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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�
Classification
Physics
Ab.itia<.ts05.70J 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 decompositions
diffdrentes sontanalysds
par diffusion de la lumibre etmicroscopie
optique. Nousmontrons 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 bylight
~cattering andoptical
microscopy. We show that this~pinodal,
characterized by aprescribed
angle between the mo~t intense wavevectors and the layer normal, is the result of the instability of the baroclinic mode oftwo-cojnponent
smectic hydrodynamics.1. Introduction.
When an
initially homogeneous
system is driven to an unstable state in such a way thatnucleation is avoided,
phase separation
processesthrough
thegrowth
of fluctuations incomposition
at wavevectors q i q~. this defines aspinodal decomposition
and results in a concentrationprofile throughout
the medium.Scattering techniques
are most suitable togive
evidence of this
phenomenon
in thereciprocal
space : the characteristic pattem is aring
or haloin which the maximum
intensity corresponds
to the wavevector of the fastestgrowing
fluctuations
(q~), Experimentally
thesimplest
way to achievespinodal decomposition
is a« critical
quench
» in which the temperature of ahomogeneous sample
of criticalcomposition
is varied as
rapidly
aspossible through
the criticalpoint.
Thephenomenon
can also be viewed in the direct space with anoptical microscope provided
that there exists asufficiently large
difference in the refractive indices of the two
separating phases.
(*) Present address :
Department
ofChemistry,
Massachusetts Institute ofTechnology, Cambridge,
MA 02139. U-S-A-
A second
important
feature ofspinodal decomposition
is its timescaling.
At very short times afterquenching
theintensity,
of thescattering
isexpected
to growexponentially
with itsposition
unaffected(q~
=
Const.,
Cahn'sregime).
Atlonger
times the fluctuations atlonger wavelengths
arefavored,
which results in thecollapse
of thering.
Forisotropic
systems theradius then decreases with a power law q~ oz
t~
with=
for the
early
stage and 3= -1 later
[I].
The rate of the evolutiondepends
on the time for diffusionthrough
acorrelation
length,
t~=
D~ '
f~,
which can beexpressed
in terms of thedepth
of thequench (AT), viscosity
(Y~),
and characteristic bare correlationlength (fo)
D
=
Do
~~ ~ '=
~ ~~ ~ ~
and f
=
to
~~ ~ A ~~ ~~ (l )Tc ~1
Tc
Tcto
Thus,
i~ =
) ) 11 )
=
~
°) (2)
c~'~ ~~
~"~~ c~
~~~~~y and v are the critical exponents that characterize the
susceptibility
and correlationlength, respectively.
Alarge
t~corresponds
to a slowdecay
in the diameter. Forexample,
thestudy
of thedynamic~
ofphase separation
over reasonable time scalesIi-e-,
100s)
insimple liquid
mixtures
requires
very shallowquenches
(~ 5 mK ), which meansequipments
withextremely good
thermal stabilization(10~~
K[I ]. Experiments
on systems in which t~ islarge
are thushighly
attractive. Some suchexperiments
have been conducted in viscous media such aspolymer
solutions or blends[2, 3]
or in systems withlarge
correlationlengths
such asmicroemulsions
[4].
Alsoinvestigated
morerecently
have been the characteristics ofphase separation involving mesophases
in a nematic solution of aliquid crystalline polymer [5]
and between alyotropic
lamellarmesophase
and anisotropic
spongephase [6].
The exponent of the power law which fits the decrease of the wavevector as a function of time looksquite
similar to the classical value obtained in
simple
fluid systemsalthough
unusualanisotropic
features could be noticed in the domain
growth.
Recently
a critical consolutepoint
has been observed in a two-component smectic Aphase [7].
We present astudy
of thespinodal decomposition
in this system. In theexperimental
section of this paper,
light scattering
andoptical microscopy pictures
recordedduring phase separation
are described andanalyzed.
Theseexperimental
observations are consistent with thetheory
forspinodal decomposition
in such ordered fluids which ispresented
in the theoretical section.2.
Experimental
section.2, SAMPLE PREPARATION. The system in which a
phase separation
between two smectic Aphases
is obtained is abinary
mixtureinvolving
the6-cyanonaphtyl-2 4-decyloxybenzoate (compound A)
and the4-hexyloxyphenyl 4-perfluoroheptylbenzoate (compound
B).CioH2i°-)O_ O ~
(A)
~
C7Fiifi-~°2-filC6H13
(B) Thephase diagram
has beenpublished previously [7]
and is shown infigure1.
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 theliquid crystalline
binary ~ystem 6-cyanonaphtyl-2
4-decyloxybenzoate 5 (left) +4-hexyloxyphenyl 4-perfluoroheptylbenzoate
(right) (from Ref. [7]). N denotes a nematicregion.
The
experiments
have beenperformed
on a mixture with acomposition
as close aspossible
to the critical
composition (volume
fraction of B ~~~ =
0.44
corresponding
to mole fraction~i~
~ =
0,40 and
weight
fractionw>~ ~ =
0.51).
The basic set-up forlight scattering experiments
is described in
figure
2. Atypical quench
was a few tenths ofdegrees deep starting
from about? °C above the critical temperature
(final
temperatures were 0.2 °C and 0.4 °C below thecritical temperature in the two
experiments
for whichquantitative
data aregiven 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 heatexchanger
of the oil bathregulating
the temperature of thesample just
the time necessary to reach the final temperature of thequench.
It took
typically
one minute tobring
the cell at the set temperature. Foroptical
observations thethermostated cell was
simply
moved on to amicroscope
stage. The samesample
andsample
holder have been used for both
light scattering
andmicroscope
observations. Thesample
semi transparent
screen cold bath
z
video recorder
He-Ne )aser
Fig.
2.Light
scattering set-up.holder was a 100 ~m thick
glass
cell. Suitablecoatings
weredeposited
to obtain two different orientations of the smecticplanes
eitherhomeotropic (planes perpendicular
to thelight
beam,Fig. 3a)
orhomogeneous planar (planes parallel
to thelight
beam,Fig. 3b).
The orientation of thesample
withregard
to thepolarization
oflight
isspecified
infigure
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 planarconfiguration.
2.2 RESULTS.
Light scattering
patterns recorded in the course ofspinodal decomposition
from
planar
orientedsamples
areanisotropic they
consist of four blobssymmetrically
located, as shown infigure
5 in which the orientation of both the director and thepolarization
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 lamellarphase.
Moreover the sequence ofpictures
infigure
5gives
evidence for thecollapse
of thescattering
pattern. Two series ofimages corresponding
to two differentquenches
have beenanalyzed
in order tostudy
the time evolution of the
position
of the maximum scatteredintensity.
Thequench depth
AT
= T~ T was 0.2 K for
quench
and 0.4 K forquench
2.Figure
6 shows alogjo-logjo
plot
of the modulus of the wavevector in(angstr0ms)~'
as a function of time in seconds for bothquenches.
These results can becompared
to the classical power law(represented by
the dashed linecorresponding
to a 0.33slope)
over some time range. One can note the saturation of q at the veryearly
stage of thedecomposition
for the shallowerquench although
theFig.
5.Sequence
oflight scattering
patterns selected from the video-recording onquench
I for a planar homogeneou~ sample. Time interval between two pictures i~ 5 s. axis (orientation of both thedirector 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
tFig. 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
faintness of the
scattering
at theseearly
times does not allow ahighly
reliable observation.Also noticeable from these curves is the trend toward
larger slopes
atlonger
times in bothcases, which suggests a cross-over as observed with other systems
[1,
4,6].
In addition,image
analysis
indicates that theangle
between the direction of maximumscattering
and the director of the smectic Aphase
decreasesregularly
with time from a finite valueranging
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 twoexperiments.
Asexpected,
the fastercollapse
occurs for thedeeper quench. Comparatively
thedecomposition proceeds
at a slower rate in our system than insimple liquids owing
to thehigher viscosity.
Thusspinodal decomposition
can be observed over a reasonable interval of time forfairly deep quenches.
Indeed the kinematic
viscosity
of a smectic Aliquid crystal
isroughly
two hundred timeslarger
than theviscosity
of the usualisotropic liquid
(Y~s~w 200 cP and the time scale is
expanded by
the same factor. Then,provided
that the bare correlationlengths
arecomparable
in bothcases, 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 mKquench
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 sizeincreasing
with time ; seefigure
8 (the orientation of the director isapproximately
S-W--N-E- in both
Figs.
8 and9).
These observationscorre~pond
to a late stage of thedecomposition compared
to thelight-scattering experiments
sincedeeper quenches (AT
=
0.9-1 K
typically)
areperformed
in transmittedlight microscopy
toproduce enough
contrast.The ?D-Fourier transforms of these
pictures nicely
confirm the geometry of thelight scattering
patterns(Figs. 9a-d).
Thecorresponding
wavevectors have been estimated fromfigure
9.Fig. 8.
Sequence
ofmicroscopic
textures observedduring
the course ofdecomposition
(quench is different from quenches and 2). Time interval between two pictures is 5 s, with Abeing
the earliest picture. The orientation of the director isapproximately
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 thelight-scattering experiments
toproduce
thescaling plot
shown infigure
10. Thisscaling plot
has been made for mean-field values for the exponents. It confirms an increase in theslope
~fi atlonger
times. In the case of smectic A-smectic A transitions dominatedby
difference inlayer
thickness(where coexisting phases
do not differappreciably
incomposition),
aspecial non-Ising
criticalpoint
ispredicted [8],
but the exponent values for these systems are not yet well established and suchnon-Ising scaling
cannot be tested.Finally
thequenches performed
on ahomeotropically aligned sample provided
no noticeablescattering.
One canexplain
this behavior if the difference in the refractive indices of the components isquite
small in this orientation. One does not expect ananisotropic
pattern in thiscase and the
scattering
oflight
over aring
instead ofbeing
focused within four spots would result in an insufficientintensity.
A veryfuzzy picture
is observed with theoptical microscope
and no useful data could then be obtained from thisconfiguration.
3. Theoretical section.
We may summarize our
description
of this novelspinodal
as follows. Thespinodal
patternresults from the
growth
of the most unstable modes of the two-component smectichydrodynamics
below the criticalpoint.
Asimple description
of two-component smecticFig. 9. 2D-Fourier transforms of the
pictures
infigure
8.'
"
+ +
~ 'x+
*+~
*
$
-2o
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 anoptical
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
Fig,
il. Sketch of thelayer displacement
in the baroclinic mode. Note theoblique
wavevector.hydrodynamics [9, 10]
above T~ containscoupled equations
for the smecticlayer displacement
u, the concentration c, and the transverse momentum g~. The
layer displacement
andconcentration variables are
coupled
in the free energy because thelayer spacing
is different forthe two mesogens
[7]
and thus a function of concentration. The three first-order time-dependent hydrodynamic equations give
rise to threehydrodynamic
modes : apair
ofpropagating
second-sound modes, and anoverdamped
«baroclinic» mode, in which the
eigenvector
is a mixture oflayer displacement
and concentration variation (seeFig.
II ).Near the critical
point
of such a system, the slowest[I II hydrodynamic
mode is made slowerby
thevanishing susceptibility
(« criticalslowing
down») [12]
in the present case this is theoverdamped
baroclinic mode.Upon
a criticalquench,
thiscritically
slowed mode becomes unstable and grows[13].
Near thespinodal,
where thegrowth
ordecay
rate of the baroclinic mode is smallcompared
to thefrequencies
or relaxation rates of all other modes, thedynamics
is well described
by
an adiabaticapproximation,
in which the time derivatives of all non-critical variables have
ordinary
relaxation rates, and so relax to values such that thehydrodynamic
« forces » on these variablesvanish,
and we obtain asingle
first-order time-dependent equation
for thegrowth
of the baroclinic mode.The
fastest-growing
wavevectorpoints
in anoblique
direction for two basic reasons. First, thediffusivity
of the mesogen concentration isstrongly anisotropic,
with moleculesdiffusing mostly along
thelayers
; this suppresses thegrowth
of fluctuations with wavevectorsparallel
ton
(z-axis).
Second, thespinodal corresponds
to thevanishing
of B, the smecticlayer compressibility
at constant chemicalpotential,
so that thegrowth
of the unstable baroclinic mode is drivenby
a «negative layer compressibility
». Thisrequires
the wave,,ector to havesome
projection along
n. Our detailed calculations below show that theangle
between the most unstable wavevector and the =-axis is related to the fourth-order elastic coefficients.Our
description
of the free energydensity
andhydrodynamic equations
for a two-component smectic is taken from Nallet et al.[9]
this system wasoriginally
describedby
Brochard and de Gennes[10].
The free energydensity
may be written in terms of thelayer displacement
uand 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 denotedby
B, and thebending elasticity by
K. Thecoupling
termC,
c d-ii expresses the fact that thelayer spacing
depends
oncomposition.
If purephases
have a relative difference(~
inlayer spacing,
we~
Sh°U'd ~~P~~t
C<
~ B(~
0
It is useful to define a new concentration variable fi
= c +
XC,
cd=u,
and to include a sourceterm hc. In terms of F
land
upon Fouriertransforming)
we havef(q)=)(hq)+Kq[)ju~j~+)x-'jBjq)j~+xc,q=hj-q)ujq)-h(-q)Bjq), j4)
where B
=
B
XC ).
The fluctuations ofu(q)
andF(q)
areindependent.
We see that as x becomes
large,
B is driven to zero, for a finite value of x. WhenB
vanishes,
the fluctuations inu(q)
withq~10
becomelarge. Moreover,
fluctuations inc(q)
becomelarge
we havein iq) Hi-
q)i
=
ihq]
+Kq[ )-
'(F(q) Ii- q))
= x
(5)
(c (q
c (- q))
= x
(Bq)
+Kq[ )(Bq)
+Kq[ )-
' We say thatu(q=) [and c(q=)] undergo
critical fluctuations as B- 0, but B is non-critical.
Reference
[9]
describes thehydrodynamics
of two-component smectics in asimplified
and usefulform,
under theassumptions
ofI) incompressibility
;2)
constant temperature ;3)
no«flexodiffusion»,
I-e-, nooff-diagonal Onsager couplings
between c and u4) highly anisotropic
diffusion of theconcentration,
so that diffusion is confined to the directionsalong
the smectic
layers;
and5) isotropic viscosity.
With theseassumptions,
the linearizedhydrodynamic equations
ared~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 threeeigenmodes
onepair
orpropagating
second-soundmodes, with
frequency
w=
~ ~ ~°~~
,
and one
overdamped
« baroclinic » mode. TheP q
baroclinic mode has a relaxation
proportional
to B as thespinodal
isapproached
andB
vanishes,
the baroclinic mode iscritically
slowed. Because Bland
g~) do not have adiverging susceptibility,
we expect an adiabaticapproximation,
d,g~= d~B = 0, to be
appropriate.
In thisapproximation
we have asingle equation
of motion0
=
Ii
+
~~~' ~~~
~~d~u +
~~
(7)
qj «q au r
[hql
+Kq~ f(4)1 ql
W
lq
=~ ~ ~
'~~~ ~~~~~~
(8) Kq~ f (4
m
Kq[
+ yq]
+ Y2ql ql
where we have defined
q(w ~~
'~ ~' Inequation (8)
we have included additional termsa
~
(yj qi
+ y~qi q(
)u
(q)
~ in the free energygiven by equation (4),
since we are interested incases where B is small or
negative.
We expect fromscaling
considerations that thesehigher-
order elastic coefficients y and y~ will be of the order
Bf~,
wheref
is the meanlayer spacing.
We note that in
typical thermotropic
smectics, thepenetration length
A definedby
~
WA ~ is close to the
layer spacing f [14]
; hence the functionf(()
may beonly weakly
B
dependent
on the direction of cl.We expect the wavenumber qo to
correspond
to amicroscopic length
as well ; note thatqo satisfies ~
q(
=
'~
q() "~~ q(~,
where the left-hand side is atypical
second-soundP P p
frequency squared,
and theright-hand
side is theproduct
of relaxation rates for viscousdiffujion
and concentration diffusion.Using
aviscosity
Y~ i
I,
a moleculardiffusivity
"~~
i 10~ ~ smectic modulus B1
10~
anddensity
p i I fortypical
smectics (cgs units), P~[15, 16]
we find ~ ~i
201.
qo
Now consider the case of a
quench
below thespinodal, I-e-,
such that B ~ 0.Thy
relaxationrate 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 thisgrowth
rate. The fastestgrowing
modes, which dominate the initialspinodal
pattern, are those wavevectors that minimize thedecay
rate,equation (8).
Consider a
relatively
shallowquench,
such that ~« IA
qo)2 (the
latterquantity,
asargued
B
above,
being
of order ofunity).
Then the denominator ofequation (8)
may beapproximated
asq( q)
;minimizing
with respect to q and am tan~ '~~ leads to
qi
sin2 9)
~ A B
~ 2
f
a)
~
(9)
~ d sin
(2
9do
f
9If
f(
9)
m
f ((
9 ) is not tooanisotropic,
theoptimum angle
will be near to 9= ± ~ ; we have
4
then q~
~
For a
sufficiently deep quench
such that ~w
(Aqo)~,
the adiabaticapproximation
is Bquestionable,
because thegrowth
rate of the unstable mode is nolonger
smallcompared
to the other characteristic time scales.Making
theapproximation
anyway, one obtains~2_
~-i~ )~) ~
~
~~~
(10) o
= +
~
4
Then the
fastest-growing
wavenumber is of the order of the inverselayer spacing,
and thepreferred angle
between q and the z-axis isagain
45°.To summarize our results the
fastest-growing
modes of a two-component smecticliquid
crystal quenched
below the criticalpoint
for thedemixing
of the twospecies
of mesogens aregrowing
baroclinic modes. Thefastest-growing
wavenumber satisfies q~~~
A ~ which is B
the usual behavior for
spinodal decomposition
of a conserveddensity (that is,
q~ isproportional
to the reduced temperature, since B w B far from the critical
point).
Thepreferred angle
between thefastest-growing
wavevectors and thelayer
normal n should be ingeneral
different from zero and morespecifically
of the order of 45° for systems with fourth-order elasticcoefficients that are not too
anisotropic.
This
preferred angle
results from thedispersion
relation for the baroclinic mode, and reflects the fact that II the diffusion of molecules is much faster within the smecticlayers
than acrossthe
layers,
so that modes with qparallel
to n are very slow, and2)
thedriving
force for thegrowing
baroclinic mode is thenegative layer compressibility fi
which actsalong
the z-direction,
so that the wavevector must have someprojection along
n to be unstable.Interesting
theoreticalque~tions
still to be addressed include the nature of thecoarsening
process
beyond
theearly-time regime
of theexponential growth
of the unstable mode. The two-component smectic withdemixing
nematogens bears some resemblance to theproblem
ofphase separation
ingels,
where the elasticdegrees
of freedom of thegel
arecoupled
to theconcentration variable in a manner similar to
equation
(3)[17].
There, thelong-range
elastically
mediated forces betweenseparated
domains affects the domainmorphology
these effects have been thesubject
of a recentstudy [18].
4. Conclusion.
Light scattering
as well asmicroscopic
observations have revealed theanisotropic
nature ofspinodal decomposition
in two-component smectics. This behavior istheoretically interpreted
as
being
the result of a destabilization of the baroclinic mode in two-component smecticswhere the
layer spacing
is different in the two purecompounds
thusdepending
onconcentration in the mixtures. This
coupling
is crucial toS~-S~ phase separation
asexperimentally
evidencedby miscibility
studies conducted on numerousbinary
systems in which thelayer
thickness of one component is modified withregard
to the other[19, 20].
The kinetics of a
spinodal decomposition
in a smectic A solution presents a classicalbehavior. The decrease of the characteristic wavevector with time is in agreement with the usual behavior observed in
liquids
or otherliquid crystal
systems. Morespecifically
it is observed that theangle
between the direction ofscattering
and the director decreasesregularly
as
decomposition proceeds.
viscosity
of themesophase
and theexperiments require
a lesssophisticated
temperature control. From thispoint
of view it seems worthextending
thestudy
ofspinodal decomposition
to smectic A solutions of
liquid crystalline polymers
in whichphase separation
have also been observed[20].
References
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Physics
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Twieg
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