1 3 2cose e e e
R
σ1
σ3 - σ2
Young Equation Dynamic Contact Angle Formula
)
θdU
Assumption:A unique angle for each speed
( )d f U
Drop Impact Experiments
10.18ms
10.25ms
)
Ud
-1(ms )U
d 30d Bayer & Megaridis 06
d ( )f U
Capillary Rise Experiments
Sobolev et al 01
Dynamic Wetting:An Interface Formation Process
Physics of Dynamic Wetting
Make a dry solid wet.
Create a new/fresh liquid-solid interface.
Class of flows with forming interfaces.
Forminginterface Formed interface
Liquid-solidinterface
Solid
Relevance of the Young Equation
U
1 3 2cose e e e 1 3 2cos d
R
σ1e
σ3e - σ2e
Dynamic contact angle results from dynamic surface tensions.
The angle is now determined by the flow field.
Slip created by surface tension gradients (Marangoni effect)
θe θd
Static situation Dynamic wetting
σ1
σ3 - σ2
R
2u 1u 0, u u upt
s s1 1 1 2 2 2
1 3 2
v e v e 0cos
s s
d
s1
*1
*1
s 1 11
s 1 111 1
1 1|| ||
v 0
n [( u) ( u) ] n n
n [( u) ( u) ] (I nn) 0
(u v ) n
( v )
(1 4 ) 4 (v u )
s se
s sss e
s
f ftp
t
* 12 || ||2
s 2 22
s 2 222 2
12|| || || 2 22
21,2 1,2 1,2
n [ u ( u) ] (I nn) (u U )
(u v ) n
( v )
v (u U ) , v U
( )
s se
s sss e
s s
s s
t
a b
In the bulk:
On liquid-solid interfaces:
At contact lines:
On free surfaces:Interface Formation Model
θd
e2
e1
nnf (r, t )=0
Interface Formation Modelling
A Finite Element Based Computational Framework
JES &YDS 2011, Viscous Flows in Domains with Corners, CMAMEJES & YDS 2012, Finite Element Framework for Simulating Dynamic Wetting Flows, Int. J. Num. Meth Fluids.JES & YDS, 2012, Finite Element Simulation of Dynamic Wetting Flows as an Interface Formation Process, to JCP.JES & YDS, 2012, The Dynamics of Liquid Drops and their Interaction with Surfaces of Varying Wettabilities, to PoF.
Mesh Resolution Critical
Arbitrary Lagrangian Eulerian Mesh Control
Drop Impact
Impact at Different Scales
Millimetre Drop
Microdrop
Nanodrop
Pyramidal (mm-sized) Drops
Experiment of Renardy et al, 03.
Microdrop Impact 25 micron water drop impacting at 5m/s on left: wettable substrate
right: nonwettable substrate
Microdrop Impact
60e
Velocity Scale
Pressure Scale
-15ms
Microdrop Impact
?
Hidden Dynamics
10t s 13.4t s
11.7t s 15t s15t s
10t s
Surfaces of Variable Wettability
2e1e
1
1.5
Flow Control on Patterned Surfaces
-14ms-15msJES & YDS 2012, to PoF
Dynamics of Flow Through a Capillary
Steady Propagation of a Meniscus
Flow Characteristics
‘Hydrodynamic Resist’
Smaller Capillaries
Washburn Model Basic Dynamic Wetting Models
Interface Formation Model and Experiments
EquilibriumDynamic
EquilibriumDynamic
EquilibriumDynamic
Meniscus
Meniscus shape unchanged by dynamic wetting
Meniscus shape dependent on speed of propagation.
Hydrodynamic Resist:Meniscus shape influenced by geometry
Summary: Dynamic Wetting Models
Capillary Rise: Models vs ExperimentsCompare to experiments of Joos et al 90 and
conventional Lucas-Washburn theory
Lucas-Washburn assumes:Poiseuille Flow ThroughoutSpherical Cap MeniscusFixed (Equilibrium) Contact Angle
h
Lucas-Washburn vs Full Simulation
R = 0.036cm; every 100secs
R = 0.074cm; every 50secs
Comparison to Experiment
Full Simulation Full Simulation
Washburn Washburn
JES & YDS 2012, to JCP
Wetting as a Microscopic Process:Flow through Porous Media
Problems and Issues
Problems and IssuesMicro: Pore scale dynamics of:
Menisci in wetting frontGanglia
Macro (Darcy-scale) dynamics of:Entire wetting frontGanglia in multiphase system
Multi-scale porosity:Motion on a microporous
substrate
Physical Reality
02 p 0u FtF
pu
0),r( tF
Kinematic boundary condition
Dynamic boundary condition
?
0u
Continuum ModelSimplest Case First: Full Displacement (no ganglia formation)
Wetting mode
Threshold modepu
02 p
2211| pApAp S
Wetting Front: Modes of Motion
1). T. Delker, D. B. Pengra & P.-z. Wong,Phys. Rev. Lett. 76, 2902 (1996).
2). M. Lago & M. Araujo, J. Colloid & Interf. Sci. 234, 35 (2001).
Some Unexplained Effects
) zg
Suggested Description
)1/(0 THRESHOLDFFudtdh
3
4
5
6
7
8
9
10
10 10 10 10 10 10 543210 t (s )
Z (cm )
)1/(111 )](1)[( ttAhHHh cc
2/3 of height in 2 mins)z
g
Washburnian
Non-Washburnian
1/3 of height in many hours
))
Developed Theory
3
4
5
6
7
8
9
10
10 10 10 10 10 10 543210 t (s )
Z (cm )
YDS & JES 2012, JFM; YDS & JES 2012, to PRE
)z
gRandom Fluctuations ‘Break’ Threshold Mode
Flow over a Porous Substrate
Wetting: Micro-Macro Coupling
Spreading on a Porous Medium
Current State of Modelling1) Contact Line Pinned 2) Shape Fixed as Spherical Cap
The RealityEquilibrium shape is history-dependent.
Spreading on a Porous Substrate
θD
θw U
θd
Spreading on a Porous Substrate
No equilibrium angle to perturb aboutFinal shape is history dependent
ApproachUse continuum limit (separation of scales)Consider flow near contact lineFind contact angles as a result:
2 2sin( ) / ; arctan p
W p D
p
UU U
U U
θD
θw
YDS & JES 2012, to JFM
Flow TransitionFormula is when contact lines coincide
Example:
Transition when
2 2sin( ) / ; arctan p
W p D
p
UU U
U U
0.5; 30 , 1642p W DUU
90p D WU U
Potential CollaborationDrop Impact
Microdrops on impermeable surfaces Drops on permeable/patterned surfaces
Capillary RiseInvestigation of ‘resist’ mechanism in micro/nano regimes
Flow with Forming/Disappearing InterfacesCoalescence, bubble detachment, jet break-up, cusp-formation, etc.
Porous MediaInvestigation of newly developed model
Thanks
Wetting: Statics
Wetting: Statics
)
0 1 12e ep p r
1 3 2cose e e e Young
Laplace
1e
θs
e
1e
2ep 0pr
1e
1e
3e
R
Contact Line
Contact Angle
Wetting: Statics
R2 cos e
eqh Rg
2 cos eeqgh
R
02 cos ep pR
eqh
R
eeqh
Wetting: Dynamics
Wetting: As a Microscopic Process
Macroscale
Microscale
MeniscusCapillary
tube
Wetting front
)
Dynamics: Classical ModellingIncompressible Navier Stokes
θe
Stress balanceKinematic condition
No-SlipImpermeability
Angle Prescribed
No Solution!
L.E.Scriven (1971), C.Huh (1971), A.W.Neumann (1971), S.H. Davis (1974), E.B.Dussan (1974), E.Ruckenstein (1974), A.M.Schwartz (1975), M.N.Esmail (1975), L.M.Hocking (1976), O.V.Voinov (1976), C.A.Miller (1976), P.Neogi (1976), S.G.Mason (1977), H.P.Greenspan (1978), F.Y.Kafka (1979), L.Tanner (1979), J.Lowndes (1980), D.J. Benney (1980), W.J.Timson (1980), C.G.Ngan (1982), G.F.Telezke (1982), L.M.Pismen (1982), A.Nir (1982), V.V.Pukhnachev (1982), V.A.Solonnikov (1982), P.-G. de Gennes (1983), V.M.Starov (1983), P.Bach (1985), O.Hassager (1985), K.M.Jansons (1985), R.G.Cox (1986), R.Léger (1986), D.Kröner (1987), J.-F.Joanny (1987), J.N.Tilton (1988), P.A.Durbin (1989), C.Baiocchi (1990), P.Sheng (1990), M.Zhou (1990), W.Boender (1991), A.K.Chesters (1991), A.J.J. van der Zanden (1991), P.J.Haley (1991), M.J.Miksis (1991), D.Li (1991), J.C.Slattery (1991), G.M.Homsy (1991), P.Ehrhard (1991), Y.D.Shikhmurzaev (1991), F.Brochard-Wyart (1992), M.P.Brenner (1993), A.Bertozzi (1993), D.Anderson (1993), R.A.Hayes (1993), L.W.Schwartz (1994), H.-C.Chang (1994), J.R.A.Pearson (1995), M.K.Smith (1995), R.J.Braun (1995), D.Finlow (1996), A.Bose (1996), S.G.Bankoff (1996), I.B.Bazhlekov (1996), P.Seppecher (1996), E.Ramé (1997), R.Chebbi (1997), R.Schunk (1999), N.G.Hadjconstantinou (1999), H.Gouin (10999), Y.Pomeau (1999), P.Bourgin (1999), M.C.T.Wilson (2000), D.Jacqmin (2000), J.A.Diez (2001), M.&Y.Renardy (2001), L.Kondic (2001), L.W.Fan (2001), Y.X.Gao (2001), R.Golestanian (2001), E.Raphael (2001), A.O’Rear (2002), K.B.Glasner (2003), X.D.Wang (2003), J.Eggers (2004), V.S.Ajaev (2005), C.A.Phan (2005), P.D.M.Spelt (2005), J.Monnier (2006)
‘Moving Contact Line Problem’
Flow Over Surfaces of Variable Wettability
Periodically Patterned Surfaces
• No slip – No effect.
Interface Formation vs MDS
Solid 2 less wettable
Qualitative agreement
JES & YDS 2007, PRE; JES &YDS 2009 EPJ
g
0p
0p
external pressure
0.0 1.0 2.0
0.0
0.5
1.0
W ashburn(no g ravity)
W ashburn D ynam ic ang le
s = 0 .9 ,
s = 0 .1 ,
h/h 0
(t / T )01/2
= 30*1
1 * = 60h (t )
An Illustrative Example
YDS & JES 2012, JFM