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Effect of shear on a lyotropic lamellar phase
Olivier Diat, Didier Roux, Frédéric Nallet
To cite this version:
Olivier Diat, Didier Roux, Frédéric Nallet. Effect of shear on a lyotropic lamellar phase. Journal de
Physique II, EDP Sciences, 1993, 3 (9), pp.1427-1452. �10.1051/jp2:1993211�. �jpa-00247917�
ClassificaIion
Physics
Abstracts61.30 82.70 46.60
Effect of shear
on alyotropic lamellar phase
Olivier Diat
(*),
Didier Roux and Frdddric NalletCentre de recherche Paul-Pascal, CNRS, avenue du Docteur Schweitzer, 33600 Pessac, France
(Received17 Mat-c-h 1993, accepted 18 May 1993)
Abstract.-We present a series of
experiments, using
differenttechniques
such aslight scattering,
conoscopy, neutron scattering and microscopic observations, to determine the orientation of lyotropic lamellarphases
under shear. Three states of orientation are observed,depending
upon both the shear rate and the inter-membraneseparation.
Thesesteady
states areseparated by dynamic
transitions.Among
the states described, we focus our attention on a state made of monodisperseclose-packed multilayered
vesicles whose Size is precisely fixedby
the shear rate.1. Introduction.
Surfactants in solution are known to
lead,
in concentratedregimes (surfactant
ratio~ 30
§b),
tolyotropic liquid crystals ].
In certain cases, suchlong-range-ordered phases
maypersist
overa very
large
range of dilution. This is the case for dilute lamellarphases (lyotropic
smecticsA)
which have beenextensively
studied[2-41. Indeed,
theability
ofpreparing phases
made of membranes withvarying continuously
the intermembraneseparation
has allowedquantitative
measurements of membrane
properties [3, 41. Owing
to itsliquid crystalline
nature, thelyotropic
lamellarphase
possesses static anddynamic properties
associated to both thecrystalline organization (long-range
translationalorder, elasticity)
and theliquid
one(viscosity,
concentration
fluctuations...).
The measurements ofmacroscopic properties
such as elastic constants, have allowed researchers to obtain information on the interactions andflexibility
of membranesconstituting
the smecticphase.
Forexample,
it has beenpossible
to demonstrate that dilute lamellarphases
are stabilized eitherby weakly-screened
electrostaticrepulsions [51
or
by
undulation forces[3-81.
One can now consider that alarge part
of theequilibrium
behaviour of these
phases
has been understood both from amicroscopic viewpoint (stack
ofinteracting membranes)
and from amacroscopic
one(two-component
smectic Aelasticity).
Much less is known
conceming
theirout-of-equilibrium properties.
The effect of shear on the structure of a
phase
is assumed to be aperturbation
of or achange
in its
spatial organization, However,
one has todistinguish
betweenlong-range-ordered
(*) Pi~esent address Installation
europdenne
de rayonnement synchrotron, ESRF, B-P. 220, avenue des Martyrs, 38043 Grenoble Cedex, France.phases,
where even a small shear canproduce large
effects such as shearmelting [91
andliquid phases
whereexpectations
tomodify
theshort-range
order arisesonly
when the shear rate ishigh enough
to be of the order of a characteristicfrequency
of the associated fluctuations. Theratio between shear rate and this characteristic
frequency
is called the Deborah number(De
). Forsimple liquids
the relevant characteristicfrequency
is in the rangelo~°-10'~
s~ 'which makes
experimentally
accessible Deborah numbers very small. In systems wherelarge
characteristic distances
(and consequently
small characteristicfrequencies)
arefound,
the effect of shear can beexperimentally
studied. This is the case for instance in colloidal systems[10],
critical fluids[11]
orliquid crystalline phases
close to the smectic-nematicphase
transition
[12].
With dilute lamellar
phases having
characteristic distances of several hundredAngstroms,
one expects several
interesting
features to takeplace.
First, inregular liquid crystals,
one notonly
expects an orientation of thephase
under flow[13],
but also achange
in the structure, or at least of the smecticproperties
Deborah numbers of the order of I are reached for reasonableshear rates
(10~/10~
s~ ').
In this
study
we report a series ofexperiments characterizing
some effects of the shear on dilute lamellarphases.
Wemainly
focus on the orientation of the system under shear.Using
visual
observations, scattering techniques
andbirefringence
measurements an « orientationdiagram
» is built that characterizes the varioussteady-state
orientations as a function of shear rate and dilution.The system studied is a quatemary mixture of SDS
(sodium dodecyl-sulphate), pentanol,
water and dodecane. The dilution consists in
adding
dodecane +pentanol (9
§b inweight)
to aninitially
concentrated lamellarphase (water
over surfactant mass ratio : 1.55 ; dodecane(resp.
pentanol) weight
fraction 31 §b(resp.
18§b)).
Thephase diagram (see Fig. I)
isgiven
inprevious
papers[2].
The lamellarphase
of this system is stabilizedby
undulation forces[5].
Upon
dilution therepeating
distance varies from 40I
to 400I.
We
briefly
describe the cells used forbirefringent
and neutronscattering
measurements andgive
the orientationdiagram,
as it results from our observations.Finally,
we describe theproperties
of two of thesteady
orientation states found.PENTANOL
I
L~
H
WATERJSDS
= 1.55 DODECANE
Fig. I. Cut of the phase
diagram
of the quatemary system water,pentanol,
dodecane and sodiumdodecylsulphate.
The water : surfactant ratio is fixed to 1.55. Thesymbol
L~ denotes the location of thelyotropic
lamellarphase.
2. Shear cells.
Couette cells made up of
cylinders
andancillary
windows ofglass
were used for directobservations and
optical experiments.
For neutronscattering experiments,
Couette cells madeof quartz instead of
glass
wereemployed.
The two concentriccylinders
have radii of about 30 mm andheights
of 60 mm. The gap between thecylinders
may be varied(changing
theinner
cylinder), by o.5,
or 2 mm. This Couette geometry is chosen because ityields
a flow with(quasi)
constant shear rate in the laminarregime
when the gap is filled with asimple
Newtonian fluid. Moreover the inner
cylinder (stator)
is fixed while the outer one(rotor)
rotates, in order to avoid the
Taylor instability. Depending
upon gap and rotorangular
velocity,
the shear rate f varies from o to 8 coo s-I(f
= Rwle, e is the gap
size,
w theangular velocity
and R the(inner)
radius of therotor).
When the gap is filled withliquid crystalline samples,
the flow isprobably
morecomplex
than thesimple,
laminar flow oneencounters with
regular
fluids. We neverthelesskept
the name« shear rate » and notation
j
for Rwle. Because oursamples
are sensitive toevaporation
andtemperature variations,
theCouette
cylinders
are contained inside a thermostated and sealed oven(see Fig. 2).
Four windows on the oven allow visual observations and neutron orlight
irradiation. The neutronscattering
cell has been made in collaboration with laboratoire Ldon-Brillouin(CEA/CNRS, Saclay, France),
where the neutronscattering experiments
have beenperformed.
A
plate/plate cell,
made of arotating glass plate
situated at agiven
distance from a fixed one(schematically
drawn inFig. 3)
has also been used. Such a cell can fit in anoptical microscope
to allow direct space observations. The shear rate is no
longer
constant but variescontinuously
with the distance from the rotation axis.
However,
for thicknesses of o. I to I mm there is noappreciable
variation of the shear rate over themicroscope
field(about 1mm2).
Since we are interested in
describing
the orientation of a lamellarphase
in a Couette cell, wedefine the
eigen
directions as follows. We refer to thecylindrical
coordinate axes of the Couette cellX,
Y and Z ;(see Fig. 2)
and to the smectic axis with unit vector n normal to thelayers.
We define X to be the(tangential) velocity axis,
Y the(radial) velocity gradient
axis and Z the(neutral)
rotation axis.3. Visual observations.
Several
samples
have been studiedalong
a dilution line.They correspond
to different oil concentrations andconsequently
have differentd-spacings.
For eachsample
visual obser- vations between crossedpolarizers
as a function of the shear rate are made eitherdirectly by
eye on the Couette cell, or under the
microscope using
theplate/plate
cell. From theseobservations we construct an « orientation
diagram
» in the shear rate-concentrationplane.
It defines three distinctregions
where differentqualitative
andquantitative
behaviours are seen(see Fig. 4).
At very low shear(region
I f <ii corresponding
to lineSj),
the texture looks veryinhomogeneous
onmacroscopic
scales(~
10 ~Lm). Amicroscopic
observation shows that the system is full of defects(which
have not beenwell-characterized)
that aremoving
with the flow(see Fig. 6a).
Above a well-defined shear rate that is a function of the concentration
(region
II aboveline S see
Fig. 4),
the texture observed seemshomogeneous.
However, the existence of anisotropic
modulation of the index of refraction at micrometer scales, is revealedthrough
the clearring
ofscattering
observed when a laser beam crosses thesample (see Fig. 5).
Thering
size is an
increasing
function of the shear rate(Figs.
5a, b andc)
and may be associated to a characteristic domain size that decreasescontinuously
from about lo ~Lm to less than I ~Lm uponincreasing
shear. With themicroscope
oneeffectively
sees a well-definedlength
in theii
-
~
z
x
Y
Fig.
2. Plan of the Couette cell Icorresponds
to the rotor, 2 to the stator, 3 is therotating
axis, 4 is the sealed therrnostated oven, 5 a sealedrotating
ballbearings,
6 a crown wheel to transmit the rotation, 8 seals, 9 Quartz or Glass windows and lo water circulationcoming
from a thermostated bath. The Z-axis is the symmetry axis the X-axis is along the
tangential (velocity)
direction the Y-axis is along the radial(velocity
gradient) direction.modulation of the
birefringence (Fig.
6b andc)
that does not exist at lower shear rate(region
I,see
Fig. 6a).
When the shear issuddenly stopped,
thering persists
and so does the modulation of the refractive index.At
higher
shear rates, thering finally disappears
when the lineS~ (which
defines shear ratef2)
is reached(see Fig. 4).
Abovef~ (and
belowj~, corresponding
to line S~ inFig. 4)
a well- defined texture isagain visually
noticeable,using
crossedpolarizers
or even withoutpolarizers
in certain cases. In the Couette
cell,
the texture is made withaltemating
dark andbright (using
.iIICROSCOPE
STATOR
~~,jpLE ,j~~~R
ROTOR
Fig.
3. Sketchyplan
of theplate/plate
cell we have used foroptical
observations (microscopy).a)
b)III o
j(s.')
>
o fi
iii
s3
il+ill ° o
,
~~ o ,
i II
si
~~
10 15 20 25
~o
joo# (fb)
C)
'j'
IS~~)
iii
~
ii S
10 20 30 40 50
j (o~)
Fig.
4. Orientationdiagram
of thelyotropic
lamellarphase
under shear. The X-axis corresponds to the membrane (water + surfactant) weight fraction. The Y-axis is the shear rateapplied
in the Couette cell.Regions
I, II and III correspond to steady « pure orientations » as described in the text. Theregion
labelled II + III corresponds to a mixed state where states II and III coexist in the cell. Notice that the
experiments
are donefixing
the shear rate a) is aplot
in linear scales b) is aplot using
a doublelogarithmic
scale. Thestraight
linescorrespond
toslopes respectively equal
to 3 (from I to II) and around 5 (from II to III) c) schematicrepresentation
with adrawing
of the orientation states.*
a) b) c)
Fig. 5. Small angle light scattering patterns, observed on a screen. The ring of scattering is observed in
region
II only. The shear increases from al to c).polarizers) band-shaped domains,
stackedroughly periodically
inequatorial planes
: there isan
axially-symmetric
modulation onmacroscopic
scales of the refractive indexalong
the Z- direction. Theperiod
of thestacking
varies with shear rate nonmonotonically.
It first increaseswith f
(in
the range o.1-2mm)
and then decreases. The modulationdisappears
whenS~ is crossed, I.e. upon
entering region
III. Themicroscopic
observation has allowed us to conclude that the state between the S~ and S~ lines is a mixed one thatcorresponds
to thecoexistence in
alternating stripes
of theregion
II andregion
III states.In
region
III(j
~
f~),
the orientation state of thesample
lookshomogeneous
: neitherscattering
or anymicroscopic
texture is observed. There are no further transitions until the maximum shear rate(j
= 5 coo s~ is reached.
The «orientation
diagram
»,figure
4,gives
the location of the boundaries betweenregions
I, II and III at agiven
gap. It is clear that the extension ofregions
I and II decreases when the dilution(or d-spacing)
increases.Region
III is thenquickly
reached. Forinstance,
a shear rate as low as a few s-' isenough
to enterregion
III for a d around 300I.
Figure
7displays
the gap size effect on the location of theregion boundaries,
for gaps 2, and 0.5 mm(resp. Figs.
7a, b andc).
Theboundary
linesSi
and52
arebasically
unaffectedhowever, the location of line S~
strongly depends
on the gap size(I.e.
the smaller the gap size thehigher
the shear ratej~).
The
regions
andregion
boundaries arereproducible
and do notdepend
on the initial state of thesystem (random
orpartial
orientation fresh oralready
usedsample). Only
the timerequired
to reach asteady
state is a function of thehistory
of thesample.
Ingeneral,
thehigher
the shear rate the faster a
steady
state is reached.Typical
transient times are of the order of 10 to 60 min. When the shear isstopped,
the texture remains at first intact. Itchanges
with timedepending
on the location of thesample respecting regions
I, II or III. Indeed, whenstarting anywhere
inregion II,
there is no noticeable evolution even afterdays
and thering
ofscattering
can be observed with no
changes
neither inposition
nor inintensity (if
not shearedagain).
Moreover,
thesample
can be removed from the shear cell with care andplaced
in a flat vesselkeeping
the same texture(the ring
is stillvisible).
The behaviour is different inregions
I andIII,
where states withmacroscopic
texturesdiffering
from the initial ones may be reached in afew hours or less.
4.
Region
U : thespherulite
state.As mentioned above, the state
prepared
inregion
II of the orientationdiagram
islong-lived
and remainsessentially
unaltered aftergentle manipulations
of thesample.
We thus removed partSk'
a)
h)
lxPm
Fig.
6. -Direct space observations under apolarizing
microscope. a)Corresponds
to a shear rate~ l s- '
(region
I) when b) and c)correspond
to shear rates inregion
II (shear higher in cl than in b)).of the
sample
from the Couette cell and observed it with apolarizing microscope.
A series of observations were made on agiven sample prepared
inregion
II,varying
the shear rate. A thinisotropic
texture with a characteristiclength
is observed similar to the one observeddirectly
in theplane/plane
cell undermicroscope (Figs.
6b and c). The order ofmagnitude
of thislength
iscompatible
with the size of thescattering ring.
As the shear rate used to prepare thesample
is increased, the observed texture becomes thinner and thinner, asexpected
from thelight
scattering experiment.
The texture does not evolvesignificantly
with time and can bekept
for severaldays
in a sealed(to
preventevaporation)
cell. We should stress that the texture of a~
a) T(s-i)
iii
20 30 40 50
#
(fb)h)
I(s-ij
~°°° III
11
20 30 40 50
#
(fb)C) y(s-1)
8000iii
11
20 30 40 50
#
(fb)Fig.
7. Effect of the gap size on the orientationdiagram.
Gap sizes arerespectively equal
to of 2 mm (a), I mm (b) and 0.5 mm (c). Limits I- II and II
- II + III are more or less insensible to the gap size when the limit from II + III to III varies
noticeably.
fresh
sample (which
has not beenpreviously
sheared in a controlled way andconsequently
with no characteristiclength
in itstexture) placed
in the same cell evolves veryslowly (within days)
toregions
ofhomeotropic
orientationsseparated
with focal conics(oily streaks).
In order to further
analyse
theregion
II texture, we have done thefollowing experiment.
Weplaced
between twomicroscope
slides a small amount of the shearedsample
to which weslowly
added to one side of thesample
a small amount ofswelling
solvent(9
9bpentanol
;91 §b
dodecane),
in order to get a contact line between the sheared lamellarphase
and the puresolvent
(see Fig. 8).
At theinterface, droplets
of lamellarphase (spherulites)
are observed.Their diameter is
equal
to the characteristic size of the textureseparating
from the bulk(see Fig. 9).
In fact, it isclearly
observed that the bulksample
consists ofclosely packed spherulites
that we are able to separate
(swell) using
thistechnique.
This observation is central to the newMICROSCOPE
~
LAMELLARPHASE
~
PURESOLVENT
/~
DILUTION
Fig.
8. Schematicdrawing
of the contactexperiment
described in the text. The lamellar phase has beenpreviously
sheared in region II and the solvent is the mixture of dodecane (91 fb) and pentanol (9 fb) that yields the dilution line followed.a) b)
C) d)
Fig.
9.-Microscopic
patterns observed using the contact line method described infigure
8:a)
corresponds
tosample
situated on the left of the contact line (in the bulk of the lamellarphase)
; pattems b) to d)correspond
tosamples
situated more and more toward the pure solvent side (on the right).way of
preparing monodisperse microcapsules by shearing
various lamellarphases,
describedelsewhere
[14, 15].
In theparticular
case described here(system
withSDS, pentanol,
dodecane and
water)
thespherulites
dissolve in the solvent after some 20 to 60 min. However in other casesII 4, 15] depending
on the surfactant and solventchosen, they
do not dissolve and remain insuspension (their
Brownian motion can be observed when their size is below 5 ~Lm) for several months.Since a well-defined characteristic size
(the spherulite diameter)
can be definedby light scattering,
we have studiedquantitatively
its variation as a function of the shear rate at variousdilutions of the lamellar
phase.
Atypical
curve is shown infigure10 whereby
the sizedecreases with the shear rate.
Anticipating
a theoreticalinterpretation,
weplot
infigure
I thespherulite
diameter as a function off~
'~~ forsamples
at different dilutions[14].
A linear behaviour is observed with adilution-dependent slope
(more dilutesamples
have a lesserslope).
We also checked for apossible
gap size effect and athigh
shear rates no such effect was observed. Nevertheless, for small shear rates thespherulite
diameterdeparts
from the linear behaviour morestrongly
for smaller gaps, with sizeslarger
thanpredicted (see Fig. 12).
More details may be extracted from
light scattering.
Indeed, when thesample
is sheared the diffractionring
is notperfectly
circular but has aslightly elliptic shape.
However, when noshear is
applied
thering
recoversquickly
a circularshape. Figure
13 presents the evolution of thering excentricity (difference
between vertical and horizontal radii dividedby
the meandiameter)
as a function of the shear rate. At low shear rate thering
is verynearly
circular athigher
shear rate a ten percentexcentricity, roughly
constant, is observed.Small-angle
neutronscattering experiments
have beenperformed,
with thescattering
geometrydisplayed
infigure
14 the beam is incidentradially (along Y-axis),
withscattering
wave vectors therefore confined to the X-Z
plane.
It was notpossible
to get reliable results witha
tangential
beam(along X-axis), mainly
because of the strongabsorption resulting
from the travelthrough
about 10 mm ofsample.
Our access to thereciprocal
space is thus restricted to theneutral/velocity
directions. This restriction is removed in theX-ray scattering experiments
made
by Safinya
et al.[16]
on lamellarsamples
sheared inregion
III.D l~m)
o
o
o
o o
o
j~s-i)
Fig.
sheared in II. The size is
measured using the position of the peak in small
scattering (see Fig. 5). It
corresponds to the
onion
size that can be haracterized independently by theexperiments described
in
igures 8 and 9.D j~m)
~
a
I.0
0.2 0.4 0.6 0.8 1.0f q~ mi/2)
Fig.
II. Plot of the characteristic onion size (in a Couette cell with a I mm gap) as a function of the inverse of the square root of the shear rate. Differentsamples
have beenregrouped
in thisfigure, corresponding
to different dilutions. The membraneweight
fraction isrespectively
47.6 fb (full circles), 42 fb (opentriangles),
27 9b (fulltriangles),
20 §6 (opensquares).
A linear behaviour is observed in eachcase.
o
~ (~'~')
A a
o a
o u
~~
a4~~
0.0 0.1 0.2 0.3 0A 0.5 0.6
ijf (s'/2j
Fig.
12. Evolution of the characteristic onion size as a function of the inverse square root of the shear rate for a givensample
(membraneweight
fraction 42 9b), using different gap sizes open circles correspond to a gap size of o.5 mm, fulltriangles
to I mm and open squares to 2 mm. Athigh
shear rates sizes aregap-independent
but at lower shear rates a systematic deviation from the linear behaviour isobserved, more pronounced for the smaller gaps.
Representative
results(sample
with membrane volume fraction37§b)
aredisplayed
infigure
15. The scatteredintensity
isrepresented by
level lines in theQx-Qz Plane.
Inregion
I, thescattering
isclearly anisotropic (Fig. lsa)
and becomesisotropic
whenregion
II is reached(Fig. lsb).
When the shear rate is further increased(still
inregion II),
there is some weakanisotropy (Fig. lsc).
A stronganisotropy, figure lsd,
characterizesregion
III.The information that we
gain
from thespectra, mainly through
the orientation andintensity
of the
Bragg diffraction, corresponds
to the membrane orientation distribution. Inregion II,
aso.15
Rv-Rh
0.12Rv+Rh
~ ~~ . . .
~
°.°°o
j(s.i)
Fig. 13. -
Evolution
as
ifference etween two iameters of
the
ring divided by theirsum. Theellipticity
is
first
very small (at low shear ates) but increases to saturate
to
avalue
ypically equal to ten
percent.
a) ~j
.
Qx
ci
, .
l
(f
=s~')
; b) and c)to
regionII
f=
24s~'
ndegion (f
=
500 s~ ' ).1(q)
is characteristic of at leastpartially
oriented dilute lamellarphases exhibiting
both smallangle scattering
and aquasi-Bragg peak [8].
Thescattering along Qx,
the(tangential)
flowdirection,
isnegligible indicating
that there are no membranesperpendicular
to the flow. Thescattering along Qz (neutral direction) originates
in the membranes that areperpendicular
to this direction. However, since theintensity along Qz
remains constant at the level measured inregion
II where thescattering
from aperfect powder
isexpected,
most of the membranes areprobably
oriented with their normalalong
the(radial) QY
direction. Thishypothesis
is wellsupported by
the conoscopyexperiments
described below.Finally,
we note that for the most dilutesamples (highest
shearrates),
theintensity
of theBragg peak along Qz
may decreaseslightly.
BIREFRINGENCE MEASUREMENTS. The smectic A
phase
is a uniaxial medium and thereforebirefringent
ingeneral.
Thepolarization
state of thelight
transmittedthrough
an orientedsample depends
on thebirefringence
of the system(An )
and on the orientation of the incidentwave vector with respect to the
optical
axis.Consequently,
theanalysis
of theintensity
of thelight
transmitted betweenpolarizers gives
information on the orientation of thesystem.
Let
p
be theangle
between the incidentlight
wave vector k and theoptical
axis n(which
is also the membranenormal),
with 0 theangle
between the incidentpolarization
direction and aa) bj
,'
~
~
o-~
~
zl_
Qx
cj dj
Fig. 16. Neutron
scattering
pattems observed in region II, fora membrane
weight
fraction of 48 9b.The
respective
shear rates are j=
8 s~ ' la), f
=
255 s~ ' (b), f 490 s~ ' (c) and f = 200 s~' id).
~~j~ ~
Fig.
17. Schematicinterpretation
of theanisotropy
observed in both light and neutronscattering (Figs.
13 and 16). The onions areslightly
deformedby
the shear however, thiselongation
remains weak(of
the order of lo 9b).reference direction
perpendicular
to both n and k(see Fig. 18).
The relativeintensity
measured(after
ananalyzer making
anangle #
with respect to thepolarizer)
for alight
beamtravelling
athickness e
through
thesample
isgiven by
the standard formula~
=
cos~
# sin 2 6 sin[2(6
+ 4
)] sin~ I
Ansin~
pJo
if one may assume that the
birefringence
An is smallcompared
to bothordinary
orextraordinary
indices.POLARIZER
n k
Uo
u o ~
ANALYSER
~
~
~ ue
z
n ~f
V
' "' y
I
X
"',(
Fig. 18. Definitions of the angles used in the conoscopy experiment. The angle between the membrane normal n and the wave vector of the light k is p the two angles Hand ~ refer to the polarizer and analyser
orientations, respectively the two angles ~ and x define the orientation of the membrane normal n in the Couette system of axes.
This
equation
has asimpler
form whenpolarizer
andanalyzer
are atright angles ii
=ar/2):
=
sin~
2sin~
"~ Ansin~
p(2)
lo
AFor
simple
orientations of the lamellarphase
in the Couette cell, withlight propagating along
the Y-axis (see
Fig. 19),
1442 JOURNAL DE PHYSIQUE II N° 9
z ~
tllvv
till
Fig.
19. Schematic representation of the simple (« pure ») orientations of a smecticlayered
system in aflow. The different states are respectively labelled as
A(nflZ), B(nflv)
andC(nflvv).
orientations A or B
~p
=~
2 lead toorientation C
(p
=
0)
leads to=
0
(3b)
lo
In order to determine the
birefringence
An, we have measured theintensity
transmittedthrough samples
of known orientation. Suchsamples
areprepared
in thinrectangular glass capillaries (?
mm wide, 200 ~mthick),
where agood homeotropic
orientation is achieved witha thermal treatment. The transmission of a
polarized
(H=
«Ml
He-Ne laser beam(A = 6 328
hi
is measuredas a function of the
angle
a between the incidentlight
and the normal to thecapillary (see Fig. 20).
Because of thehomeotropic
orientation p= a, the
transmitted
light
with crossedpolarizers (#
=
ar/2)
isgiven by
:~~~~
i
~"co~
a
~~~~ " ~~~
where e is now the thickness of the
capillary (optical path
e/cos a).
Fits of the data toequation (4),
shown infigure
21,give
thebirefringence
as a function of the membraneweight
fraction#~, figure
22. Thebirefringence
An varieslinearly
with#~
and we getAn a + hi
~
(5)
with a
=
1.055 x
10~~
and b= 4.91 x
10~~
n
~ beam
LASER
CAPILLARY
Fig. 20. Schematic drawing of the set-up used to measure the birefringence of a series of samples
perfectly aligned
incapillaries.
Theintensity
transmitted between crossedpolarizers
is recorded as afunction of the angle a.
O
~86.9
$
~j
@o
NO °d
~ i
O
cQ
O '
160
q -40 -20 0 20 40 60tl
(°)
l~19.7
~fl0
~~
~
~C>
~
-40 -20 0 20 40 60
°
(°)
Fig.
21. Typical transmission curves obtainedusing
the set uprepresented
figure 20. The full lines are obtained by fitting theexperimental points
to the theoretical expression, equation (4).Anx10'~
0 20 40 60 80 100
#(%)
Fig. 22. Values of birefringence obtained for samples with different membrane weight fractions ~.
The behaviour is
basically
linear and the best fitcorresponds
to An= a + b~
,
with a 1.055 x IO ~ and b 4.91 x IO ~~
The same
technique
is now used to determine the orientation(knowing
thebirefringence)
ofa lamellar
phase
under shear. Theexperimental
set-up allows to send the beamthrough
one gaponly (see Fig. 23).
It also allows theangle
a(between
the incident beam and theY-axis)
to vary. In order tosimplify
theanalysis
and tooptimize
theintensity,
thepolarization
is rotated ar/4 away from the Z-axis/beamplane
and theanalyser
set atright angle (#
= ar/2 ). We have
checked that the maximum
intensity
iseffectively
obtained with such a geometry.Two types of
experiments
have beenperformed.
On onehand,
we have recorded theintensity
fora =
0 as a function of the shear rate. Some
typical
data are shown infigure
24.The
intensity
first increases as a function of the shear rate when thesample
goesthrough regions
I andII,
then saturates inregion
III. As for the neutronscattering,
in the case of the most dilutesample
theintensity slightly
decreases atlarge
shear rates. When thebirefringence
is
high enough,
the ratio between the measuredintensity
and incident one may oscillate inCOUETTE
M P ~/2
CELLM
jh
,,,,
D
A L
LASER
MOTOR
Fig.
23. Schematicdrawing
of the set-up used to determine the orientation of a sample of known birefringence but unknown orientation when it is sheared in the Couette cell. The angle a is varied by a Small rotating mirror placed inside the stator.il10
.
'
.
~
,~mmmmmeo m * * * * m
m ~
o o oo o o ~~
0.4
0.2
0 2000 4000 6000 8000
jis.t)
Fig. 24. Variation of the
intensity
transmitted between crossedpolarizers
through differentsamples,
as a function of the shear rate, for normal incidence (a
= 0). The
plateau corresponds
to the appearance of region III.region
II + III beforereaching
itsplateau
value inregion
III. For the most concentratedsample
several oscillations can be seen
(Fig. 25).
This effect iseasily
understood in terms of an increase of thephase
termbeyond ar/2,
inequation (2).
This firstexperiment
confirms the results obtained with neutronscattering, namely
thatregion
IIIcorresponds
to a constantorientation
(except
for the most dilutesample
where aslight
evolution exists we come backon that
point
lateron).
IIj II + III III
a ~
I/I0
0.6
0.
n
0 1000 2000
30§0
4000'j'(s.1)
Fig.
25. Same asprevious figure
for agiven
concentratedsample.
The oscillations are due to the fact the phase becomes larger than w/2.We then
analyze
the orientation inregion
III, in a secondexperiment
where we vary the incidentangle (around
normalincidence),
with a shear rate fixed in theplateau region,
for different dilutions. From the neutronscattering experiment
we know that there are no domainshaving
the membrane normalalong
theX-axis,
I-e-parallel
to the flow. We thus describe theorientation state in terms of domains oriented in the Y-Z
plane.
The model we use assumes aGaussian orientation distribution with width
A~,
centered around the C orientation(see
Fig.
19 membrane normal nparallel
to theradial,
orvelocity gradient axis).
This leads(see appendix)
to thefollowing
transmittedintensity
:~
-
SIn~
"l~
~A~~
+ « ~II
~l~~ I1 16)
for small values of
a.
Two
quantities, namely
thebirefringence
An and the mosaicA~,
may beindependently
extracted in
principle
from the data. Plots of arcsin[(I/Io)"~]
as a function of a ~, with linear fits arepresented
infigure
26, with theresulting
values for the two parametersgiven
in table I.The
birefringence
values areconsistently
very close to the ones determined on orientedsamples.
The evolution with dilution of the mosaicangle
A~ isgiven
infigure
27. Its valueseems to be constant and of the order of 25° except for the most dilute
samples,
whichgive
higher A~
values at their lowestregion
III shear rates. However as we havealready noticed,
for most dilutesamples
there is an evolution of theBragg peak intensity corresponding
to achange
of orientation inregion III,
as shear is increased. The conoscopyanalysis
indicates that the mosaicangle, initially high,
comes back to about 25° athigher
shear rates(see Fig. 28).
al
sir~ I
IO
.0.0 0.1 0.2 0.3
02 (rad2j
b)
asiIl4
0.0 0.1 0.2 0.3
02 (rad2)
Fig.
26. Evolution of the normalizedintensity
as a function of the square of theangle
a for smalla s.
Knowing
thebirefringence,
theslope
allows to get the mosaicangle using equation
(6).The same kind of model has been used in
analyzing
the neutronscattering
intensities,comparing
theBragg
intensities for aperfect powder sample (obtained
inregion II)
and for asample
inregion
III,assuming again
a Gaussianmosaicity arouid
the direction of thevelocity gradient.
We found a width in the 30 to 45° range, in agreement with the conoscopymeasurements.
6. Discussion.
From the results we
obtained,
we conclude that as shear increases three types of orientation areseen. At low and
high
shear rates, the dominant orientation of the smectic domains is the Corientation and
corresponds
to the membrane normalpointing along
the radialvelocity gradient
direction. The main difference between the low
(region Ii
andhigh (region III)
shearregions
is that their mosaicities arequite
different. Inregion I,
there are domains orientedalong
the flowas well as
along
theZ-axis,
while inregion
III thephase
is better oriented with anegligible
mosaic in the direction of the flow and about 25° disorientation with respect to a pure C
Table I. Values
ofparameters for
the linearfit
to the curves shown infigure
26. The valuesof
thebirefringence
and mosaic-angle
are calculatedusing equation (6).
Thecomparison
betweendifferent
gap sizes(I
and 2mm)
isgiven.
lx An (°) (Invn)
Anby (°) (2nwn)
39.98 19.20
xllJ-4 22.05
35.49 17.25
x10-4 22.26
29.67 16.21
x10-4 22.80
28.76 14.25
xllJ-4 23.63 11.lJl
xllJ-4 24.13
24.45 12.23
xllJ-4 22.43
22.24 8.40
xllJ-4 27.4 llJ.26
xllJ-4 23.75
19.13 12.24
xllJ-4 22.49
16.99 7.28
xllJ-4 25.74
13.54 5.20
xllJ-4 28.05
9.45 3.04
xllJ-4 40.75
50
~~ .
by
30
~ m
m
10
1 (it)
ig.
27.
weight fraction region III. Full square
corresponds to a
1mm
gap and to 2 mm.orientation. One of the most
striking
result is the existence of acompletely isotropic
orientation in an intermediateregime
of shear rates : inregion II,
the membranes arewrapped
around aspherical
coreforming large objects (the spherulites)
that areclose-packed
and with their size determinedby
the shear rate. These differenthomogeneous
states of orientation areseparated
with
dynamic lout-of-equilibrium)
transitions. The nature of such transitions is underinvestigation
however, it is clear thatgoing
fromregion
II toregion
III involves a first order transition acoexisting region
isclearly
seen in between. Thecomplete understanding
of this28
.,
a_
26 A.~
24 ill
.
22
0
Fig.
29. -Schematicdescription
of the orientation of the membranes between the walls in statel.Dislocations allow to match the fluctuations of the thickness. The dashed line indicates that there are many more layers in the real system that what is shown here (the scale is not preserved).
related to the undulation
instability
mayhappen [17-18].
The criticalvelocity
above which thedislocations are unable to follow the flow is related to the
permeation
coefficientA~ and elastic constants of the smectic
phase [18].
We have checked that the critical value of the shear rate at which the transition I
- II appears decreases when d increases
(see Fig. 4).
When the dislocations can nolonger
follow the
flow,
there is a constraint which appearsnormally
to the flowleading
to anundulation
instability.
In the Couette cell thisinstability develops
arectangular
lattice in the X- Zplane.
When the dilation islarge
the undulations fuse into a lattice of focal conics[19]
and it is thenprobable
that the system cannot flow as aliquid
any more. We may think that at this shear rate the system has to find another way oforienting
the lamellae tosupport
the flow.From the
experimental
results we obtained, it seems that apossible
solution is to formspherulites
which can roll on each other.The
spherulite
size can be calculatedusing
a verysimple
estimate that issupported by
moredetailed models
[20], following Taylor's explanation
of the size of emulsionsprepared
under shear[2 II. Considering
aspherulite
of size R(made
of n=
R/d
layers),
we balance the viscous stressS~ = 7~R~ j
with the elastic stress stored in this
spherical particle S~=4ar(2K +k)/d.
The
limiting
size R reached isconsequently
:14ar(2K+k)
R"
~.
(7)
'~ Y
At this
level,
this has to be considered as a dimensionalargument,
however moremicroscopic
models of thebreaking
of a smecticdroplet
under shear leads to similarexpressions [20].
We havealready
observed that the j~ "~ behaviour has beenexperimentally
verified. One of the