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A FemVariational approach to the droplet spreading over dry surfaces. S.Manservisi Nuclear Engineering Lab. of Montecuccolino University of Bologna, Italy Department of mathematics Texas Tech University, USA. - PowerPoint PPT Presentation
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A FemVariational approach to the droplet spreading over dry surfaces
S.Manservisi
Nuclear Engineering Lab. of Montecuccolino University of Bologna, Italy Department of mathematics Texas Tech University, USA
Simulations of droplets impacting orthogonally over dry surfaces at Low Reynolds Numbers
OUTLINE OF THE PRESENTATION
- Introduction to the impact problem- Front tracking method- Variational formulation of the contact problem- Numerical experiments
Depostion
Prompt Splashd
Corona Splashd
INTRODUCTION
Depostion
Partial reboundd
Total reboundd
INTRODUCTION
An experimental
An experimental investigation .....C.D. Stow & M.G. Hadfield
Spreading smooth surfacev=3.65 m/sr=1.65mm
INTRODUCTION
An experimental
An experimental investigation .....C.D. Stow & M.G. Hadfield
Splashing rough surfacev=3.65 m/sr=1.65mm
INTRODUCTION
An experimental
INTRODUCTION
1) Problem : Numerical Representation of Interfaces• Impact Dynamics : solid surface + liquid interface = drop surface • Splash Dynamics : liquid interface -> more liquid interfaces
2) Problem : Correct Physics•Impact Dynamics : solid surface + liquid interface = drop surface
• Splash Dynamics : liquid interface -> more liquid interfaces
Hypoteses:No simulation of the impactNo splash o total rebound (low Re numbers, no rough surfaces) Axisymmetric simulation
Numerical Representation of Interfaces -> okCorrect Physics ?
Some features:
• Behavior of the impact for: Wettable-P/Wettable N/Wettable surfaces • •Deposition – Partial rebound – total rebound
• Surface capillary waves
• Spreading ratio and Max spreading ratio
• Static/Dynamic/apparent Contact angle
INTRODUCTION
D=1.4mmv=0.77m/s
Re=1000We=10
Wettable Partially Wettable Non-Wettable
Deposition
Partially Wettable
Non-Wettable
INTRODUCTION
τ= τ(μ) = Stress tensor
Dynamics (incompressible. N.S.eqs)
incompressible
u = velocity p=pressure
f_s = Surface tension f = Body force
μ =viscosity = μ1 χ + (1-χ) μ2
ρ =viscosity = ρ1 χ + (1-χ) ρ2
Kinematics (Phase eq.)
Equation for χ (phase indicator)χ =0 phase 1χ =1 phase 2
Solution:1) Weak form (method of characteristics)2) Geometrical algorithm
Boundary conditions
Static cos() =cos(s) v=0 no-slip boundary condition
Non Static cos() =cos(s) ? v=0 no-slip boundary condition ?
V. FORM OF THE STOKES PROBLEM
2
0,||min 1
0uSS
VuHu
0
0
up
upuu
V
VV
gives
20
10
Lp
Hu
20
10
Lp
Hu
CONTACT PROBLEM (NO INERTIAL FORCES)
dAdAdAF
dVuS
FS
gsls
gsls
V
uHu
lg
10
2
0,
||2
1
)min(
10
10
Hu
Hu
F = Shape derivative in the direction u
CONTACT PROBLEM (NO INERTIAL FORCES)
un
dAdAdAdt
dF
gsls
gsls
lg
lg
0
0lg
up
unupuu
V
VV
Minimization gives
20
10
Lp
Hu
20
10
Lp
Hu
10Hu
No angle condition
)2
1(min 2
20,10
s
zdAuFS
uHu 1
0zHu
dAussun
utunF
sc
cs
s
2))cos()(cos()(
))cos()(cos(
lg
lg
MINIMIZATION WITH PENALTY
10
10 HuHu z
Remarks:s
dAu222
1 Is a dissipation term
Contact angle condition
CONTACT PROBLEM WITH PENALTY
0
0))cos()(cos(lg
2
up
utun
uuupuu
V
cs
VV s
Minimization gives
20
10
Lp
Hu z
20
10
Lp
Hu z
10zHu
0))cos()(cos()(
2
ssc
sss
uss
uuupuu
s
sss
Boundary condition over the solid surface
)(10 ss Hu
02 u
0),,,,( suf Boundary condition
0 Full slip boundary cond
V.F.OF THE CONTACT PROBLEM
0
0))cos()(cos(
)(
lg
2
up
utun
uuupuu
uuuut
u
V
cs
VV
VV
s
20
10
Lp
Hu z
20
10
Lp
Hu z
0 Near the contact point
otherwise
Numerical solution
Fem solution
•Weak form -> fem•Advection equation -> integral form•Density and viscosity are discountinuous -> weak f.•Surface term singularity-> weak form
ADVECTION EQUATION
0
ut
1
0
0t
t
udtxx
10 tt Surface advection
Integral form
Advection equation
(2D)
ReconstructionAdvection
ADVECTION EQUATION
Markers= intersection (2markers) Conservation (2markers)
Fixed mrks (if necessary)
VORTEX_SQUARE.MPEG
ADVECTION EQUATION
Vortex testsADVECTION EQUATION
ADVECTION EQUATION
ADVECTION EQUATION
Fem surface tension formulationSurface form
Volume formc
hhhh
hh uds
dxdA
ds
u
ds
dxdAun
lglg
dVudVu
dVudAun
V
hh
V
hh
V
hhhh
lglg
lglg
Is extended over the droplet domain
Static: Laplace equationSolution for bubble v=0, p=p0
Spurious Currents
Fem surface tension formulation
Static: Laplace equationSolution for bubble v=0, p=p0
1) Computation of the curvature2) Computation of the singular term
Solution v=0, v=0p=0 outside p=P0=a/R inside
Fem surface tension formulation
Casa A: exact curvature
SolutionCurvature=1/RSurface tens=σV=0; p=p0
No parassitic currents
Fem surface tension formulation
Case B: Numerical curvatureWith exact initial shape
A t=0 B t=15 C t=50Curvature
Initial velocity
Final velocity
Fem surface tension formulation
Case C: Numerical curvature (ellipse)
Shape
time
Fem surface tension formulation
Steady solution
angle=120
angle=60
angle=90
Boundary condition over the solid surface
Boundary condition over the solid surface
1
)(10 ss Hu
02 u
0),,,,( suf
02 Full slip boundary cond
Re=100 We=20 =60 Deposition
t=0
t=2.5
t=4
t=15
t=50
t=0t=0
t=0
t=0.5
t=3
t=1.5
t=1
Re=100 We=20 =60 Deposition
Re=100 We=20 =90 partial rebound
t=4
t=5
t=0t=0t=0t=0t=0t=0
t=6
t=0t=0
t=3
t=2
t=1.5
t=1
t=0.5
t=0
t=7
t=9
t=8
t=10
t=11
t=14
Re=100 We=20 =90 partial rebound
Re=100 We=20 =120 total rebound
t=.5
t=1.5 t=3t=0
t=2 t=4
t=7
t=2.5t=1
Re=100 We=20 =120 total rebound
DIFFERENT WETTABILITY
Wettable (60) A Non-wettable (120) C
partially wettable (90) B
Re=100 We=100 =120
Re=100 We =120 u0 =120
We= 100 A 50 B 20 C 10 D
u0= 2 A 1 B .5 C
Different impact velocityDifferent We
DYNAMICAL ANGLE
cWeaD
D)(Re 5.0
max0
Glycerin droplet impact v=1.4m/s D=1.4mm
Wettable (18) Partially wettable (90)
DYNAMICAL ANGLE
0))cos()(cos()(
)(
2
ssc
ss
SS
uss
uuupuu
uuuut
u
s
sss
ss
))cos())(cos((' sdcss
' dFriction over the solid surface Friction over the rotation
DYNAMICAL ANGLE MODEL
Cox
mds ACa )cos()cos(
)96.4tanh()cos()cos( 706.0CaAds
)sinh()cos()cos( BCaAds Blake
Power law
Jing
Non-Wettable
Wettable
D=1.4mm u0=1.4m/s glycerin droplet
A=1B=2C=10
A=1B=2C=10
D/D0
h angle
Conclusions
- Variational contact models can be used
- Open question: Can we simulate large classes • of droplet impacts with a unique setting of• boundary conditions ?
Thanks