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Distortion waves and phase slippage in nematics
J.-M. Dreyfus, P. Pieranski
To cite this version:
J.-M. Dreyfus, P. Pieranski. Distortion waves and phase slippage in nematics. Journal de Physique,
1981, 42 (3), pp.459-467. �10.1051/jphys:01981004203045900�. �jpa-00209030�
Distortion waves and phase slippage in nematics
J.-M. Dreyfus
Laboratoire d’Hydrodynamique Physique, E.S.P.C.I., 10, rue Vauquelin, 75005 Paris, France and P. Pieranski
Laboratoire de Physique des Solides, Bât. 510, Faculté des Sciences, 91405 Orsay, France (Reçu le 9 septembre 1980, accepté le 12 novembre 1980)
Résumé.
2014On démontre que les ondes de distorsion peuvent se propager dans un milieu nématique infini lorsque
celui-ci est soumis au cisaillement polarisé elliptiquement. Ces ondes sont hélicoïdales et leur propagation cor- respond à la rotation de la distorsion hélicoïdale. On indique l’analogie avec la propagation des ondes de cisail- lement dans un fluide newtonien en rotation.
Dans une couche nématique d’épaisseur finie la rotation de la distorsion est observée en présence d’un champ électrique qui empêche la relaxation de la distorsion.
On développe l’analogie entre la distorsion dans une couche nématique et le paramètre d’ordre bidimensionnel d’un superfluide.
On observe l’enroulement et le glissement de phase.
Abstract.
2014It is shown that in the infinite nematic liquid, the distortion waves can propagate when submitted to the elliptically polarized shear deformation. These waves are helical and their propagation can also be seen as a
rotation of the helical distortion. The analogy with the shear wave propagation in the rotating newtonian fluid is indicated.
The rotation of the distortion is observed in a finite nematic slab submitted to an electric field in order to prevent the relaxation of the distortion.
The analogy between the distortion and the two-dimensional superfluid order parameter is developed. The phase winding and slippage is observed experimentally.
Classification
Physics Abstracts
61.30
-67.40
1. Introduction. -The coupling, via viscous stresses,
between the director n and the flow velocity v, is one
of the factors which determine the original hydro- dynamic properties of the nematic liquid crys- tals [1, 2, 3]. Because of this coupling the viscometric flows such as simple shear flow or Poiseuille flow can
become unstable even for very low Reynolds numbers.
The instability phenomena of these viscometric flows
were investigated for several years through experi-
mental measurements and theoretical calcula- tions [1, 2, 3].
One of the most striking results was that the insta-
bility threshold in viscometric flows is determined
mainly by the value of the Ericksen number Er [3].
It was pointed out by Pieranski and Guyon [4] that
this result is not général ; the case of the elliptically polarized flow shows some original features :
A. The instability threshold is not determined by
the Ericksen number but by another dimensionless number which takes into account the frequency
of the elliptical shear flow [4]. The detailed experi-
mental and theoretical investigations of these insta- bilities can be found in references [6] and [5].
B. In the present paper we pursue the conjectures
of reference [4] and our aims are : (1) to show theore-
tically that the helical distortion waves can propagate in an infinite nematic liquid submitted to the elliptical
shear flow and to point out the analogy with shear
wave propagation in rotating fluid (section 2), (2) to investigate experimentally the effect of the elliptical
shear flow on the sinusoidal distortion in samples
of finite thickness (section 4), (3) to point out the analogy with the phase winding and phase slippage phenomena in superfluids (section 5).
2. Helical distortion waves.
-2. 1 UNPERTURBED
SHEAR FLOW.
-Let us consider an infinité nematic
liquid initially oriented in z-direction (ninit = (0, 0, 1))
and submitted to the elliptically polarized shear flow
Article published online by EDP Sciences and available at http://dx.doi.org/10.1051/jphys:01981004203045900
460
described by the following displacement field u :
where Exo and E00FFo are respectively the amplitudes of the
.
aux au
déformations
ai’ az ; all other components of the
deformation tensor Ê
=Vu are zero.
The velocity gradients Vu will induce the oscilla- tions of the director field via viscous torques. In the limit of small deformations (Eaxo, Eayo 1) the director components are :
where a2 and yi are the viscosity coefficient characte- ristic of the nematic compound used. Usually the
ratio (- a2 jyl) ranges between 0 and 1; the upper limit corresponds to the most common cases.
2.2 WAVE PERTURBATION.
-The altemating flows (1) and the distortions (2) are the background on which
we superpose the distortion waves
of small amplitudes (nxo, nsyo Exo, eayo « 1).
The frequency mi 1 is now supposed to be much
smaller than w, so that the perturbation ns may be considered as quasi-static. Because of the coupling
between the flow and director, the distortion (3) will
be accompanied by the flows of the same frequency w1 : :
The total distortion n = na + nS and flow v = va + vS
must satisfy the Leslie-Ericksen equations. Due to the
fact that cal was supposed to be much smaller than cv
these equations may be averaged over the period
2 nlw. This averaging procedure is presented else-
where [5]. For the purpose of the present calculations
we report only the final form of the averaged equations (eqs. (3.18), (3.19), (3.21), (3.22)) in reference [5].
where
a’s are the usual definitions of the viscosity coeffi-
cients [3] while K is the Frank constant in the approxi-
mation K11 1 = K22
=K33 = K (1).
From equations (5a) and (5b) we get :
Substituting equations (3), (4) and (6) in equations (5c) and (5d) we get the following system of the homo.
geneous linear equations for the amplitudes nsXO and nsyo :
2.3 DISPERSION RELATION. - The condition that the determinant of the equations (7) must be zero gives the dispersion equation :
The imaginary part imi of the frequency wi represents the damping factor due to the elasticity K. The real
part wi(= ± C03A9) determines the frequency of the
wave and is of the order of magnitude of Q (defined above) multiplied by the factor C which depends on
the viscosity coefficients of the nematic material.
Using the same values of the viscosity coefficients as
that used in reference [5] we calculate
and justify the initial approximation of the quasi-
static perturbations (mi « w).
(1) As observed by one of referees, in fact only one elastic constant
(K33) is involved in the case of the helicoidal distortion waves of
small amplitude.
2.4 HELICOmAL SOLUTIONS.
-Using the dispersion
relation (8) we obtain from equations (7) the following
relation between the distortion amplitudes :
If, arbitrarily, we set nxo to be a real number no, then the final expression for the distortion waves will be :
The solutions corresponding to + and - signs in the
above equations are nothing else but the left and right
hand winded helices rotating around z axis with the
angular frequency C03A9 in the same direction. This helical type of distortion is visualized in figure 1.
Fig. 1.
-The helical distortion waves. Their propagation can be
seen as the rotation of the distortion as a whole.
From the equations (4) and (6) we deduce that the shear waves associated with the helical distortions are
helicoidal as well. However there is a phase lag between
the distortion and the flow (given by equation (6))
such that the shear avs/oz is oriented at right angle to
the distortion ns at each point of the helix. Its effect will
only be a rotation of the distortion helix with the
angular velocity CQ. In other words we can say that because of this phase lag the distortion and the asso-
ciated flow are self-consistent.
2.5 ANALOGY WITH SHEAR WAVES IN ROTATING FLUID.
-In the newtonian fluid at rest the shear
waves cannot propagate because of lack of the restor-
ing stresses other than the viscous ones which are
purely dissipative. However, if we suppose that the fluid rotates as a whole with respect to the inertial frame of reference, then the Coriolis forces must be
taken into account. Their role is to provide the reac-
tive restoring stresses necessary for propagation.
Following reference [7] let us suppose that the fluid is rotating as a whole around the z axis with the angu- lar velocity co. Then let us consider a perturbation having the form of a transverse shear wave :
where the velocities Vx and vy are taken in the frame of reference (x, y, z) rotating with the fluid.
The perturbations (11) must satisfy the Navier- Stokes equations
-which in the rotating coordinates
are :
where v is the dynamic viscosity of the fluid. The right
hand sides terms are the Coriolis accelerations.
Equations (12) are analogous to the equations (7) :
-
the velocities v correspond to the distortions ns,
-
the Coriolis forces in equations (12) are perpen- dicular to the velocities v, while in equations (7) these
were the viscous torques which were perpendicular
to the distortions ns.
The dispersion relation obtained from equations (12)
is analogous to the previous one (eq. (8)) but the
orders of magnitude of the factors which are involved
are quite different :
-
The damping factor in the case of the distortion
waves was determined by the ratio K/y, which for
MBBA is of the order of 5 x 10-6 cm2/s ; in the
newtonian fluid such as water the dynamic viscosity
v
=ttlp is of the order of 10-2 cm2/s.
-
The angular velocity CQ, in the case of the distortion waves, is only a small fraction of w, while
the inertial shear waves rotate with the angular velocity 2 w.
3. Experimental.
-3. 1 PRODUCTION OF THE SHEAR FLOW.
-The experimental set up which we used to
produce the elliptical shear flow was described in details in reference [6]. Figure 2 depicts it only sche- matically. The nematic sample (MBBA) is oriented along the vertical axis z between two horizontal glass plates. Each glass plate vibrates independently with the frequency 03C9 in the horizontal plane ; one plate in the
x-direction and the other one in the y-direction.
A phase difference of n/2 is introduced between two vibrations. The respective motions of the plates then
can be written as :
462
Fig. 2.
-Creation of an elliptical shear in the nematic slab by
the combination of two perpendicular linear shears. These linear shears are obtained by the displacements of the two glass plates
in perpendicular directions ; - 03C9/ 203C0~ 203C0 - 200-500 Hz, xo and yo, the
amplitudes of the plates displacements are of order of a few microns.
The actual motion of the liquid in the gap of thickness D between the limit plates depends on the viscous
penetration depth :
where p - 1 g/cm3 is the nematic density and
For 03B4 « D the shear waves are damped near each plate and do not interfere. For 03B4 » D the damping
can be neglected and the vibrations of the plates create
two independent linear shear deformations of ampli-
tudes :
which, when superposed, correspond to the ellipti- cally polarized shear deformation described by the equations (1) and visualized in figure 2.
The inequality ô » D limit the upper range of
frequencies to 03C9 « 2 ~bl(pD2) ~ 104 Hz for the sam-
ple of thickness D = 100 pm. Due to the inertia of the moving parts in the experimental set up, the
frequency of excitation was additionally limited to
500 Hz so that in all experiments reported in this
article the deformation in the sample can be well approximated by equations (1).
3.2 CAN THE HELICOIDAL DISTORTION WAVES BE
OBSERVED ?
-The necessary condition, which must be satisfied in order to observe effectively the rotation of the helical distortion is that the damping factor
Kq2/yl (eq. (8)) should be smaller than the frequency
of rotation CQ :
The minimum value of the damping factor (in the case
where no external fields are applied) is imposed by the
thickness of the sample D ; the wave vector q = 2 ni À.
cannot be smaller than 2 niD. The frequency CQ
on the other hand is limited for two reasons : (1)
The amplitudes of the shear deformations must be small enough in order to satisfy the initial approxi-
mations of the theory (Exo, Eayo « 1) and (2) the exci-
tation (- Q as defined in reference [6]) must be small enough in order to avoid the flow instabilities. The
experimental results in reference [6] suggest that the instabilities cannot develop for :
The superposition of ( 16) and (17) leads to the following inequality
The fact that the upper and lower limits in this in-
equality overlap slightly suggests that the direct obser- vation of the distortion waves is rather beyond the possibilities of the unmodified experimental set up.
3.3 EFFECT OF THE ELECTRIC FIELD.
-The way to avoid the difficulty is to prevent the relaxation of the distortion by the application of electric field parallel
to the z axis. In MBBA a sinusoidal distortion (Fig. 3) :
develops when the electric field larger than the Free- dericksz threshold Ec is applied. Following this idea
the experimental set up was modified. Using the
limit glass plates precoated with the transparent InO
Fig. 3.
-Definition of a two-dimensional order parameter above
the Freedericksz transition.
electrodes, the electric field was applied and induced the permanent distortion in the sample (2).
3.4 INFLUENCE OF THE LIMIT CONDITIONS.
-The
homeotropic anchoring conditions (O(z = +D/2)=0)
at the limit plates impose the sinusoidal shape of the
distortion (19), the calculation of section 2 could
apply nevertheless to such a distortion because it can be
represented as a linear combination of two helical distortions of the opposite chirality. Consequently,
the sinusoidal distortion (19) could be expected to
rotate under the elliptical shear in the same way as the helical distortions (Fig. 1).
Unfortunately, the nonslipping boundary conditions
for the velocities v’(x(z
=± D/2) = 0) are not compa-
tible with the shear wave pattern (eqs. (4) and (6)).
Therefore there exists a boundary layer close to each glass plate and the theory developed in chapter 2 is only an approximation to the real experimental
situation. In particular, the angular velocity of the rotating distortion can slightly differ from the pre- dicted one (which equals to CQ) by the numerical factor C ’(03C9’1 = C’Q).
3.5 OBSERVATION OF THE DISTORTION IN THE POLA- RIZING MICROSCOPE.
-The distortion in nematic slab is easy to monitor between crossed polarizers
with the microscope. The interferential image allows
the straightforward determination of both the phase (p
and the amplitude cos 03B8m (Fig. 3) :
-
isoclines indicate the isophase lines (modulo n/2) whére the director n 1- is parallel to the polarizer
or to the analyser,
-
isochromes indicate the actual amplitude of the
distortion.
Let us consider as an example the singularities
characteristic of the Freedericksz transition in the
homeotropically oriented sample known as umbi-
lics [8] (Fig. 4). These defects were observed to occur
in our samples spontaneously. In the polarizing microscope, they appear as black crosses (Fig. 5) as expected from the configuration of the corresponding
distortions (Fig. 4) (see also section 4).
Fig. 4.
-The three-dimensional structure of umbilics s
=+ 1 and s
= -1. The black lines are parallel to the director. The
arrows represent the projection of the director in the mid-plane.
Fig. 5.
-Photographs of a pair of umbilics s
=+ 1 and s
= -1 observed in the polarizing microscope. Under the elliptical shear, the umbilics rotate in opposite directions. The photographs are separated by time intervals of a few seconds (see text).
4. Evidence for the rotation of the distortion.
-The first evidence for the rotation of the distortion
(predicted in section 3.4) is provided by the behaviour
of the pair of umbilics (+ 1 and - 1) when the elliptical shear is applied to the sample. The figures 5a, b and c show the configuration of isoclines at three différent times ta = 0 s, tb = 5 sand tc B= 10 s.
It is evident from these photographs that the black
crosses characteristic of the umbilics are rotating :
The upper cross, which corresponds to the s = + 1
umbilic rotates counterclockwise whereas the lower umbilic (s
= -1) rotates clockwise.
Let us consider more in detail the transformation of the umbilic s = + 1. The figures 6a-6h show how
e) The electrohydrodynamic instabilities are avoided because of high frequency (- 104 Hz) and low value (- 5 V) of the voltage
used in experiment.
it transforms under the uniform clockwise rotation of the distortion. Each of the eight configurations i$
unique, nevertheless the corresponding isoclines have
all the same shape of a cross. During the successive
Fig. 6.
-Eight configurations taken by the umbilic s
=+ 1 under the elliptical shear. The arrows are the directions of nl in the
mid-plane of the cell. The elastic energy varies during this cycle.
464
transformations the cross is rotating in the counter-
clockwise direction.
The detailed observation reveals that the angular velocity of the cross corresponding to the s = + 1
umbilic is not uniform. This is probably due to the anisotropy of the elastic constants :
and can be explained as follows :
The set of the eight configurations { a, ..., h } can
be divided in three subsets {a, e }, { b, d, f, h } an4 {c, g} with different elastic energies E. The inequality (20) suggests that :
The energy differences result in elastic torques which slow down or accelerate the rotation of the cross.
The behaviour of the umbilic s = - -1 is different.
The hyperbolic configuration (Fig. 4b) is not affected by the (clockwise) rotation of the director other than
as a uniform solid body rotation of the whole configu-
ration (in the clockwise direction). In the microscope
this is seen as a uniform rotation of the isoclines.
The angular velocity of the umbilics was observed to be dependent on the amplitude and sign of the quantity xo yo m as expected from the relationship :
5. Phase winding and relaxation.
-The successful
experimental evidence for the rotation of the distortion under the action of the elliptically polarized shear flow provided us with a basis on which we developed a series
of experiments which have an intrinsic value as a way to visualize the winding and relaxation phenomenon
of the two-dimensional order parameter.
5. .1 INTRODUCTION OF THE TWO-DIMENSIONAL ORDER PARAMETER. ANALOGY WITH SUPERFLUIDS.
-The dis- tortion (19) is characterized completely by the pro-
jection n 1. of the director in the plane (x, y) (Fig. 3).
From the formal point of view the vector n 1. can be considered as a two-dimensional order parameter
(j n 1. 1 = cos Bm, cp) analogous to that of superfluids
or supraconductors. In superfluids, for example, the
order parameter being a wave function
cos 0. in the present case will correspond to the ampli- tude 1 03C8| and the azimuthal angle cp to the phase ~.
Following this analogy the umbilics (Fig. 4) are equi-
valent to vortices and antivortices in superfluids. It
must be emphasized that the important experimental advantage of the nematic liquid crystals is the straight-
forward visualization of the order parameter n~ ~
by the microscopic observation between crossed
polarizers (Sec. 3.5).
5.2 GENERAL PROPERTIES OF THE NONSINGULAR PHASE FIELD.
-The general expression for the phase
field in the nematic sample is given by
where C’ is the numerical factor defined in section 3. 4.
Experimentally, the interesting characteristics of the phase field, which can be observed, are the velocity
of isoclines and their density. The isoclines being
defined as the lines of the constant phase, the phase
variation Vqp.ôr, produced by the displacement ôr,
must be annihilated by the phase rotation C’ 03A9 bt
during the time interval ôt :
C’ Q(x, y) bt + V(p - ôr
=0 . (24) C’Q(x, y) ôt + V~.ôr
=0. (24)
From this relation, the velocity v.1, measured in the direction perpendicular to the isoclines lines, can be
determined as follows :
where a~, the unit vector perpendicular to the isoclines,
can be calculated as
The density of isoclines is directly proportional to
the modulus of the phase gradient :
In the case when the gradient of the angular velocity q
exists across the sample, the isoclines density will
vary in time. Such a situation, possible to realize experimentally, as we will see in the following, is expected to give rise to the phenomena of the phase winding and relaxation.
5. 3 EVIDENCE FOR THE PHASE WINDING.
-The
angular velocity 03C91’ = ~ = C’ 03A9 is a function both of the material constants such as viscosities a’s and y 1
and of the quantity xo yo wlD2 which is determined by
the characteristics of the shear flow apparatus. In the case, when the thickness D varies across the sample,
the angular velocity C’ Q is a function of the position
in the sample :
A simple configuration to realize is that of the wedge,
where the limit glass plates are not parallel but form
an angle a. Then, we can write :
where D * is the thickness of the sample for x = 0 (Fig. 7), D is supposed to be a function of x only.
Let us suppose now that at time t = 0 the order parameter nl ~ is uniform in the sample and parallel to
the x axis (cp(x, y)
=0). According to the equation (27)
at time t the density of isoclines (measured along the
x axis) will be :
while their velocity as calculated from equation (25) is :
Fig. 7.
-Wedge parallel to the y axis between, the glass plates.
We observed directly, using the polarizing microscope (and simultaneous recording on the photographic film), the transformation of the isoclines configuration
under the action of the elliptical shear. The following
sequence of events was observed :
-
At time t = 0, the homogeneous aspect of the sample was indicative of the uniform orientation of the order parameter nl.
-
After the application of the elliptical shear the
isoclines started to appear at the thin edge of the sample
and to move in the direction of the increasing thickness (x axis).
-
The formation of the new isoclines was more rapid than their evacuation and as a result the isoclines
were progressively accumulated in the sample (Fig. 8).
Fig. 8.
-Photograph of the wedge shaped cell as observed between
crossed polarizers. The black lines are isoclines. Several umbilics disturb the isoclines alignment. The isoclines density decreases
in the x direction, as the thickness increases.
-
The density of isoclines was observed to increase
at a given point accordingly to the formula (30).
Also, at a given time t this density was observed to
decrease with the coordinate x (as expected from
eq. (30)).
-