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Permeation and self-diffusion in smectics A
O. Parodi
To cite this version:
O. Parodi. Permeation and self-diffusion in smectics A. Journal de Physique Lettres, Edp sciences,
1976, 37 (6), pp.143-144. �10.1051/jphyslet:01976003706014300�. �jpa-00231259�
L-143
PERMEATION AND SELF-DIFFUSION IN SMECTICS A
O. PARODI
Groupe
deDynamique
des Phases Condensées(*), U.S.T.L.,
Laboratoire de
Minéralogie, place Eugène-Bataillon,
34060Montpellier Cedex,
France(Re.Vu
le27 fevrier 1976, accepte
le 15 avril1976)
Résumé. 2014 Des expériences récentes de R.M.N. et de diffusion
quasi-élastique
des neutrons dansles smectiques A ont donné des valeurs comparables pour les coefficients de self-diffusion
D~
(dif-fusion normale aux couches) et D~. On montre que la
perméation
n’intervient pas dans une expé-rience de self-diffusion et, par suite, que la relation d’Einstein relie
D~
à une viscosité effective ~~,et non au coefficient de perméation
03BBp,
ce quiexplique
les résultats expérimentaux.Abstract. 2014 Recent R.M.N. and quasi-elastic neutron scattering experiments on smectics A have
given comparable values for the self-diffusion coefficients
D~
(diffusion normal to the layers) and D~,in spite of the
possible
occurence of a permeation process which would lead to much lower values for D ~. It is shown that there is no permeation in a self-diffusionexperiment,
and therefore that theEinstein relation connects
D~
to an effectiveviscosity
~~ but not to thepermeation
coefficient03BBp,
which explains the
experimental
results.LE JOURNAL DE PHYSIQUE - LETTRES TOME 37, JUIN 1976,
Classification
Physics Abstracts
7.130
1. Introduction. - Proton
magnetic
resonanceexperiments [1] parallel
andperpendicular
self-diffu- sion coefficients were measured in smectics A-TBBA and EBBA(D~~
is related to diffusionparallel
to theoptical axis,
i.e. normal to thelayers).
It was foundthat
Djj
andDl
were of the same order ofmagni-
tude. This results are consistent with
high
resolutionneutron
quasi-elastic
data on TBBA obtained both with apowder [2a]
and analigned sample [2b].
Thisresult seemed
surprising, since, taking
into accountthe very small value of the
permeation coefficient,
one could expect a much smaller value for
D)j
~~ than forD..l,
as waspointed
outby
certainparticipants
to the
European
Conference onThermotropic
Smec-tics
(Les Arcs, 1975).
It will be shown herethat,
insmectics, D
II is related not topermeation but,
as innematics and
isotropic fluids,
toviscosity.
2. Theoretical
approach.
- Thestarting point
isclassical
[3].
From Einstein’srelation
where Ill! is a
mobility
definedby
fil
is theparallel component
of the forceacting
on adiffusing
molecule.In
isotropic fluids,
one then considers the moleculeas a
sphere,
andapplies
Stokes’law,
which leads to17 is the
viscosity
and a a molecular radius.(*) Laboratoire associe au C.N.R.S.
~
In
smectics,
theproblem
is a little morecomplex,
since a motion
through
thelayers
can involve per- meation. It is therefore useful to turn back to the definition ofpermeation [4, 5]
as the relative motion of the fluid and of thelayers.
Consider a self-diffusion
experiment performed
on a smectic A in a
planar configuration.
Some of themolecules are marked and the system is
prepared
insuch a way that at time t =
0,
a concentrationgradient along
the Z-direction(normal
to thelayers) aC/aZ
isimposed.
Then the marked molecules diffuseaccording
to
,2-
Their flow is balanced
by
a back-flow of non-marked molecules such that the totalfluid-velocity,
vZ, vanishes.The
equations
of motion for a smectic in aquasi- planar configuration (with only
small distortions of theplanar structures)
are[4]
where :
u is the
layer displacement,
g is the
restoring
forceacting
on thelayers and q
is the viscous tensor : for a pure shear flowArticle published online by EDP Sciences and available at http://dx.doi.org/10.1051/jphyslet:01976003706014300
L-144 JOURNAL DE PHYSIQUE - LETTRES
Look first at eq.
(4). Here vZ
isgiven
as a functionof u and g, which characterize the
layer’s dynamics.
But the concept of
layers
has ameaning only
at amacroscopic scale,
in that sense that their curvature radius must be muchlarger
than a molecularlength.
This means
that,
in eq.(4), u and g
vary veryslowly
at amicroscopic scale,
and hence that we cannot takefor v.
thevelocity
of a marked molecule but anaverage over a volume much
larger
than a molecularvolume. In other
words,
in eq.(4),
vz is the fluidvelocity,
and therefore vanishes. Fromthat,
since attime t =
0, g
=0,
both £and g
remain null and thelayer configuration
is notchanged.
Turn back now to eq.
(5).
In ourexperiment
p isconstant, g vanishes,
and theonly remaining
force isthe viscous one, which characterizes the
dissipation
due to molecular collision. Thus eq.
(5) keeps
ameaning
at a molecular scale :pvZ
is the force per unit volume.Applying
eq.(5)
to markedmolecules,
onefinds
where 0 is a molecular volume
and 1111
an effectiveviscosity
A
crude calculation,
for rods oflength a
and diame-ter b, gives
-1
and
finally
where v is a numerical coefficient of order one.
Using
now eqs.(1)
and(2)
one finds3. Discussion. - In this
calculation
the energy barrier forpermeating
molecules betweenadjacent
smectic
layers (as
far as one canspeak
ofpermeation
for an individual
molecule)
has not been taken intoaccount. It will now be shown that the presence of this energy barrier does not
modify
theprevious
results.It is well known that the
validity
of Einstein’s relation(1),
which is deduced fromequilibrium conditions,
does notdepend
on the presence or absence of an energy barrier. As anexample,
Einsteinrelation is valid for electrical conduction in semi-
conductors,
where an activation energy is needed forexciting
an electron from a bound donorimpurity
level to the conduction band. On the other
hand,
thepresence of this energy barrier does not result in any
new
force,
since the totalfree-energy
is notchanged
inthe
self-diffusion
process(the depths
of the energy wells are the same for marked and non-markedmolecules).
In fact theonly
effect of this energy barrier is to introduce an activation energy term in the tem-perature
dependence
of pl, jj(and consequently DII)
inthe smectic A
phase.
The fact that the
permeation
constantÅp
is notdirectly
related toDII explains
the results obtainedby
neutron
quasi-elastic scattering experiments [1, 2].
A similar calculation would
give
with
The fact that a4 and a56 do have not the same
temperature
dependence explains
the differentslopes
found for the
plots of D_L
andDj)
versus temperature.The numerical coefficients v and v’ are of the same
order,
butprobably slightly different,
and theexperi-
ments
performed
onTBBA suggest
that vY/11 ~~and ~ ~
are of the same order of
magnitude
in the smectic A temperature range.A
previous
evaluation ofDj)
had been madeby
de Gennes
[6]
whoexpected
it to becomparable
to~Ap,
where B is therigidity
coefficient of thelayers.
Keeping
in mind that B NkT/a3
and~,p ~ a2/r~,
onefinds
which is in
good
agreement with our results.Acknowledgments.
- It is apleasure
to thank hereDrs F.
Brochard,
A. J.Dianoux,
E.Dubois-Violette,
G. Durand and F. Volino for fruitful discussions.
References
[1] KRÜGER, G. J., SPIESECKE, H. and VAN STEENWINKEL, R., Communication à la Conférence Européenne sur les Smectiques thermotropes et leurs applications. Les Arcs,
décembre 1975, to be published in J. Physique Colloq.
37 (1976) C 3.
[2] DIANOUX, A. J., VOLINO, F., HEIDEMANN, A. and HERVET, H., a) J. Physique Lett. 36 (1975) L-275, b) to be published.
[3] See for example : LANDAU, L. and LIFCHITS, E., Mécanique des Fluides (Editions MIR, Moscou) 1971, p. 285.
[4] HELFRICH, W., Phys. Rev. Lett. 23 (1969) 372.
[5] MARTIN, P. C., PARODI, O. and PERSHAN, P. S., Phys. Rev. A 6 (1972) 2401.
[6] DE GENNES, P. G., The Physics of Liquid Crystals (Clarendon Press, Oxford) 1974. De Gennes notations for viscous coefficient will be used in this letter.