HAL Id: jpa-00232200
https://hal.archives-ouvertes.fr/jpa-00232200
Submitted on 1 Jan 1983
HAL is a multi-disciplinary open access
archive for the deposit and dissemination of
sci-entific research documents, whether they are
pub-lished or not. The documents may come from
teaching and research institutions in France or
abroad, or from public or private research centers.
L’archive ouverte pluridisciplinaire HAL, est
destinée au dépôt et à la diffusion de documents
scientifiques de niveau recherche, publiés ou non,
émanant des établissements d’enseignement et de
recherche français ou étrangers, des laboratoires
publics ou privés.
Macroscopic dynamics in nematics near the
uniaxial-biaxial phase transition
H. Brand, J. Swift
To cite this version:
H. Brand, J. Swift.
Macroscopic dynamics in nematics near the uniaxial-biaxial phase
transition.
Journal
de
Physique
Lettres,
Edp
sciences,
1983,
44
(9),
pp.333-337.
�10.1051/jphyslet:01983004409033300�. �jpa-00232200�
Macroscopic dynamics
in nematics
near
the uniaxial-biaxial
phase
transition
H. BrandBell
Telephone
Laboratories,Murray
Hill, New Jersey 07974, U.S.A. and J. SwiftDept.
Physics, University
of Texas, Austin, Texas 78712, U.S.A.(Recu le 15 decembre 1982, accepte le 17 mars 1983)
Résumé. 2014 Nous
présentons
une discussion desexpériences
possibles
révélant lespropriétés
macro-scopiques
desnématiques
uniaxesprès
de la transition uniaxe-biaxe. Enparticulier,
nous proposons une mesure d’un nouveaucouplage statique
entre lesgradients
des fluctuations du directeur(03B4n)
dela
phase
uniaxe et duparamètre
d’ordre(03BEij)
de laphase
biaxe. Abstract. 2014 Basedon the derivation of the
macroscopic dynamics,
we present a discussion ofpossible
experiments
whichprobe
themacroscopic
behaviour of uniaxial nematics close to the transition tothe biaxial phase. In
particular
we propose anexperiment
to measure the influence of a novel static crosscoupling
betweengradients
of the director fluctuations(03B4n)
of the uniaxialphase
and the order parameter(03BEij)
of the biaxialphase.
Classification
Physics Abstracts 61.30G
Starting
with the identification[1]
oflyotropic
biaxial nematics in 1980 there has been anincreasing
interest in theexperimental [2,
3]
and theoretical[Ref.
4 and references citedtherein]
investigation
of themacroscopic properties
of thesesystems.
Very recently
Jacobsen and one ofthe
present
authors[5] presented
ahydrodynamic description
of the uniaxialphase
close to the transition to the biaxialphase.
In addition to thestrictly hydrodynamic
variables of the uniaxialphase namely density
p, entropydensity
7,density
of linear momentum g and the director fluc-tuations bn(characterizing
thespontaneously
broken rotationalsymmetry)
the authors ofreference
[5]
introduced the orderparameter
which is slowalthough
with along,
but finiterelaxation time t. The
assumption
which enters thisdescription
is,
of course, that no additional« slow »
quantities
exist.In the present note we
generalize
the staticsgiven
in[5] by
including
the effects of externalmagnetic
fields. We alsogive
a novel crosscoupling
term between thegradients
of the directorfluctuations and
gradients
of thequantity
(a
symmetric,
traceless tensor; cf[5]
fordetails).
It seemsimportant
to notice that this crosscoupling,
unlike many of the other features discussedbelow,
has noanalogue
near theuniaxial-isotropic
phase
transition. The latter has been studied in a series of papersby
de Gennes[6].
To
probe
the new crosscoupling
experimentally
we propose a staticconfiguration
in anL-334 JOURNAL DE PHYSIQUE - LETTRES
inhomogeneous magnetic
field. In addition we discuss whichexperiments
can be done tostudy
the static anddynamic
behaviour in somedetail;
as it turns out there are strong similaritieswith the
corresponding
situations near theuniaxial-isotropic phase
transition. It isimportant
to note,
however,
oneimportant
difference between the two transitions. Theisotropic-uniaxial
transition isweakly
first order(and
associated with a latentheat)
thusgiving
rise to finite fluctua-tions of considerablemagnitude.
The situation near the uniaxial-biaxial transitionis,
from anexperimental point
ofview,
even more favourable because this transitionis,
at least in meanfield
approximation [7]
of secondorder,
and theexperimental
results available so far seem to confirm thesepredictions.
Thus,
we canexpect
diverging
fluctuations of variousquantities
whenapproaching
the uniaxial-biaxialphase
transition from above. For thegeneralized Ginzburg
Landau free energy we havewhere
6!!
=ð¡j
-ni
nj
and where the first two lines have beenpresented
in reference[5]. Fo
contains the
purely
hydrodynamic
contributions which can be found e.g., in reference[8].
The new crosscoupling
term has the detailed formThe effects of an external
magnetic
field can beeasily
included intoequation (1) giving
rise to the additional terms(FH)
where
and
where x
contains twoindependent
nontrivial termsgiving
rise to the contributionswhere
H 1. symbolizes
themagnetic
fieldperpendicular
to n. It should bekept
inmind, however,
that x
contains an additional factorç¡j
compared
toX
and is thereforepresumably
of minorimportance.
Thedynamics
remainsunchanged,
i.e.,
the reversible and the irreversible currentsare a mere
superposition
of the termsgiven
in[5]
and[8].
No additional crosscouplings
appear.A first
simple application
of the basicequation
ismagnetic
birefringence
in theplane
perpen-dicular to the uniaxial director. If we assume a
homeotropic sample
with n% ~(enforced e.g.,
by
a staticmagnetic
field inz-direction)
we consider the effects of a static field in thexy-plane,
say in the x-direction. We then find from
equations (1)
and(3)
for thexy-plane
Proceeding
in the same way as in[6]
we find for theanisotropy
of the refractive indices in theplane
where // and -L refer to the directions
parallel
andperpendicular
to themagnetic
field in theplane.
Since (X ’"l/a
the effectspredicted by equation (7)
will become verylarge
near thephase
transition(cf.
also Ref.[2]
for a discussion of thispoint).
Of course, ananalogous
argument goesthrough
for electricbirefringence
in thexy-plane.
Next we consider the case of flowbirefringence.
We assume as above that the uniaxial director is oriented in the
z-direction,
furthermore weconsider a flow
velocity along
x with thevelocity
gradient Dvxl0y.
We then
get
from the basicequations
(Eq.
(1)
andEqs. (6~ (9), (12), (16)-(24)
of ref.[5])
where we use the notation of reference
[5]
wherepossible
(e.g., Aij
=2 L(vi V
i +v
V;)).
For the
configuration
we havechosen,
we assume a timedependence
of the formeiwt
and obtainIn
deriving (9)
we havekept
the viscousterm’
and thebending
energy of the~-field.
It is wellknown for the
isotropic-uniaxial
nematic transition(9)
that the effects of thebending
energycan be
neglected.
Then we deduce fromequation
(9)
in the lowfrequency
limitProceeding
as in theuniaxial-isotropic
case[6]
fromequation (10)
weget
for the difference in therefractive indices
where the characteristic time f
diverges
at thetransition ;
for the constant S we refer to[6].
From the basicequations
it iseasily
checked that all other variables(e.g.
bni)
do notcouple
in thespecific
configuration
we have chosen. As soon as theequilibrium
value of the uniaxial director no has acomponent in the
plane
of theshear,
however,
the aboveanalysis
has to bechanged completely
and nosimple
resultprobing
themagnitude
of ç¡j
can be obtained.The influence of fluctuations of
~1~
can also beinvestigated by looking
at the shear wave atte-nuation. We assume, asabove,
no jz
and thevelocity
in x-direction with variations in they-direc-tion. Then from
equations (12),..., (26)
of[5]
we can extract for the stress tensorL-336 JOURNAL DE PHYSIQUE - LETTRES
Combining
equations
(12)
and(13)
weget,
after a Fouriertransform,
the effectiveviscosity
fleffThus we
get
a fnite correction forflerr(0153
=0)
of the order7;2/,
whichgives
apossibility
to mea-sure thisquantity
because athigher frequencies
(ro2 ~ (~xo ~ )~ )
there is no correction. We mentionin
passing
that ourexpression
for the shearviscosity
differssignificantly
from the result derivedby
de Gennes for theuniaxial-isotropic phase
transition. De Gennesfinds,
forexample,
no staticcorrection.
Furthermore,
there is ahigh frequency
correction in the latterphase
transition[6].
Finally,
we discuss thepossibilities
ofmeasuring
the static crosscoupling presented
here for the first time.Light
scattering
insimple
geometries
has been discussed in reference[5].
As iseasily
checked,
thecoel~icient ~
does not enter for thesespecial
cases,. thusleaving
thepresentation
of [5] unchanged.
It isstraightforward
to convinceoneself however,
by
looking
into morecompli-cated
configurations,
that ~
enters ingeneral
situations,
although
thedependence
on 0
becomes rather involved. In thepresent
paper we propose a staticexperiment
togain
somequalitative
insight
into the effects of~.
To achieve this one sees,by
inspection
ofequation
(1),
that one needsinhomogeneous
externalfields,
and amagnetic
fieldmight
be aparticularly
good
candidate.We examine the situation sketched in
figure
1. We assume that onepole
of themagnet
iswedge
shaped
in thexy-plane
and extends to ± oo iny-direction
which renders the situationessentially
two-dimensional. In the uniaxial
phase
the n field is thendistorted,
but in asymmetric
way in z and - z-direction because the twist termK2
does not enter. If the uniaxialphase
is cooled towards the biaxialphase
transition the~-term,
which breaks the z -+ - zsymmetry
in theconfiguration
chosenhere,
becomes more and moreimportant
and thus thepattern
(observed
e.g., in a
microscope) picks
up anasymmetric
distortion(in
z-direction),
which
should bedetec-table
experimentally.
This can be inferred from the variationalequations
obtained from(1), (3)
In conclusion we have discussed
possible experimental
configurations
tostudy
the influence of the orderparameter
near the uniaxial-biaxial nematicphase
transition. Inparticular
we haveproposed
anexperimental
set up tostudy
the novelcoupling
term between the director fieldFig.
1. -Proposed experimental
set up to detect thecross-coupling coe~cient ~ by application
of aninhomogeneous
magnetic
field. Without theinhomogeneous
field one can assume ahomogeneous
texture, if necessary this can be enforcedby
a homogeneous field in z-direction.and the
slowly varying quantity
~;~
which should allow for asimple qualitative
determination ofthe
importance
of this term.Acknowledgments.
It is a
pleasure
to thank PatCladis,
W. D. McCormick and Ron Pindak for useful discussions.The research of one of us
(J.S.)
wassupported
inpart
by
the Robert A. Welch Foundation undergrant
number F-767.References