on the origin of the vorticity-banding instability 5 cm 2 cm constant shear rate throughout the...

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1 band 2 band applied On the origin of the vorticity-banding instability 5 cm 2 cm tant shear rate throughout the system multi-valued flow curve isotropic and nematic branch different concentrations shear-induced viscous phase not clear what the origin of t banding instability is

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Page 1: On the origin of the vorticity-banding instability 5 cm 2 cm constant shear rate throughout the system multi-valued flow curve isotropic and nematic branch

1band

2band applied

On the origin of the vorticity-banding instability

5 cm

2 cm

constant shear rate throughout the system

multi-valued flow curve

isotropic and nematic branch different concentrations

shear-induced viscous phase

not clear what the origin of the banding instability is

Page 2: On the origin of the vorticity-banding instability 5 cm 2 cm constant shear rate throughout the system multi-valued flow curve isotropic and nematic branch

low high

rolling flow within the bands normal stresses along the gradient direction

normal streses generated within the interface of a gradient-banded flow ( S. Fielding, Phys. Rev. E 2007 ; 76 ; 016311 )

Page 3: On the origin of the vorticity-banding instability 5 cm 2 cm constant shear rate throughout the system multi-valued flow curve isotropic and nematic branch

Binodal

0.0 0.2 0.4 0.6 0.8 1.00

1

2

[s-1]

.

nem

]s[ 1Vorticity banding

Spinodals

Tumblingwagging

Critical point

concentration concentration

1

fd virus :

L = 880 nmD = 6.7 nmP = 2200 nm

( P. Lettinga )

nem0 1

Page 4: On the origin of the vorticity-banding instability 5 cm 2 cm constant shear rate throughout the system multi-valued flow curve isotropic and nematic branch

almost crossed polarizers distinguishorientational order

vorticitydirection

P

A

100 m

Page 5: On the origin of the vorticity-banding instability 5 cm 2 cm constant shear rate throughout the system multi-valued flow curve isotropic and nematic branch

1 2 3 4 5 6 7 8

0 10 20 30 40 50 60

60

80

100

120H[m]

Time [min]

1 2 3 4 5 6 7 8

stretching of inhomogeneities

growth of bands

Shear flow

vorticity direction

Gapwidth 2.0 mm

~ 1

mm

00( ) 1 expA

t tH t H

A

Page 6: On the origin of the vorticity-banding instability 5 cm 2 cm constant shear rate throughout the system multi-valued flow curve isotropic and nematic branch

N

band width growth rate

00( ) 1 exp

t tH t H A

23 % :

35 % :

;A finite 0;A finite

heterogeneous vorticity banding

0H

A

interconnected

disconnected

Page 7: On the origin of the vorticity-banding instability 5 cm 2 cm constant shear rate throughout the system multi-valued flow curve isotropic and nematic branch

spinodal decomposition : nucleation and growth :

m100

( with Didi Derks, Arnout Imhof and Alfons van Blaaderen )

0.75nem 0.23nem

Page 8: On the origin of the vorticity-banding instability 5 cm 2 cm constant shear rate throughout the system multi-valued flow curve isotropic and nematic branch

tracking of a seed particle( counter-rotating couette cell )

with Bernard Pouligny (Bordeaux)

Page 9: On the origin of the vorticity-banding instability 5 cm 2 cm constant shear rate throughout the system multi-valued flow curve isotropic and nematic branch

increasing shear rate

elastic instability for polymers :

non-uniform deformation equidistant velocity lines

1.0 1.5 2.0 2.560

70

80

90

100

H [m]

G [mm]

Weissenberg or rod-climbing effectK. Kang, P. Lettinga, Z. Dogic, J.K.G. Dhont Phys. Rev. E 74, 2006, 026307-1 – 026307-12

Page 10: On the origin of the vorticity-banding instability 5 cm 2 cm constant shear rate throughout the system multi-valued flow curve isotropic and nematic branch

New viscous phases can be induced by the flow (under controlled shear-rate conditions )

stress

shear rate

new phase

homogeneous

inhomogeneous

personal communication with John Melrose

Page 11: On the origin of the vorticity-banding instability 5 cm 2 cm constant shear rate throughout the system multi-valued flow curve isotropic and nematic branch

( , , ) ( , , ) ( , , )( , , )y y y

m y z y

u y z t u y z t u y z tu u B y z t

t y z

Stability analysis :

discreteness of inhomogeneities along the flow direction is of minor importance :

mass density gradient component of the body force

( , , ) ( ) expyu y z t u y ik z t

( , , ) ( ) expyB y z t B y ik z t

z-dependence exp ki z t 2 / k with the typical distance between inhomogeneities

ˆ( , , )yB F r u t

“Brownian contributions”

+”rod-rod interactions”

+“flow-structure coupling”

linear

bi-linear

linear

probability density for the position and orientation of a rod

r

u

xy

z

u

r

J.K.G. Dhont and W.J. Briels J. Chem Phys. 117, 2002, 3992-3999 J. Chem Phys. 118, 2003, 1466-1478

z

y

Page 12: On the origin of the vorticity-banding instability 5 cm 2 cm constant shear rate throughout the system multi-valued flow curve isotropic and nematic branch

2

yB small 0 large

0 1ˆ ˆ ˆ( , , ) ( , ) ( ) ( , , )r u t A r u A y r u t

“renormalized base flow probability”

2

4( ) ( )1

yB y A y

linear contributions

22

4( ) ( )1

yB y A A y

bi-linear contributions

1

2 2

42 4( ) ( )1 1

yB y A A yC C

rod-rod interactions

2

41

2 2

4 41 2( ) ( )1 1

m u y A A yC C

0A 0A 0u

2

1

2

42 4 01 1

C AC

1 0C 2 0C

2

4 01

A C

Page 13: On the origin of the vorticity-banding instability 5 cm 2 cm constant shear rate throughout the system multi-valued flow curve isotropic and nematic branch

l

u

2

4

( )

1 ( )A

C unstable stable

A C

4A C

2

4 01

A C

depends on the microstructuralproperties of the inhomogeneities

0.0 0.2 0.4 0.6 concentration

Page 14: On the origin of the vorticity-banding instability 5 cm 2 cm constant shear rate throughout the system multi-valued flow curve isotropic and nematic branch

Wilkins GMH, Olmsted PD, Vorticity bandingduring the lamellar-to-onion transition in a lyotropic surfactantsolution in shear flow, Eur. Phys. J. E 2006 ; 21 ; 133-143.

Fischer P, Wheeler EK, Fuller GG, Shear-bandingstructure oriented in the vorticity direction observed forequimolar micellar solution, Rheol. Acta 2002 ; 41 ; 35-44.

Lin-Gibson S, Pathak JA, Grulke EA, Wang H,Hobbie EK, elastic flow instability in nanotube suspensions, Phys. Rev. Lett. 2004 ; 92, 048302-1 - 048302-4.

Vermant J, Raynaud L, Mewis J, Ernst B, Fuller GG,Large-scale bundle ordering in sterically stabilized latices, J. Coll. Int. Sci. 1999 ; 211 ; 221-229.

Bonn D, Meunier J, Greffier O, Al-Kahwaji A, Kellay H,Bistability in non-Newtonian flow : rheology and lyotropic liquidcrystals, Phys. Rev. E 1998 ; 58 ; 2115-2118.

Micellar worms

Nanotube bundles

Colloidal aggregates

-Worms- Entanglements- Shear-induced phase

Page 15: On the origin of the vorticity-banding instability 5 cm 2 cm constant shear rate throughout the system multi-valued flow curve isotropic and nematic branch

Kyongok Kang Pavlik Lettinga Wim Briels