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Orientational optical non-linearity near the instability of nematic liquid crystal flow over an inclined plane
Yu. S. Chilingaryan, R.S. Hakopyan, N.V. Tabiryan, B. Ya. Zel’Dovich
To cite this version:
Yu. S. Chilingaryan, R.S. Hakopyan, N.V. Tabiryan, B. Ya. Zel’Dovich. Orientational optical non-
linearity near the instability of nematic liquid crystal flow over an inclined plane. Journal de Physique,
1984, 45 (3), pp.413-420. �10.1051/jphys:01984004503041300�. �jpa-00209771�
Orientational optical non-linearity near the instability
of nematic liquid crystal flow over an inclined plane
Yu. S. Chilingaryan, R. S. Hakopyan, N. V. Tabiryan and B. Ya. Zel’dovich (*)
Physics Department of Yerevan State University, 375049, Yerevan, U.S.S.R.
(Reçu le 20 avril 1983, révisé le 7 octobre, accepté le 27 octobre 1983)
Résumé.
2014On étudie le problème de l’écoulement d’un nématique sur un plan incliné. Dans le cas où le directeur est ancré sur la surface du plan incliné perpendiculairement à la direction de la gravité et à celle de l’écoulement, on prédit une instabilité spécifique de l’orientation dont on calcule le seuil. On étudie la non-linéarité optique d’orien-
tation du nématique au voisinage du seuil de l’instabilité d’écoulement.
Abstract.
2014The problem of the gravity flow of nematic liquid crystal (NLC) mesophase over an inclined plane is investigated. In the case when the director of NLC is strongly anchored on the inclined plane surface perpendi-
cular to the gravitational force and flow direction, a specific orientational instability arises for which the flow threshold value is obtained. Orientational optical non-linearity at the threshold of NLC flow instability is investi-
gated.
Classification Physics Abstracts
47 . 20 - 61. 30G
1. Introduction.
The coupling, via viscous stresses, between the direc- tor n and the flow velocity v, is one of the factors which determines the original hydrodynamic properties of
nematic liquid crystals (NLC) [1-5]. Due to this coupl- ing, viscous flow such as simple shear flow or Poi- seuille flow can become unstable even for very low
(10-3-10-4) Reynolds numbers. The instability phe-
nomena of these viscous flows were investigated experimentally and theoretically in detail [1-5]. In particular two types of instabilities are mentioned.
The first one corresponds to a distortion of the director which is uniform in the plane (no; vo) composed of the
undisturbed director and the flow direction. The second one corresponds to a so-called roll instability (with the roll axis parallel to the flow direction Oy).
Both instabilities arise at several critical values of shear rate and the threshold of the first type of insta-
bility is lower than the threshold of the second type.
The problem of ordinary viscous fluid flow over an
inclined plane is well known (see [6], § 5). If the boun-
dary conditions on the lower plane correspond to
strong anchoring but the upper surface of the fluid is free, the velocity profile has the form of the parabola
(*) Institute on Problems in Mechanics, prospect Ver- nadskovo, 101, 117526, Moscow, U.S.S.R.
and it is easy to obtain the dependence of the steady
state thickness of the layer on flow.
The theoretically predicted and experimentally
verified orientational optical non-linearity of liquid crystals [7, 8] is a matter of intensive investigations at
present. In particular in several works (see [9, 10] and
the references therein) NLC optical non-linearity
near the Fredericks transition induced by a magnetic
or electric field is discussed, as well as near phase
transitions between liquid crystals modifications.
In the present paper we consider the problem of
NLC flow on an inclined plane assuming the conditions
of zero velocity and strong anchoring on the plane.
It is shown that for the definite geometry a specific
orientational instability arises at some threshold
value of flow. This threshold value and distortion
profiles are obtained for the case when the velocity
and director distortions are uniform in the plane (no; vo). The orientational optical non-linearity at the
threshold of the considered type instability of NLC
flow over the inclined plane is discussed.
2. Recording of boundary conditions.
A quantity Q (em 3 /s) of the liquid crystal, which is
contained in the xy plane and has a width along the
x axis given by l, continuously flows along the y axis
which is inclined at an angle a with respect to the
Article published online by EDP Sciences and available at http://dx.doi.org/10.1051/jphys:01984004503041300
414
Fig. 1.
-Geometry : liquid crystal with thickness h flows
along the direction ey over an inclined plane which makes
angle a with the horizontal. The boundary conditions cor-
respond to no
=ex.
horizontal. Then at not very high flow velocities (i.e. for not very high Q) steady liquid flow with a
thickness h occurs. If the boundary conditions on the inclined plane (plane z = 0) correspond to a director
orientation along ey (no
=ey) or along ez (no
=ez),
then in the whole volume except in a boundary layer
of width ç, where
the molecules will be reorientated by the flow, making
an angle 0s = arctg (--’3/a2) with the axis ey and stay in the plane (y, z). Here K is the average elastic cons-
tant and q the viscous coefficient for the corresponding geometry.
We shall discuss in detail the situation when, on the boundary z
=0 molecules are anchored along
ex (n°
=ex). On the same surface the condition on the flow velocity v is v (z
=0)
=0. The boundary condi-
tions on the free surface z = h have the form
where Ki are the Frank constants; and (Ja is the sur-
face tension anisotropy. At the free surface the shear stress vanishes and this leads to the first condition in
(1). The two last conditions are obtained by consider- ring the addition to the surface part of the free energy
depending on the orientation having the form A =
0.5 6a(nez)2 [12, 15, 16]. ca = 0 if the surface does not influence the director orientation. In the other limit (fa -> oo the surface strictly orients the director in the
layer plane (if (fa > 0) or perpendicular to it (if 7a 0).
Since we consider a situation where the undisturbed director direction is planar and homogeneous over
the whole volume of the NLC, it is necessary to consi-
der 6a > 0. In this case the orienting action of the free surface supports the director planar orientation.
Such a situation can be experimentally realized with the nematic PAA for example [17,18].
When the flow is very weak the above mentioned orientation (n°
=ex) will be unperturbed over the
whole volume due to elastic effects. The viscous torque
acting on the director is zero and the viscosity, measur-
ed in this geometry, is fla = 0.5 a4. If we consider the inclined plane to be infinitely long, we obtain from
(A. 14) for velocity profile.
Then the pressure distribution is
It is easy to define the relation between the steady
state thickness h of LC and its quantity of flow Q, giving on the upper part of inclined plane :
All these expressions coincide with those for an ordi- nary liquid by a suitable definition of viscous cons-
tant na-
3. The system of linearized hydrodynamic equations.
Consider a light wave with wave vector and polariza-
tion vector lying in the plane (X, Z), so that K = (Kx, 0, KJ, E
=(Ex, 0, EJ, and which is incident on
the described system. At sufficiently high flow velo-
cities the stationary profiles of velocity (2) and direc-
tor no are disturbed even without the presence of an
electromagnetic wave.
Let us denote by bn = (0, n r n _,), bv = (’Dx’ ’Dy, CU,- )
and P the orientation, velocity and pressure distur- bances. Equations coupling these disturbances can be obtained by linearizing (A. 12), (A. 14) and the equa- tion of uncompressibility OVi/OXi == Oi Vi = 0. We
carry out the linearization for the problem which is homogeneous in the inclined plane, i.e. we do not
discuss the domain structure (010y
=0), and the roll
instability (%x = 0). Then we obtain the following
system of equations :
where the symbol * means complex conjugation; ga = ell jj
-
E1 is the anisotropy of the mesophase dielectric
constant at the light frequency; S is the velocity gradient of the undisturbed flow along z :
fla’ fib are the Miesowicz viscosity coefficients :
The director perturbations lead to the field modification in the medium. However we can consider that in the
equations (4a)-( 4 f) E const. because we are interested in weak perturbations of the director proportional
to the light intensity. In the same approximation the director reorientation does not give rise to an Ey component
of the light field and therefore there is only y component of the torque acting on the director. Thus we only consi-
der (for the stationary problem) the z-dependence of the disturbances. In this case, as for the simple shear or
Poiseuille flows problems, one can show that ’U’y = ’U’z
=p
=0 everywhere, which corresponds to a distur-
bance of v(z) of the form bv = ex’U’x(z). From the equation (4c) and boundary conditions at z = 0 and z = h
we have :
With equation (6), equations (4a) and (4b) take the form :
Performing the transformation :
We obtain the dimensionless equations :
In this notation 4J., is determined from the equation :
where CÜx = h.1 (13 I crJx/K1.
Then, using new variables U = a2/3.(ii, + nz), W = a2/3.(ii, - nz) and X
=all3 Z from (9) we obtain two
uncoupled equations :
416
The boundary conditions (1) in new variables take the form :
where X1
4. Investigation of flow instability.
General solutions of equations (11 a) and (llb) without an external electromagnetic wave are expressed through
the Airy functions Ai(X ) and Bi(X) [20] :
where A1, A2, B1 and B2 are arbitrary constants. From the boundary conditions (12) we get four homogeneous equations for four unknowns A1, B1, A2 and B2. This system has non-trival solution when its determinant is zero.
Thus we shall find an equation for critical X1, i.e. for critical flow Qc :
where
D1, D2 are constants connected with Az(O) and Bi(O) :
Critical thickness he and flow Q, are expressed through the root Xl of equation (14) :
Consider the influence of the surface forces on the value of the threshold. We present the numerical solutions of equation (14) for the cases far = 0 and Ea -+ oo because we do not know the value of NLC surface tension
anisotroPYO"a.If.Ea = 0 we get from ( 14) (F1 + D 1 ) (F2 + D 1 )
=0 and, because F 1 (XJ is positive for all Xl > 0
we have F2 = - D1 and, therefore, X@ = 1.98. For example from (16) we obtain h’ 3 sin a = 23.5 gm and cor-
respondingly the critical flow Q 0 "/l l-- 1.04 x lO- 5 cm2 s-t for the parameters characteristic for LC p = 1 g/cm3, K1 = 6 x 10-’ dyne, K2
=4 x 10-’ dyne, Ila = 0.25 poise, fib = 0.4 poise, a2 = - 0.77 poise, CX3
= -0.012
poise [ 11 ].
When Ea -+ oo from equation (14) we get F1 = F2, therefore X c = 2.347. We have h 3 sin a 27.85 um
and correspondingly for critical flow we obtain Qoo/l ~ 1.7 x 10- 5 cm2 s-1 for above mentioned parameters.
We obtained that the threshold in the case (Ja -+ oo is somewhat greater than in the case ca = 0. This is connected with the circumstance that the surface force supporting the director undisturbed orientation increases with the increase of the a..
Knowing Xi we can obtain the disturbances profiles near the threshold, up to an indefinite constant multi-
plier. To an accuracy of two decimal places we find :
where A and B are arbitrary constants.
Let us note that at z = 0 X = X 1 and at z = h X = 0.
’Ù’ x can be found from equation (10) by integrating.
The profiles of disturbances nY’ iíz and ctJ x at Ea = 0, ooare given in figure 2. As can be seen on figure 2 the profile of nz essentially depends on the value of ca in contrast to the quantities ny and ’BJx. This is connected with
the given boundary conditions (1). For obtaining the steady state amplitudes of disturbances above the threshold it is necessary to solve a non-linear problem. We will not discuss such a problem in this paper.
5. Orientational optical non-linearity near a flow instability.
Dividing both parts of equations (l la) and (lib) by I we get equations whose solution is given by the Airy func-
tions Ai(X ), Bi(X ) and Gi(X ) :
’
where A1, A2, B1 and B2 are constants to be determined from the boundary conditions (12).
Near the threshold of the instability which would have the flow on the inclined plane without a light field, they have the form
where i
In particular in the case of Ea = 0, inserting numerical values for the parameters in (18) and omitting higher order
terms, we have :
When X. 0 0 the critical index for all four parameters AI, A2, B1 and B2 is the same and is equal to - 1. For example when Ma --> oo we have :
Fig. 2.
-Disturbance profiles nY’ nz at I a
=0 (a) and ¿a -+ oo (b). Disturbance profile of ’BJ x (c).
418
6. Discussion.
NLC flow on an inclined plane is considered in the present paper. The instability of such a flow corresponding to
director disturbance depended only on the z coordinate transverse to the layer is investigated. The physical
reason for the instability is the decrease in the effective viscosity with a decrease of the angle between the director and velocity [ 13], and this decrease is the same for positive and negative bn. Mathematically this is connected with
inequalities a2 0, a3 0, a2 I > I a3 I which are valid for most of NLC.
.