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Spinodal decomposition in two-component smectics

G. Sigaud, C. Garland, H. Nguyen, D. Roux, S. Milner

To cite this version:

G. Sigaud, C. Garland, H. Nguyen, D. Roux, S. Milner. Spinodal decomposition in two-component smectics. Journal de Physique II, EDP Sciences, 1993, 3 (9), pp.1343-1355. �10.1051/jp2:1993205�.

�jpa-00247911�

(2)

Classification

Physics

Ab.itia<.ts

05.70J 64.70M 64.75

Spinodal decomposition in two-component smectics

G.

Sigaud ('),

C. W. Garland

(', *),

H. T.

Nguyen ('),

D. Roux

(')

and S. T. Milner

(2)

(') Centre de Recherche~ Paul Pascal, CNRS, Universitd de Bordeau~ I, Av. A. Schweitzer, F-33600 Pe%ac. France

(2) Exxon Research and

Engineering,

Annandale, NJ 08801, U-S-A-

(Receii.ed lo Mw.cfi 1993, ac<.epted 9.time 1993)

Rdsumd. Les aspects originaux de la

ddcompo~ition

spinodale entre deux phases smectiques A de

compositions

diffdrentes sont

analysds

par diffusion de la lumibre et

microscopie

optique. Nous

montrons que cette ddmixtion caractdrisde par un angle entre le~ vecteurs d'onde [es plus intenses

et la normale aux couches est le r6sultat de l'instabilitd du mode

baroclinique.

Abstract. -A two-component smectic undergoing a demixing tran~ition to two coexisting

smectic pha~es exhibits a novel

spinodal

pattern as observed by

light

~cattering and

optical

microscopy. We show that this

~pinodal,

characterized by a

prescribed

angle between the mo~t intense wavevectors and the layer normal, is the result of the instability of the baroclinic mode of

two-cojnponent

smectic hydrodynamics.

1. Introduction.

When an

initially homogeneous

system is driven to an unstable state in such a way that

nucleation is avoided,

phase separation

processes

through

the

growth

of fluctuations in

composition

at wavevectors q i q~. this defines a

spinodal decomposition

and results in a concentration

profile throughout

the medium.

Scattering techniques

are most suitable to

give

evidence of this

phenomenon

in the

reciprocal

space : the characteristic pattem is a

ring

or halo

in which the maximum

intensity corresponds

to the wavevector of the fastest

growing

fluctuations

(q~), Experimentally

the

simplest

way to achieve

spinodal decomposition

is a

« critical

quench

» in which the temperature of a

homogeneous sample

of critical

composition

is varied as

rapidly

as

possible through

the critical

point.

The

phenomenon

can also be viewed in the direct space with an

optical microscope provided

that there exists a

sufficiently large

difference in the refractive indices of the two

separating phases.

(*) Present address :

Department

of

Chemistry,

Massachusetts Institute of

Technology, Cambridge,

MA 02139. U-S-A-

(3)

A second

important

feature of

spinodal decomposition

is its time

scaling.

At very short times after

quenching

the

intensity,

of the

scattering

is

expected

to grow

exponentially

with its

position

unaffected

(q~

=

Const.,

Cahn's

regime).

At

longer

times the fluctuations at

longer wavelengths

are

favored,

which results in the

collapse

of the

ring.

For

isotropic

systems the

radius then decreases with a power law q~ oz

t~

with

=

for the

early

stage and 3

= -1 later

[I].

The rate of the evolution

depends

on the time for diffusion

through

a

correlation

length,

t~

=

D~ '

f~,

which can be

expressed

in terms of the

depth

of the

quench (AT), viscosity

(Y~

),

and characteristic bare correlation

length (fo)

D

=

Do

~~ ~ '

=

~ ~~ ~ ~

and f

=

to

~~ ~ A ~~ ~~ (l )

Tc ~1

Tc

Tc

to

Thus,

i~ =

) ) 11 )

=

~

°

) (2)

c~'~ ~~

~"

~~ c~

~~~~~

y and v are the critical exponents that characterize the

susceptibility

and correlation

length, respectively.

A

large

t~

corresponds

to a slow

decay

in the diameter. For

example,

the

study

of the

dynamic~

of

phase separation

over reasonable time scales

Ii-e-,

100

s)

in

simple liquid

mixtures

requires

very shallow

quenches

(~ 5 mK ), which means

equipments

with

extremely good

thermal stabilization

(10~~

K

[I ]. Experiments

on systems in which t~ is

large

are thus

highly

attractive. Some such

experiments

have been conducted in viscous media such as

polymer

solutions or blends

[2, 3]

or in systems with

large

correlation

lengths

such as

microemulsions

[4].

Also

investigated

more

recently

have been the characteristics of

phase separation involving mesophases

in a nematic solution of a

liquid crystalline polymer [5]

and between a

lyotropic

lamellar

mesophase

and an

isotropic

sponge

phase [6].

The exponent of the power law which fits the decrease of the wavevector as a function of time looks

quite

similar to the classical value obtained in

simple

fluid systems

although

unusual

anisotropic

features could be noticed in the domain

growth.

Recently

a critical consolute

point

has been observed in a two-component smectic A

phase [7].

We present a

study

of the

spinodal decomposition

in this system. In the

experimental

section of this paper,

light scattering

and

optical microscopy pictures

recorded

during phase separation

are described and

analyzed.

These

experimental

observations are consistent with the

theory

for

spinodal decomposition

in such ordered fluids which is

presented

in the theoretical section.

2.

Experimental

section.

2, SAMPLE PREPARATION. The system in which a

phase separation

between two smectic A

phases

is obtained is a

binary

mixture

involving

the

6-cyanonaphtyl-2 4-decyloxybenzoate (compound A)

and the

4-hexyloxyphenyl 4-perfluoroheptylbenzoate (compound

B).

CioH2i°-)O_ O ~

(A)

~

C7Fiifi-~°2-filC6H13

(B) The

phase diagram

has been

published previously [7]

and is shown in

figure1.

(4)

Isotropic liquid

N cJ

~

F- Smectic A

phase

0,0 0,2 0,4 0,6 0,8 1,0

Volume fraction of mesogen B

Fig.

I.-Composition-temperature

phase diagram for the

liquid crystalline

binary ~ystem 6-

cyanonaphtyl-2

4-decyloxybenzoate 5 (left) +

4-hexyloxyphenyl 4-perfluoroheptylbenzoate

(right) (from Ref. [7]). N denotes a nematic

region.

The

experiments

have been

performed

on a mixture with a

composition

as close as

possible

to the critical

composition (volume

fraction of B ~~

~ =

0.44

corresponding

to mole fraction

~i~

~ =

0,40 and

weight

fraction

w>~ ~ =

0.51).

The basic set-up for

light scattering experiments

is described in

figure

2. A

typical quench

was a few tenths of

degrees deep starting

from about

? °C above the critical temperature

(final

temperatures were 0.2 °C and 0.4 °C below the

critical temperature in the two

experiments

for which

quantitative

data are

given below).

Cooling

was obtained I>ia two thermostats.

Using

a three way valve the fluid from a water bath maintained at 10 °C was allowed to circulate in the heat

exchanger

of the oil bath

regulating

the temperature of the

sample just

the time necessary to reach the final temperature of the

quench.

It took

typically

one minute to

bring

the cell at the set temperature. For

optical

observations the

thermostated cell was

simply

moved on to a

microscope

stage. The same

sample

and

sample

holder have been used for both

light scattering

and

microscope

observations. The

sample

semi transparent

screen cold bath

z

video recorder

He-Ne )aser

Fig.

2.

Light

scattering set-up.

(5)

holder was a 100 ~m thick

glass

cell. Suitable

coatings

were

deposited

to obtain two different orientations of the smectic

planes

either

homeotropic (planes perpendicular

to the

light

beam,

Fig. 3a)

or

homogeneous planar (planes parallel

to the

light

beam,

Fig. 3b).

The orientation of the

sample

with

regard

to the

polarization

of

light

is

specified

in

figure

4.

~" -',,

'lfl(#t9+~-,".-

i°"

~%lfi#I

(

E

°ating

~

@JaSi jl&SS

al ' ' ' '

b

' ' ' ' ' '

' ' ' ' ' '

be%m

belm1

' ' ' ' ' '

' ' ' ' ' '

Fig.

3. The two different orientation~ of the ~mectic A layer~ in the cell a)

homeotropic

b)

planar

homogeneou~.

Z beam

i

' n

" Y

X

Ey

Fig.

4. Orientation of the sample with respect to the polarized laser beam in the planar

configuration.

2.2 RESULTS.

Light scattering

patterns recorded in the course of

spinodal decomposition

from

planar

oriented

samples

are

anisotropic they

consist of four blobs

symmetrically

located, as shown in

figure

5 in which the orientation of both the director and the

polarization

is vertical. This four-leaved clover geometry is reminiscent of the pattern

previously reported

for a shear induced transition in

lyotropic

systems

[6] involving

a lamellar

phase.

Moreover the sequence of

pictures

in

figure

5

gives

evidence for the

collapse

of the

scattering

pattern. Two series of

images corresponding

to two different

quenches

have been

analyzed

in order to

study

the time evolution of the

position

of the maximum scattered

intensity.

The

quench depth

AT

= T~ T was 0.2 K for

quench

and 0.4 K for

quench

2.

Figure

6 shows a

logjo-logjo

plot

of the modulus of the wavevector in

(angstr0ms)~'

as a function of time in seconds for both

quenches.

These results can be

compared

to the classical power law

(represented by

the dashed line

corresponding

to a 0.33

slope)

over some time range. One can note the saturation of q at the very

early

stage of the

decomposition

for the shallower

quench although

the

(6)

Fig.

5.

Sequence

of

light scattering

patterns selected from the video-recording on

quench

I for a planar homogeneou~ sample. Time interval between two pictures i~ 5 s. axis (orientation of both the

director and the

polarization,

see Fig. 4) is vertical.

-3

+ AT=0.2K

+ X + x AT=OAK

x x.

x +

x +

+

~ x *

w X +

o +

-4

0 2

log

t

Fig. 6.-logj~-logj~ plot

of the wavevector q a~ a function of time t for quenches (+:

T T 0.2 K) and 2 (x T T 0.4 K). The dashed line

corresponds

to 4

~ ' 3

(7)

faintness of the

scattering

at these

early

times does not allow a

highly

reliable observation.

Also noticeable from these curves is the trend toward

larger slopes

at

longer

times in both

cases, which suggests a cross-over as observed with other systems

[1,

4,

6].

In addition,

image

analysis

indicates that the

angle

between the direction of maximum

scattering

and the director of the smectic A

phase

decreases

regularly

with time from a finite value

ranging

between 60°

and 70° at t

= 0, as shown in

figure

7.

~~

fi

x AT = 0.4 K

65 ~ +

~

x +

~

*

+

~

~

~

+

z X

~

x

~

x .

55

x

50

~ ~~ ~~

t/ s ~~ ~~ ~~

Fig. 7. Plot of the angle & between the direction of maximum scattering and the director (Y axis) as a function of time. + :

quench

I, x quench 2.

It is also

interesting

to discuss the duration of the two

experiments.

As

expected,

the faster

collapse

occurs for the

deeper quench. Comparatively

the

decomposition proceeds

at a slower rate in our system than in

simple liquids owing

to the

higher viscosity.

Thus

spinodal decomposition

can be observed over a reasonable interval of time for

fairly deep quenches.

Indeed the kinematic

viscosity

of a smectic A

liquid crystal

is

roughly

two hundred times

larger

than the

viscosity

of the usual

isotropic liquid

(Y~s~

w 200 cP and the time scale is

expanded by

the same factor. Then,

provided

that the bare correlation

lengths

are

comparable

in both

cases, one obtains from

equation (2)

~~S~ 'iS,

~Y ' '

~~simpleliquid ~l~impleliquid

Using

mean-field values for the exponents y + v =

1.5 one can estimate that a 0? K

quench

on the smectic A mixture would result in the same rate of

decomposition

as a 5-10 mK

quench

on a

simple liquid mixture,

which is consistent with the results in reference

[I].

The fabric-like textures observed in the direct space are also

highly

characteristic with a mesh size

increasing

with time ; see

figure

8 (the orientation of the director is

approximately

S-W--N-E- in both

Figs.

8 and

9).

These observations

corre~pond

to a late stage of the

decomposition compared

to the

light-scattering experiments

since

deeper quenches (AT

=

0.9-1 K

typically)

are

performed

in transmitted

light microscopy

to

produce enough

contrast.

The ?D-Fourier transforms of these

pictures nicely

confirm the geometry of the

light scattering

patterns

(Figs. 9a-d).

The

corresponding

wavevectors have been estimated from

figure

9.

(8)

Fig. 8.

Sequence

of

microscopic

textures observed

during

the course of

decomposition

(quench is different from quenches and 2). Time interval between two pictures is 5 s, with A

being

the earliest picture. The orientation of the director is

approximately

S-W--N-E- The actual size of the field in each picture is (175 ~m x 175 ~m).

These

microscope

data can be combined with the data from the

light-scattering experiments

to

produce

the

scaling plot

shown in

figure

10. This

scaling plot

has been made for mean-field values for the exponents. It confirms an increase in the

slope

~fi at

longer

times. In the case of smectic A-smectic A transitions dominated

by

difference in

layer

thickness

(where coexisting phases

do not differ

appreciably

in

composition),

a

special non-Ising

critical

point

is

predicted [8],

but the exponent values for these systems are not yet well established and such

non-Ising scaling

cannot be tested.

Finally

the

quenches performed

on a

homeotropically aligned sample provided

no noticeable

scattering.

One can

explain

this behavior if the difference in the refractive indices of the components is

quite

small in this orientation. One does not expect an

anisotropic

pattern in this

case and the

scattering

of

light

over a

ring

instead of

being

focused within four spots would result in an insufficient

intensity.

A very

fuzzy picture

is observed with the

optical microscope

and no useful data could then be obtained from this

configuration.

3. Theoretical section.

We may summarize our

description

of this novel

spinodal

as follows. The

spinodal

pattern

results from the

growth

of the most unstable modes of the two-component smectic

hydrodynamics

below the critical

point.

A

simple description

of two-component smectic

(9)

Fig. 9. 2D-Fourier transforms of the

pictures

in

figure

8.

'

"

+ +

~ 'x+

*+~

*

$

-2

o

o o

o

3

~ ~

log

~

~ ~

Fig. 10. Log-log plot of the scaled wavevector q *

as a function of scaled time r for the light

scattering experiments

(+: AT =0.2K, x: AT=0.4K) and an

optical

observation lo AT=0.9K).

T T~ v T T~ (Y +v

~~ -

T~ ~ and T

=

T~

t. MeanfIeid exP°rents Y = ~ =

0.5 have been

used. The dashed lines

correspond

to the classical values 4

= and ~b -1.

3

(10)

Fig,

il. Sketch of the

layer displacement

in the baroclinic mode. Note the

oblique

wavevector.

hydrodynamics [9, 10]

above T~ contains

coupled equations

for the smectic

layer displacement

u, the concentration c, and the transverse momentum g~. The

layer displacement

and

concentration variables are

coupled

in the free energy because the

layer spacing

is different for

the two mesogens

[7]

and thus a function of concentration. The three first-order time-

dependent hydrodynamic equations give

rise to three

hydrodynamic

modes : a

pair

of

propagating

second-sound modes, and an

overdamped

«baroclinic

» mode, in which the

eigenvector

is a mixture of

layer displacement

and concentration variation (see

Fig.

II ).

Near the critical

point

of such a system, the slowest

[I II hydrodynamic

mode is made slower

by

the

vanishing susceptibility

critical

slowing

down

») [12]

in the present case this is the

overdamped

baroclinic mode.

Upon

a critical

quench,

this

critically

slowed mode becomes unstable and grows

[13].

Near the

spinodal,

where the

growth

or

decay

rate of the baroclinic mode is small

compared

to the

frequencies

or relaxation rates of all other modes, the

dynamics

is well described

by

an adiabatic

approximation,

in which the time derivatives of all non-

critical variables have

ordinary

relaxation rates, and so relax to values such that the

hydrodynamic

« forces » on these variables

vanish,

and we obtain a

single

first-order time-

dependent equation

for the

growth

of the baroclinic mode.

The

fastest-growing

wavevector

points

in an

oblique

direction for two basic reasons. First, the

diffusivity

of the mesogen concentration is

strongly anisotropic,

with molecules

diffusing mostly along

the

layers

; this suppresses the

growth

of fluctuations with wavevectors

parallel

to

n

(z-axis).

Second, the

spinodal corresponds

to the

vanishing

of B, the smectic

layer compressibility

at constant chemical

potential,

so that the

growth

of the unstable baroclinic mode is driven

by

a «

negative layer compressibility

». This

requires

the wave,,ector to have

some

projection along

n. Our detailed calculations below show that the

angle

between the most unstable wavevector and the =-axis is related to the fourth-order elastic coefficients.

Our

description

of the free energy

density

and

hydrodynamic equations

for a two-component smectic is taken from Nallet et al.

[9]

this system was

originally

described

by

Brochard and de Gennes

[10].

The free energy

density

may be written in terms of the

layer displacement

u

and the deviation c. from the mean mesogen concentration as

f

=

B(J,u)~

+

K(V(

a)~ + x ' c~ +

C,

c d-u

(3)

2 2 ?

The smectic

compressional

modulus at constant concentration is denoted

by

B, and the

bending elasticity by

K. The

coupling

term

C,

c d-ii expresses the fact that the

layer spacing

(11)

depends

on

composition.

If pure

phases

have a relative difference

(~

in

layer spacing,

we

~

Sh°U'd ~~P~~t

C<

~ B

(~

0

It is useful to define a new concentration variable fi

= c +

XC,

c

d=u,

and to include a source

term hc. In terms of F

land

upon Fourier

transforming)

we have

f(q)=)(hq)+Kq[)ju~j~+)x-'jBjq)j~+xc,q=hj-q)ujq)-h(-q)Bjq), j4)

where B

=

B

XC ).

The fluctuations of

u(q)

and

F(q)

are

independent.

We see that as x becomes

large,

B is driven to zero, for a finite value of x. When

B

vanishes,

the fluctuations in

u(q)

with

q~10

become

large. Moreover,

fluctuations in

c(q)

become

large

we have

in iq) Hi-

q

)i

=

ihq]

+

Kq[ )-

'

(F(q) Ii- q))

= x

(5)

(c (q

c (- q

))

= x

(Bq)

+

Kq[ )(Bq)

+

Kq[ )-

' We say that

u(q=) [and c(q=)] undergo

critical fluctuations as B

- 0, but B is non-critical.

Reference

[9]

describes the

hydrodynamics

of two-component smectics in a

simplified

and useful

form,

under the

assumptions

of

I) incompressibility

;

2)

constant temperature ;

3)

no

«flexodiffusion»,

I-e-, no

off-diagonal Onsager couplings

between c and u

4) highly anisotropic

diffusion of the

concentration,

so that diffusion is confined to the directions

along

the smectic

layers;

and

5) isotropic viscosity.

With these

assumptions,

the linearized

hydrodynamic equations

are

d~u =

~~

g~

q

~

~tgt

~

~)~

gi +

~j $ (6)

"q~

dF

~tC " fi

p

P ~

(Here

F

=

f

dV is the free energy. )

These three

equations

have three

eigenmodes

one

pair

or

propagating

second-sound

modes, with

frequency

w

=

~ ~ ~°~~

,

and one

overdamped

« baroclinic » mode. The

P q

baroclinic mode has a relaxation

proportional

to B as the

spinodal

is

approached

and

B

vanishes,

the baroclinic mode is

critically

slowed. Because B

land

g~) do not have a

diverging susceptibility,

we expect an adiabatic

approximation,

d,g~

= d~B = 0, to be

appropriate.

In this

approximation

we have a

single equation

of motion

0

=

Ii

+

~~~' ~~~

~~

d~u +

~~

(7)

qj «q au r

(12)

[hql

+

Kq~ f(4)1 ql

W

lq

=

~ ~ ~

'~~~ ~~~~~~

(8) Kq~ f (4

m

Kq[

+ y

q]

+ Y2

ql ql

where we have defined

q(w ~~

'~ ~' In

equation (8)

we have included additional terms

a

~

(yj qi

+ y~

qi q(

)

u

(q)

~ in the free energy

given by equation (4),

since we are interested in

cases where B is small or

negative.

We expect from

scaling

considerations that these

higher-

order elastic coefficients y and y~ will be of the order

Bf~,

where

f

is the mean

layer spacing.

We note that in

typical thermotropic

smectics, the

penetration length

A defined

by

~

WA ~ is close to the

layer spacing f [14]

; hence the function

f(()

may be

only weakly

B

dependent

on the direction of cl.

We expect the wavenumber qo to

correspond

to a

microscopic length

as well ; note that

qo satisfies ~

q(

=

'~

q() "~~ q(~,

where the left-hand side is a

typical

second-sound

P P p

frequency squared,

and the

right-hand

side is the

product

of relaxation rates for viscous

diffujion

and concentration diffusion.

Using

a

viscosity

Y~ i

I,

a molecular

diffusivity

"~~

i 10~ ~ smectic modulus B1

10~

and

density

p i I for

typical

smectics (cgs units), P~

[15, 16]

we find ~ ~

i

201.

qo

Now consider the case of a

quench

below the

spinodal, I-e-,

such that B ~ 0.

Thy

relaxation

rate for the baroclinic mode in the limit of small q

(except

for q- -

0)

i~ w

(q )

i

~~j

,

which is

~lqo

negative

in fact, a small baroclinic distortion with such a wavenumber would grow with this

growth

rate. The fastest

growing

modes, which dominate the initial

spinodal

pattern, are those wavevectors that minimize the

decay

rate,

equation (8).

Consider a

relatively

shallow

quench,

such that ~

« IA

qo)2 (the

latter

quantity,

as

argued

B

above,

being

of order of

unity).

Then the denominator of

equation (8)

may be

approximated

as

q( q)

;

minimizing

with respect to q and am tan~ '

~~ leads to

qi

sin2 9)

~ A B

~ 2

f

a

)

~

(9)

~ d sin

(2

9

do

f

9

If

f(

9

)

m

f ((

9 ) is not too

anisotropic,

the

optimum angle

will be near to 9

= ± ~ ; we have

4

then q~

~

(13)

For a

sufficiently deep quench

such that ~

w

(Aqo)~,

the adiabatic

approximation

is B

questionable,

because the

growth

rate of the unstable mode is no

longer

small

compared

to the other characteristic time scales.

Making

the

approximation

anyway, one obtains

~2_

~

-i~ )~) ~

~

~~~

(10) o

= +

~

4

Then the

fastest-growing

wavenumber is of the order of the inverse

layer spacing,

and the

preferred angle

between q and the z-axis is

again

45°.

To summarize our results the

fastest-growing

modes of a two-component smectic

liquid

crystal quenched

below the critical

point

for the

demixing

of the two

species

of mesogens are

growing

baroclinic modes. The

fastest-growing

wavenumber satisfies q~

~~

A ~ which is B

the usual behavior for

spinodal decomposition

of a conserved

density (that is,

q~ is

proportional

to the reduced temperature, since B w B far from the critical

point).

The

preferred angle

between the

fastest-growing

wavevectors and the

layer

normal n should be in

general

different from zero and more

specifically

of the order of 45° for systems with fourth-order elastic

coefficients that are not too

anisotropic.

This

preferred angle

results from the

dispersion

relation for the baroclinic mode, and reflects the fact that II the diffusion of molecules is much faster within the smectic

layers

than across

the

layers,

so that modes with q

parallel

to n are very slow, and

2)

the

driving

force for the

growing

baroclinic mode is the

negative layer compressibility fi

which acts

along

the z-

direction,

so that the wavevector must have some

projection along

n to be unstable.

Interesting

theoretical

que~tions

still to be addressed include the nature of the

coarsening

process

beyond

the

early-time regime

of the

exponential growth

of the unstable mode. The two-component smectic with

demixing

nematogens bears some resemblance to the

problem

of

phase separation

in

gels,

where the elastic

degrees

of freedom of the

gel

are

coupled

to the

concentration variable in a manner similar to

equation

(3)

[17].

There, the

long-range

elastically

mediated forces between

separated

domains affects the domain

morphology

these effects have been the

subject

of a recent

study [18].

4. Conclusion.

Light scattering

as well as

microscopic

observations have revealed the

anisotropic

nature of

spinodal decomposition

in two-component smectics. This behavior is

theoretically interpreted

as

being

the result of a destabilization of the baroclinic mode in two-component smectics

where the

layer spacing

is different in the two pure

compounds

thus

depending

on

concentration in the mixtures. This

coupling

is crucial to

S~-S~ phase separation

as

experimentally

evidenced

by miscibility

studies conducted on numerous

binary

systems in which the

layer

thickness of one component is modified with

regard

to the other

[19, 20].

The kinetics of a

spinodal decomposition

in a smectic A solution presents a classical

behavior. The decrease of the characteristic wavevector with time is in agreement with the usual behavior observed in

liquids

or other

liquid crystal

systems. More

specifically

it is observed that the

angle

between the direction of

scattering

and the director decreases

regularly

as

decomposition proceeds.

(14)

viscosity

of the

mesophase

and the

experiments require

a less

sophisticated

temperature control. From this

point

of view it seems worth

extending

the

study

of

spinodal decomposition

to smectic A solutions of

liquid crystalline polymers

in which

phase separation

have also been observed

[20].

References

[ii Chou Y. C.,

Goldburg

W. I., Phys. Rev. A 20 (1979) 2105.

[2] Snyder H. L., Meakin P., J. Chem. Phys. 79 (1983) 5588.

[3]

Krishnamurthy

S., Bansil R.,

Phys.

Ret>. Lent. 50 (1983) 2010.

[4] Roux D., J. Phys. Fiance 47 (1986) 733.

[5] Casagrande C., Veys~ie M., Knobler C. M., Phy.I. Ret>. Lent. 58 (1987) 2079.

[6] Roux D., Knobler C. M., Pfiy.I. Rev. Lent. 60 (1988) 373.

[7]

Sigaud

G., Nguyen H. T., Achard M. F.,

Twieg

R. J., Phj,s. Rev. Lent. 65 (1990) 2796.

[8] Park Y., Lubensky T. C., Barois P., Prost J., Phys. Ret> A 37 (1988) 2197.

[9] Nallet F., Roux D., Prost J., J. Phys. Fiance 50

(1989)

3147.

[10] Brochard F., de Gennes P.-G., Pianiana

suppl.

1 (1975) 1.

[I I] A brief argument that the slowest hydrodynamic mode in a system with several modes is made slower by the approach to the critical point is given in MiIner S. T., Martin P. C., Ph»s. Ret,.

A 33 (1986) 1996.

[12] Ma S.-K., Modern Theory of Critical Phenomena, chap. XI (Addison-Wesley, Reading, MA.

1975).

[13] For a review see Gunton J. D., San Miguel M., Sahni P. S., Phase Transitions and Critical Phenomena, vol. 8, C. Domb, J. Liebowitz Eds. (Academic Pres~, New York) p. 319.

j14] de Gennes P.-G., The

Physics

of

Liquid Crystals

(Clarendon Press, Oxford, 1975) p. 291.

[15]

Bhattacharya

S., Sarrna B. K., Ketterson J. B., Pfiys. Ret, B 23 (1981) 2397.

[16] Cheng B. Y., Sarma B. K., Calder J. D., Bhattacharya S., Ketterson J. B., Pfiys. Ret,. Lent. 46 (1981) 878.

[17] Onuki A., J. Ph_vs. Sac. Jpn 58 (1989) 3065.

[18] Onuki A., J. Phys. Sac. Jpn 58 (1989) 3069.

[19] Sigaud G., Nguyen H. T.,

Twieg

R. J., to be

published.

[20] Laffitte J. D., Sigaud G., Nguyen H. T., to be

published.

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