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Poiseuille flow in nematics : experimental study of the instabilities
I. Jánossy, P. Pieranski, E. Guyon
To cite this version:
I. Jánossy, P. Pieranski, E. Guyon. Poiseuille flow in nematics : experimental study of the insta- bilities. Journal de Physique, 1976, 37 (10), pp.1105-1113. �10.1051/jphys:0197600370100110500�.
�jpa-00208508�
POISEUILLE FLOW IN NEMATICS :
EXPERIMENTAL STUDY OF THE INSTABILITIES (*)
I.
JÁNOSSY (**),
P. PIERANSKI and E. GUYONLaboratoire de
Physique
desSolides,
UniversitéParis-Sud,
91405Orsay,
France(Reçu
le 17 mars1976, accepté
le 17 mai1976)
Résumé. - On discute expérimentalement les modes d’instabilités hydrodynamiques obtenues lorsqu’un film nématique est placé dans un écoulement de Poiseuille plan tel que le directeur soit
perpendiculaire à la vitesse et au
gradient
de vitesse.On peut obtenir des instabilités homogènes (distorsion uniforme dans le plan des plaques limites)
avec ou sans écoulement transverse induit. Les valeurs des seuils sont comparées avec l’analyse théorique donnée dans l’article suivant.
L’effet d’écoulements alternatifs et celui de champs extérieurs appliqués sur la nature des modes
et la valeur des seuils sont étudiés. On s’intéresse en particulier à la transition avec le mode en rouleaux.
Comme aucune théorie n’existe actuellement sur ces problèmes, l’analyse est faite en référence avec
le problème de cisaillement simple bien que des différences importantes existent.
Abstract. - This work discusses
experimentally
thehydrodynamic
instabilities of an oriented nematic film contained in a plane Poiseuille flow cell such that the director is initially perpendicularto the velocity and
velocity gradient.
Homogeneous instabilities having a uniform distortion in the plane of the boundary plates are
obtained with or without distortion of the flow profile. The thresholds are analysed and compared
with the theoretical analysis given in the following paper.
The effect of
alternating
flow and of the application of external fields on the nature of the mode and on the threshold is analyzed with attention to the transition from the homogeneous to rollinstabilities. No detailed theory exists for these problems and the analysis is carried with reference to the simple shear flow case
although
marked differences are observed.Classification Physics Abstracts
6.350 - 7.130
1. Introduction. - In a
previous
article[1] (here-
after called
I)
we havegiven
an initialqualitative description
of some instabilities obtained when anematic
liquid crystal
is inserted in aplane
Poiseuilleflow cell with the initial director
alignment
atright angles
to theplane
of thevelocity (Geometry
ofFig. la).
We wish tocomplement
thisstudy by
semi-quantitative results,
bothexperimental
andtheoretical,
which lead to a betterunderstanding
of the homo- geneousinstability
and to a closer contact with thecorresponding
shear flowproblem [2].
We will also present some additional data on the convective modesalthough
thetheory
of these modes has yet to bedeveloped.
A
semiquantitative analysis
of both shear and Poiseuilleproblems
has beengiven,
based on consi-deration of the balance between elastic torques
magnetic,
electric andhydrodynamic (including
theeffect of
hydrodynamic focusing
effects in the case of aheterogeneous distortion).
This one dimensional modelneglects
the variation ofproperties
across the cellthickness and in
particular
it fails topredict
the exactFIG. 1. - a) Director configuration in the Poiseuille flow cell in small enough flows. b) Is an even function of z in twist, odd in splay.
c) Is an odd function of z in twist, even in splay.
threshold as well as the detailed structure in the
plane
of the cell
(wave length
of convective rolls in theinhomogeneous
case, existence of domains in thehomogeneous one). Recently,
a detailed two dimen-sional
analysis
of the shear flowinstability problem
has been
given [3]
which extends theprevious
treatmentand is in excellent
agreement
withexperiments
in this(*) Ce travail a bénéficié de l’aide de 1’A.T.P. lnstabilités dans les
fluides et plasmas du C. N. R. S.
(**) On leave from Central Research Institute for Physics,.
Budapest, Hungary.
Article published online by EDP Sciences and available at http://dx.doi.org/10.1051/jphys:0197600370100110500
1106
geometry. A similar
study
has been undertaken in the Poiseuille case and will be described in thefollowing
article
by
Manneville and Dubois-Violette(II
in thefollowing).
The
problem
is morecomplex
here because the shear flow rateis a function of the distance to the
boundary plates perpendicular
to z. Asimple approach
is to considerthat the distortion
develops
first near theboundary plates
where the shear islargest. However,
interference between these solutions due to elastic as well as flowcoupling
needs to be considered and the zdependence
effect is essential to the
description.
In
chapter 2,
we discuss theoriginal
features in theexperimental description
of the flow cell and of the pressure measurement and control.the theoretical
description
for the homogeneousinstability.
Considerations of
symmetry
of the solutions will shed somelight
on the morecomplex
modes not yet studiedtheoretically.
Inthe
same part3,
we discuss theexperimental
occurrence of severalhomogeneous instability
modes. Part 4 discusses the effect of alter-nating
flows as well as of electric andmagnetic
field.Despite
the richness of theinstability
modesobtained,
much remains to be done before a
quantitative understanding
of the convective modes can be obtained.2.
Apparatus.
- 2.1 1 FLOW CELL. - The flow cell is made up of twoparallel plates
oforganic glass (altuglass) P1
andP2 separated by
uniform metallic wires F(diameter d
= 0.2mm),
stretchedalong
thelength
of the cell(Fig. 2) ;
the width of the cell 1 has been varied between 1 and 20 mm. The wires also limit the transverse flows. In the upperplate
two cavities Chave been milled near the ends.
They
act as reservoirsfor the L.C.
supply
in the cell and also serve to prevent the formation of a meniscus inside the flow cell. Then volumes arepartially
filled with L.C.(M.B.B.A.,
aroom
temperature nematic,
was usedthroughout
theexperiment).
The flow is inducedby applying
a pressure differenceAp
between the small tubes T connectedto
the reservoirs. The size of the reservoirs is
large enough
to allow us to be able to
neglect
the pressure differential due to the difference of levels incomparison
withAp.
The
planar alignment
of the nematic(n perpendicular
to the flow axis
y)
is obtainedby polishing
the innerplates
orby coating
them with asemitransparent’
conducting
Au filmdeposited
underoblique
incidenceif
conducting
electrodes are needed. The cell is atta- chedrigidly by
two sets of screws and sealed with epoxy.2.2 PRESSURE MEASUREMENT AND REGULATION. -
A
typical
threshold forhomogeneous
instabilities forFIG. 2. - Schematic of the Poiseuille cell. The directions correspond
to those in the first figure.
the geometry used
(length
of the cell L = 108 mm;d= 0.2
mm) corresponds
toAp-
1.5 mmH20.
Thethreshold can be 10 to 50 times
larger
if astabilizing magnetic
field is used or in alarge enough frequency alternating
flow(the sign
of the pressure difference is inverted with afrequency f
from10-’
to 10Hz).
In order to
produce
and stabilize the small pressures involved with an accuracy of the order of 1%,
we havedeveloped
thefollowing
device with four pressurestages
(Fig. 3).
FIG. 3. - Pressure regulation and reading equipment.
The first
stage I uses a filter and a pressurereducing
valve
(Fi, Va)
to decrease the air pressure from apressure tank to an overpressure
P, ~
1 atm with anaccuracy of 10
%.
The second stage II is a more accurate
regulating valve (Re, . Va) (Gec
Elliott Automation40-2) which
lowers the pressure to a value
P2
which can beregulated
from 1 to
100 cm H20.
The third stage III is the crucial one : A thin tube
C1 (length -
50 cm, diameter 5mm)
connects the secondstage
to a needle valve Vopened
to the outside. Theopening
of the needle valve isautomatically regulated
as a function of the pressure
P3
at the entrance of thevalve
(the
pressure headP2-P3
is obtained from the value of thelength of C1
and theopening of V).
The pressure
P3
is read with a differential mano- meter with an accuracy of 0.1 mm. The pressure isregulated using
anindependent
oil manometer. Theoil level is
kept accurately
constantusing
a system with aphotocell
and alight
sourcefacing
each otherand
placed against
one arm of the manometer[4].
As the oil level rises above that of the
light
beamand
photocell,
thecylindrical
lens formed focuseslight
on thephotocell.
This causes an increase of thephotoelectric
current - the errorsignal
- used tocontrol the
opening
of the valve via a feedback system(F.B.).
In
practice
a direct action of theamplified signal
tocontrol the motor
opening
the valve is not very convenient : there isalways
a small dead zone in the rotation of thevalve ;
the valve willonly
react for aminimum value of the
photodiode signal.
We havedeveloped
an electronic circuit where the motorcontroling
the valve issubjected
to a permanentalternating
motionby applying
avoltage
Uduring
a time t+ and - U
during
a time t-. Theperiod
t = t+ + t- and U can be
adjusted
tooptimize
theresponse time. The electronic
circuit,
between thephotodiode
and a poweramplifier
which delivers thevoltage U, perform
thefollowing
function : itchops
the
unequal
time intervals t- and t+ which are such that(t- - t+)
isproportional
to the errorvoltage
read on the
photodiode [5].
The systemdeveloped
isfree from all the
disadvantages
of the direct command of the motor of the valveby
the errorsignal
andgives
an excellent
long
termstability.
The fourth
stage IV : In order to increase the sensi-tivity
of thereading
ofP3
we havedeveloped
asimple
pressure divider. The pressure
P3
isapplied
to alarge
reservoir
through
along
thintubing C2.
A leak(F2)
isproduced by connecting
the reservoir with the outsidethrough
a thin open tubeC3
of the same diameter.The overpressure
P4
in the buffer reservoir is a small fraction of the overpressureP3.
An estimate of the ratioP 31 P 4
is obtained from the ratio of thelengths
of the tube
C2
overC3. However,
this is not very accurate and a direct calibration(showing
deviationsfrom
linearity)
has been used. The pressureP4 (typi- cally
between 0 and 10 cmH20)
isapplied
to the flowcell and can be
regulated
and readthrough
theP3 stage
with an accuracy of 5%.
3.
Homogeneous instability (corresponds
toP 1 A
in ref.
[1]).
- 3.1 INTRODUCTION. - We consider the case of a dc flow in the absence of external fields.The flow can be
applied
for a timesufficiently long along
one direction(frequency f ~ 10 - 2
to10-3 Hz)
so that the maximum
displacement
of theliquid
D =
vml f
islarger
than the characteristic dimensions(width
of thecell 1,
thicknessd( I)).
When the pres-sure
gradient G,
measuredby Ap
= GL and propor- tional to the maximumvelocity
vm, isincreased,
the nematic becomes distorted above a critical thresholdApc.
Just abovethreshold,
the distortion characterizedby
thepolar angles 0,
T definedbelow,
ishomogeneous
across the width of the cell.
It can be controlled
by
the rotation 0(associated with Q)
and lateraldisplacement (0)
of theconoscopic image
formed in convergent monochromaticlight
incident on the cell
(y
andë
are averages across thick-ness).
Anotherimportant
factor is the finiteangle W
of the
flow,
measured in the centralportion
of thecell,
withthe y
axis when distortion is present. Theangle
is measured frommicroscopic
observation of the motion of dustparticles
introduced in the L.C.It is found in
practice that,
above thethreshold,
theonly
modification of theconoscopic image
from theclassical double set of
hyperbola
obtained for aplanar sample
is an overall rotation.Typical experi-
mental results are
given
onfigures
4 and 5.FIG. 4. - Variation of the twist distortion (measured by (p) above threshold APc,A for the homogeneous instability mode A (the angle
of the flow lines with y, tp, is practically zero everywhere).
FIG. 5. - Same variations as in figure 4 for homogeneous mode B (03C8 is different from zero above threshold APcB).
3.2 MODEL. - The
experiments
and model deve-loped
hereapply
to materials such that the twohydrodynamic
torques a2 and a3 arenegative.
This isthe case when the
coupling
of the torque components due tofluctuating
distortionsnz, ny { (ny), (n.) , 1 }
isdestabilizing.
The effect isacting against
thestabilizing
influence of the twist
(K2)
andsplay (Kl) elasticity.
In addition we include the effect of a transverse flow
vx(z)
due to the componento(Jzx/oz
of the Leslie-Ericksen stress tensor.
1108
The
unperturbed velocity profile
isgiven by (origin
of the coordinates
midway
between theplates) :
and the shear rate
by
we deduce the
equations governing
a fluctuation from those of thesimple
shear flowproblem [3].
1) Torque equations : they
areunchanged
2)
Forceequation :
we must take into account thespatial
variationof s(z)
inôu zx/ ôz ;
thisgives
The consideration of
instability
mechanisms described in ref.[2, 3]
allows one todistinguish
twotypes
of distortion[ 1 ]
which involves an average twist over the thickness.
which involves an average
splay.
This
property
isalready
apparent in eq.(3.2).
Inaddition,
from eq.(3.1)
and(3.3),
we deducethat vx
and ny have the same
parity. Moreover,
we may consider the mostgeneral instability
mode where thevelocity fluctuations vyand Vz
and the pressure fluctua-tion no
longer
vanish.Using
thecontinuity equation
we deduce
that vy
has the sameparity
as vx or ny,and v_,
that of nz. This result is of course
compatible
with thewhole set of
equations
that may beadapted
from thesimple
shear flowproblem (ref. [3 J, appendix A).
A
complete
solution of the system(3.1)
to(3.3) taking
into accountboundary
conditionsis
developed
in 2.Let us
give
asimplified description
of the solution.Equation (3.3)
describes a transverse floweffect,
coupling
the distortion of n in the xyplane
to adeflection of the flow line
along
the x axis.By
reinsert-ing
the variation ofvx(z)
inequation (3. 1),
one obtainsa term linear in shear which renormalizes the a3 term.
If we
neglect
this renormalization which is tantamount toneglecting
the transverse flow(such
a solution canin fact be
produced experimentally) [7, 8]
we obtainthe
simple
setUsing
the reduced variablesfly
= nywe get the
symmetrical equations
with a
diffusivity
of orientationby
addition andsubstraction,
weget
thedecoupled equations
where u =
ny + nZ, v
=ny - iíz.
The
eigenvalue problems
with theboundary
condi-tions
(3.4)
are somewhat similar toSchrodinger equations
with a variablepotential
well± s’ z/D (Fig. 6)
and aneigenvalue
= 0. We have obtained anumerical solution of the two
equivalent
equa- tions(3.9), (3. 10).
The lowesteigenvalue
isgiven by
an Ericksen number
characterizing
the critical flow rateThe
corresponding eigenfunctions
localized nearthe bottom of the
potential
well aregiven
in thefigure
6. From the functions u, v one can construct two solutions for the distortion. The first one,given
onthe bottom of the
figure 6,
isantisymmetric
in thesplay
FIG. 6. - The solutions u, v of the eigenvalue equations (3 . 9)-(3 .10)
for the two possible forms + Ez (E = s’/D) and one of the possible solutions
for ny
and nz (the one even in ny(z), which is obtainedexperimentally).
variable
(nz(- z) = - nz(z))
andsymmetric
in twist.Another
equally probable
solution issymmetric
insplay
andantisymmetric
in twist.In
experiments dealing
with very widecells,
thefirst one is found to be more stable. The difference
comes from the
neglect
of the flowcoupling
in thisanalysis :
A transverse flowvx(z) symmetric
in z iscoupled
with the twist solutionsymmetric
in z.The exact solution
given
in 2 includes the effect of transverse flow. Manneville and Dubois-Violette usein the
following
variablesand an Ericksen number
The
dependence
of the critical thresholdErc;
with(r¡a/r¡b) is given
for both the average twist(T)
andaverage
splay (S)
mode infigure
4(II).
The
analysis
of II reducesexactly
to our in thelimit
na/nb
= 1. In this case, the thresholds for the S and T solutions are the same. Note that in this limit the transverse flowdisappears [6]. (The viscosity in
the xy
plane
becomes alsoisotropic.)
3.3 EXPERIMENTS. 2013 The solution
(3.1)
neverapplies exactly
to theexperimental
condition as itneglects
the effect of lateralboundary
conditions which limit the transverse flow.We discuss first
experiments
doneusing relatively
wide cells
(1
~ 10mm, d
= 200u). Interesting
effectsassociated with the finite width will be discussed next.
Two
instability
modes are obtained which arecharacterized
by
the absence(A),
or the presence(B)
of transverse flows
[l3].
Regime
A. - Infigure 4,
we haveplotted
therotation
angle 0
as a function ofAp.
In thismode,
(p does not vary across the
length
of the cell exceptpossibly
near the ends where the flow pattern is ill defined.Starting
fromlarge Ap,
we see that Q is close ton/2.
The director iseverywhere nearly
in theplane
of the flow. The effect of the
splay
is limited to anangle Om
with the flowaxis,
such thattg’ Om
=a3/a2.
This is however an
antisymmetric
contribution across d and theconoscopic image
remains centered around the z axis. As the flow rate isreduced,
0 decreases and vanishes for acritical
pressure variationAp,,A.
Notethe
parabolic
and continuous variation of 0 near threshold. This is characteristic of the second ordermean field transition. On the same
figure,
wehave, plotted
theangle Y’
of the flow with y, determined from the motion of dustparticles.
Noappreciable
transverse flow is observed.
Regime
B. -Increasing
the pressure from zero, anotherpossible
solution is obtained which is shownon
figure
5. Above a critical valueApc,B,
an average twist distortion 0develops
as in theprevious
case.An
original
feature of this solution is the existence of a transverseflow,
characterizedby
a finiteangle IF,
aboveAp,,B.
The maximum value of 03C8 around 0 = 450 iseasily
understood if one refers to ourprevious study [6]
of transverse flows where the uniform orien- tation of the nematic in a Poiseuille flow cell wasobtained
by applying
alarge magnetic
field at anangle
Q with the flow axis. It wasfound,
andexplained,
that the flow is deflected towards the direction of the
director,
due to the effect of the variable shear acrossthickness,
and that a maximum deflectionangle
03C8 - 10° was obtained around an
oblique
orientation of 450 as in thisstudy.
A
quantitative comparison
between the tworegimes
lead to the
following
results.-
Regime
B appears to be more stable thanregime
A for small distortions(typically o 45o)
and has a smaller threshold.
This is
why regime
B is obtainedby applying progressively larger Ap. However,
in the case oflarge distortions, regime
A is the most stable one and leadsto a
larger
distortion 9 for the sameAsp.
In
figure 7,
we have indicated the variation of 0 obtained fordecreasing
values ofAp.
Between twopoints
of measurements, a verylong
time waskept (typically
1hour).
The discontinuous decreaseof 0
is associated with the onset of mode B.However,
as the time constant is solong,
it ispossible
to describe thecomplete
A and B curves as the time needed to obtaina new distortion value within the same
regime
is muchshorter.
1110
FIG. 7. - In this experiment the pressure difference Ap was reduced extremely slowly starting from a largely distorted state without.
transverse flow (solution A). For an intermediate pressure value another branch is reached which corresponds to the domain of
stability of solution B (with transverse flow). Solution B is the most stable at threshold.
The existence of two solutions is consistent with the theoretical
description.
Solution B
corresponds
to the solution(3.17)
of IIincluding
the effect of transverse flow. Acomparison
between the
experimental
threshold and the theoreticalone
gives
thefollowing
results for theexperiment
offigure
10 :Gexp
= 24.5 cgs,corresponding
to atheoretical
evaluation, using equations (3.11)
and(3.1)
and theviscosity
datagiven by
Gahwiller[14], Gth
= 16.5 cgs. The order ofmagnitude
agreement is an indication of the overallvalidity
of the modelon the
experiments.
The lack of
quantitative
agreement cannot be takentoo
seriously
at the present stage as(3.11)
involves acombination of viscous and elastic coefficients which
are not known
accurately
from one set ofexperimental
data to the next
(for example
theuncertainty
on a3 is of the order of 50%).
Solution A can be understood if one considers the
possibility
of a pressuregradient
termoplox
acrossthe width of the cell which compensates the d.c. flow
across the cell. This is
possible
for the solutioninvolving
an average twist(ny(z)
even inz)
obtainedexperimentally,
where thevelocity vx(z)
variation is also even in z(for
a type S solution wherevx(z)
is oddin z there is a
possibility
of transverse closed flowloops
as obtained in the
corresponding
shear flowproblem).
The solution of this
problem
is obtainedby
can-celling
the contribution of the transverse flow(see
form
(3.11)).
Itclearly
leads to ahigher
thresholdthan B. However a correct solution of this
problem
should
clearly imply
a discussion of the xdepen-
dence and on the side
boundary effects,
and thequantitative comparison
cannot bepursed
in thepresent stage.
Domains. - In our discussion of mode B we have not yet mentioned the very
spectacular
formation ofregular
domainsalong
thelength
of the cell. The twist Q is uniform within one domain butchanges sign rapidly
as one crosses the narrow twist wallseparating
two domains. A
photograph showing
theoptical
contrast due to the different diffusion of
light
betweendomains was
given
inI, Fig.
4.Very regular
structurescan be
produced
if theinstability
isproduced
in thepresence of a transverse
magnetic
field which limits the effect of defects due to surfacemisalignment.
Thevery
long
time needed before theregular
structure isobtained
(whose
effect wasalready
obvious in the discussion ofprevious paragraph),
arises from the fact that the creation of domains involves a diffusion of orientation over verylarge
distances.The
wavelength
of thedomains, A,
is anincreasing
function of the width I and varies
roughly linearly
with it :
For cells of width 1 =
5 ; 10;
20 mm, we have found A =3.1 ; 4.3 ;
8.6 mm.(In fact,
the characteristic time is solong,
that thequantitative
results must be takenwith some care as
they
do notnecessarily
represent finalequilibrium states.)
A
possible
mechanism for thedescription
of thewalls can be obtained from consideration of
figure 8, giving schematically
thevelocity
distribution in aframe
moving
with thevelocity
Vrn’FIG. 8. - In a frame of reference XY’ Z moving at the velocity of the flow in the central portion of the cell the additional flow
( f )
due to transverse forces is seen and cause a slightly backward motion
of the walls VI to x) separating domains of opposite average twist.
The formation of domains allows the
development
of a transverse
velocity
vT in a limited geometry. Thetriangular shapes
which can be seen in thefigure 8
insure the
continuity
of thevelocity
from one domainto the next. The
sign
of the z component of thehydro- dynamic
torques due to thegradient OVT/OY
is the samein both domains 1 and 2.
Consequently
the domain ofexistence of 1 increases and a backward relative motion of the domain walls is obtained. Indeed it is observed
experimentally
that the motion of the walls is slowerthat the flow
velocity
in the central flow field. We have also followed the motion of smallparticles.
When aparticle,
in relative motion with respect to awall,
crosses
it,
its transverse motionchanges sign quite discontinuously.
Narrow cells. - In cells
typically
narrower thanI = 3 mm, the formation of domains and the solution B
are
strongly
inhibited. In these cells it ispossible
toproduce
in aquite equivalent
fashion the average twist(type 1)
and averagesplay (type 2)
solutions.By applying temporarily
anoblique magnetic
field(H
inthe
plane perpendicular
to theflow)
in the presence of theflow,
one induces asplay
of n in the cell. If thepressure
gradient
islarger
than the criticalvalue,
thesplay
solution(ny
oddand nz_,
even functions ofz)
of the Poiseuille
problem
remains after the field issuppressed.
It appears that the threshold of this solution and that of the twist one are very close for agiven
cell. This is consistent with thesimplified
solu-tions obtained when one
neglects
the transverse flow.The
splay
solution should however involve some flow(vx
has the same oddparity
as ny and a transverse pressure cannotcancel vx completely).
As a conclusion of this discussion we want to
point
out the limit of
applicability
of the model to theexperimental
situation and the need for a(apparently complex)
solution wherelong
range two dimensional effects in theplane
of the film are considered.4.
Alternating
flow and field effects. - Anoriginal
feature in the
study
of instabilities in nematics is thepossibility
of controlby application
of electric andmagnetic
fields. We have used both astabilizing magnetic
fieldH, acting
on ny and nz, and astabilizing
electric field
Ez acting
on nZ.The effect of the field can be introduced in the definition of the relaxation time constants for ny and nZ.
The effect of H and
f
on the threshold have been considered at thesame
time on thegraphic
construc-tion of
figure
9.FIG. 9. - 3 D diagram indicating the limit of stability of the homo- geneous (H.I.) and roll (R.I.) instabilities; the constant ap curves (p) and magnetic field curves (h) were obtained experimentally.
The d.c. threshold curve ( f = 0) agrees quantitatively with the analysis of (I) (see 3-3 of I). The unstable region is above the surface.
4.1 FREQUENCY EFFECT
(H
= E =0).
- Let uSfirst consider the situation in the absence of fields
(Fig. 10).
The threshold of thehomogeneous
insta-bility (H.I.)
increases first withfrequency.
This issimple
to understand as the effect of a finite time for thegrowth
of aninstability
should increase the effective threshold.However for
frequencies typically larger
than0.15 Hz another mode
(which
will be referred asR.I.)
is obtained at
threshold,
where convective rollsalong
the flow axis are formed. A
qualitative description
ofFIG. 10. - Gives in more detail a constant field curve (for H = 0)
for a 200 u thick, 10.8 cm long flow cell. In the transition regime (TR) between the H.I. and R.I. ones, both modes can be found at the same
time in different regions of the cell.
the rolls has been
given
in I and willonly
be recalledbriefly.
The mode obtained at threshold is even in ny and oddin nz, just
as thehomogeneous
one(see Fig.
8of
I).
The rolls involve a
periodic
distortionny(x)
of nacross the rolls. The effect of the distortion in
inducing hydrodynamic
focalization terms and new destabiliz-ing
mechanisms has beenanalysed
in detail in thecorresponding
shear flowproblems [2, 3].
The
wavelength
of the rolls is of the order of d for lowAp
and decreases asAp increases (typically
asOp-1/2).
This feature indicates that the distortion is localized in each halfplane
near thelimiting plates
and
suggests
the formation of two sets of convective rolls near theplates.
This result is consistent with the fact that thevelocity vz(x)
should have the sameparity
asnZ(x) (see
table ofII)
and be zero in the centralplane.
The convective rolls formed near oneplate
donot extend to the
opposite
one and do not contributeto the
coupling
between the two solutions. Howeveran elastic
coupling
is still present between the dis- tortions present in the twosuperficial
sheaths where the shear islargest.
The convective
[10]
flow has been detecteddirectly
from the observation of the motion of dust
particles undergoing spiral
motions in the flow.As the
sign
of the flow isinverted,
the distortion nychanges sign
but not n,,. This result was obtainedby optical
observation of the focal lines which are formed due to the modulationnz(x).
The lines do notchange position
over each halfperiod.
In thecorresponding
shear flow
problem [2]
such aregime
was called Ymode. It is not clear whether such a
simple description
of the
dynamic interplay of ny and nz
is sufficient here.One can characterize the threshold from the
occurrence of the diffraction pattern of a wide
parallel
1112
monochromatic beam incident on the
sample.
Aphotocell
linear in response iscoupled
with a X - trecorder and the onset of the transition is detected
accurately.
4.2 MAGNETIC FIELD. -
Coming
back tofigure 9,
we
analyse
the additional effect of anapplied
field.A curve similar to that of
figure
10 but obtained in afield
Hx
= 2 750 G isgiven (h).
It also shows the existence of a H.I. domain for smallfrequencies
anda R.I. one for
larger
ones. Note however that the thresholdsA/?e
arelarger
than for H = 0 due to thestabilizing
influence of H. We may also note that the domain of existence of the H.I. does not appear to decrease as H increases unlike the shear flow case.In fact the limit
frequency f =
0.15 Hz(for d
= 200g)
is the same on both H = 0 and 2 750 G curves. The variation of threshold with fields at
f
= 0 is discussed in II. It is shown that theexperimental
variationof
Apc(H) expressed
in terms of the Ericksen number agrees with theoreticalpredictions (see figure
9 ofII).
The critical surface can be also
mapped by studying
the variation of the critical
frequency
versus Hkeeping Ap
constant(curves p).
The curves alsodisplay
thechange
ofregime
between RI and HI. It may looksurprising
that thehomogeneous instability develops
in this case for
large
values of H. One could haveexpected
that thestabilizing
effect ofH,
which isindependent
of thespatial
variation of n, overcomesthat of the
elasticity
and tends to favor the formation of rolls if thedestabilizing
mechanisms are moreeffective in this case. The detailed
analysis
of the forces in this case remains to be done. We also notethat,
as H increases at constantAp,
thewavelength
of the rolls tends to increaseslightly (by 10 %
from H = 0 to thetransition
regime).
This is due to the effect of thecorresponding
decrease off ;
A is never verylarge
ascompared
with themagnetic
coherencelength
andthe
elastic effect can never been
neglected
unlike the shearflow case.
4.3 ELECTRIC FIELD. - The effect of an electric field
applied
between twotransparent conducting
electrodes
deposited
on theboundary plates
has beenused
extensively
to control thetype
ofinstability
modepresent at threshold.
The
figure
11presents
the limit ofstability
ofconvective solutions in coordinates
V, T -1.
Eachcurve
corresponds
to agiven
pressure difference and themagnetic
field iskept
constantthrough
theexperiment.
The characteristic Sshape
solution hasalready
been obtained in otherinstability problems
in nematics
[2], [11]
and defines twotypes
of convective solutions.For V
Vcu,
whereVcu
refers to the cusp of the curve, theinstability
observed atfrequencies
belowthe critical
corresponds
to that discussed above for V = 0.Above
Vcu,
theinstability
mode appears to be characterizedby
thefollowing
features :FIG. 11. - Instability thresholds for roll instabilities obtained in AC flow. Constant ap curves are given. A destabilizing electric field along z(E = Vld) has been applied. Note the hysteretic effect shown
on curve Ap = 100 mm. The broken line curve was obtained in
decreasing voltages.
- Zero average twist and non zero average
splay
across thickness.
- Periodic modulation
of ny and nz along x (across
the
rolls).
-
Wavelength
of the rollsrelatively independent
of
voltage (the change
ofwavelength
between the two convectiveregimes
can bequite large
as thewavelength
in the
previous
case could be much smaller than d forlarge frequencies
anddp).
- The
velocity vz(x)
is an even function of z(same parity
asnz(z)).
Thispoint
is consistent with the pre- vious one as it indicates thepossibility
ofsimple
convective
loops
across thecell,
whose size iscontinued by
the cell thickness.- The time
dependent properties
of this mode areconsistent with a Z type
solution,
as introduced in shear flowproblem [2],
whereonly nZ changes sign
over each
period.
The conditions of existence of this solution as well as thedynamic
behaviour are connect-ed with the fact
that,
as Eincreases, TZ/Ty decreases,
which makes
the nZ
relaxation easier.The characteristics of this mode
(refered
asII)
arevery similar to those of the mode
P2B
discussed in I and which can beproduced by application
of avalue
ap sufficiently larger
than the threshold value.The cusp
shape
can be revealed in asingle experi-
ment at a constant
frequency f
= 0.5Hz (keeping Op
= 80 mmH20 constant).
Figure
12gives schematically
therecording
of theintensity
of the lowest order diffractedpeak
of aparallel
laser beam. For E =0, Ap
islarger
than thecritical value and the
light intensity
is finite.As E is increased towards a first critical value
E10,
theintensity
decreasesregularly
to zero(indicative
of asecond order transition on the branch
I).
The inter-mediate stable domain