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Critical behaviour of the elastic constant and the friction coefficient in the gel phase of gelatin
J.-C. Bacri, D. Gorse
To cite this version:
J.-C. Bacri, D. Gorse. Critical behaviour of the elastic constant and the friction coefficient in the gel phase of gelatin. Journal de Physique, 1983, 44 (8), pp.985-991. �10.1051/jphys:01983004408098500�.
�jpa-00209682�
Critical behaviour of the elastic constant and the friction coefficient in the gel phase of gelatin
J.-C. Bacri and D. Gorse
(*)
Laboratoire d’Ultrasons (**), Université Pierre et Marie Curie, Tour 13, 4 place Jussieu, 75230 Paris Cedex 05, France (Rep le 23 février 1983, révisé le 24 mars, accepté le 28 avril 1983)
Résumé. 2014 Nous avons étudié le comportement critique de la constante élastique et du coefficient de friction dans la phase gel de la gélatine. Les exposants critiques trouvés, 1,8 pour la constante élastique et 1 pour le coef- ficient de friction, sont en bon accord avec une théorie de 3d-percolation.
Abstract. 2014 The critical behaviour of the elastic constant and the friction coefficient have been measured in the
gel phase of gelatin. The critical exponents, 1.8 for the elastic constant, and 1 for the friction coefficient are in
good agreement with 3d-percolation theory.
Classification
Physics Abstracts
46.30J - 64.70M - 64.80
1. Introduction
The aim of this paper is to describe the critical beha- viour of a
typical physical gel, gelatin,
near thesol-gel
phase transition. Athigh
temperatures, in the sol phase,gelatin
appears as a viscouspolymeric
solutionof random coils. As the temperature decreases,
gela-
tion occurs because of two
competing phenomena :
one is an intramolecular
phenomena
where thetriple
helicoidal structure is recovered [1] from the initial random coil, the other is an intermolecular
phenomena
which is a random
bonding
betweenadjacent poly-
meric chains.
It is assumed that
going
from the sol to thegel
phase involves a criticalpoint.
At the critical tempe- rature,bonding
hasspread
from oneedge
to the otherof the sample; the
gelatin
is now considered, in the gelphase,
to be a 3d-elastic medium(collagen
net-work)
immersed in the solvent(water).
Two different theories describe the
sol-gel phase
transition : in the classical
gelation
theory of Flory [2],the
gel
is viewed asgrowing
up like aspanning
tree(Cayley
tree). Then excluded volume effects andcyclic bonds are omitted The classical
expectation
for the exponent t of the network elastic constant is
(*) Present address : C.E.N. Saclay, S.P.A.S., F-91191
Gif sur Yvette Cedex.
(**) Associated with the Centre National de la Recherche
Scientifique.
t = 3. The deviations from this idealistic tree model
stipulated
’above are taken into account in the perco- lation model[3].
Theprediction
is 1.7 t 1.8 in3d-percolation theory.
The
gel phase
isinvestigated
hereby
the methodof
magnetic probes (ferrofluids [14])
immersed in thepolymeric
solution. Under a staticmagnetic
field(H
100 G) the ferrofluidparticles
rotate and inducea shear deformation in the network
(the
solventremaining
motionless). The motion equation of the gel network isgiven by
u is the transverse
displacement
vector of the elastic medium from itsequilibrium
position, p thedensity
of the network, G the shear elastic constant ot the network and
f
is defined as the friction coefficient between the network and the solvent. We deduce fromequation
(1) that the ferrofluidparticle
relaxation time, when the field is cut-off, will beproportional
tofr2/G
where r is a characteristiclength
of the magnetic particle (cf. § 6.1). The elastic energy of the ferrofluidparticle is
equal
to2 I C02
(cf. § 3.2) where 0 is the rotationangle
of the ferrofluidparticle
under H, and C is theproduct
of the shear elastic constant G and theperturbed
volume. So we are able to obtain,independently,
the variations of these two characte- ristic coefficients of thegel,
Gand f,
aroundTg,
as functions of the temperature.
Article published online by EDP Sciences and available at http://dx.doi.org/10.1051/jphys:01983004408098500
986
2.
Experimental
method.The
experiment
uses a method which has been described elsewhere [4]. A small number of magnetic particles (ferrofluids) are added to thegelatin
sample.When
applying
a uniformmagnetic
field H(by
meansof two coils
surrounding
thesample)
these particlestend to line up
along
the field ; amacroscopic
bire-fringence
An is induced in thesample.
In the sol
phase,
we obtain the critical variation of theviscosity il by measuring
thebirefringence
relaxa-tion time, at the instant the field H is switched off.
In the
gel phase,
the measurement of thebirefringence
level leads to the critical variation of the elastic constant; the
birefringence
relaxation timegives
thefriction
coefficient f.
Our ferrofluids are obtained
by
a new chemicalmethod [5]. Every elementary
magnetic grain (100
Adiameter)
is a macroanion immersed in an aqueous solution. The balance between therepulsive
electro-static energy and the attractive
magnetic dipole- dipole
interaction energy leads to anagglomeration
of few grains. The
resulting
agglomerate has theshape
of aprolate ellipsoid
ofmajor
axis 2 a N 1 400 Aand minor axis 2 b - 300 A
[6].
3. Theoretical expression of the
birefringence
induced by the ferrofluid particles.We suppose that each grain has its own internal birefringence. An
assembly
ofgrains
in aliquid
isoptically
isotropic because of the brownian motion,but in the presence of a
magnetic
field thesuspension
becomes birefringent. This
optical birefringence
isrelated to the anisotropy of the electrical
susceptibility
tensor x. This tensor for an uniaxial dielectric
particle
located
by
0, (p is :where
and
G 1 is the dielectric constant of the
liquid,
8jj and 81 theprincipal
dielectric constant of theparticle,
v its volume and L its
depolarizing
factor, withThe
anisotropic
part of the electricalsusceptibility
of a
suspension
of theseparticles
in aliquid
isXan = r(X I I - Xi)(( f(0, qJ) )ø,qJ
where r is the volume fraction of the
particles (r
= N vwhere N is the number of
particles
per unitvolume)
and
f( 0, qJ))
represents the average valueof/(0, T)
with respect to 0 and T. The
birefringence
(whichwe shall call An from now on) is
proportional
to theanisotropic
part of thesusceptibility
tensor, An oc xan.3.1 APPLICATIONS.
3.1.1 In the sol
phase.
- For temperatures above thegelatin
threshold, thegelatin sample
is aliquid
The ferrofluid
particles
are submitted to thermalmotion. If we
apply
amagnetic
field Halong
theZ-axis
(the
Y-axisbeing along
the laserbeam),
the magneticparticles
line up in the field(Fig. 1); they
make the
sample
uniaxial. We can writeIn this case the distribution function
P(O, qJ)
is not wFig. 1. - (J and 9 angles definition in sol phase.
dependent
because of the revolution symmetry around Z-axis. Thuswith
where J-lH cos 0 is the
magnetic
energyand fl
=1 /k T.
After
integration
over 0 and T we get(with fllth
= a) :Experimentally,
we measure :with A = Xil - XI.
3.1.2 In the gel
phase.
- For theoretical andexperi-
mental
simplifications,
themagnetic particles, quenched
in thepolymeric
networkby
a strongmagnetic
held, are allaligned
in the direction of the laser beam(Z-axis).
Amagnetic
field H isapplied perpendicular
to the Z-axis(X-axis).
The measuredbirefringence
is the result of anequilibrium
betweenthe
magnetic
energy - ,uH sin 0 cos qJ and the elasticenergy 2
C02 due to thegel
network : 0 and rp describe theposition
of themagnetic
moment in the field H(Fig. 2) ;
C is theproduct
of the shear elastic constant G times the volumeperturbed by
theparticle
rotation.In this geometry
(Fig.
2) thebirefringence
is obtained,Fig. 2. - Definition of the angles 0 and T. X and Z are
respectively the directions of the applied magnetic field H
and the light propagation direction which is also the initial
position of magnetic dipole p in the gel phase.
making
a thermal average over all the contributions of the ferrofluids,taking
into account their individual orientations. The distribution function is here :Experimentally
we measureFor the critical determination of the elastic constant, it is useful to make a limited
expansion
of On aroundTg
whenPC
1 with a low magnetic field(f3 p,H
1).We find :
with
f(flC) = - 0.33(pC)2
+ 0.15j8C
+ 1.We note that,
surprisingly,
An has a maximum forpC =j:.
0. This maximum must appear at a temperature smaller thanTg (where pC
= 0).4. Experimental conditions.
Gelatin is an
example
of weak gel [7]; the crosslinks between theneighbouring peptide
chains fluctuate with time, at thermalequilibrium.
Here, the evolution of the parameters of thegelatin
is studied as a function of temperature. We avoid the evolution in time of thegelatin with a
good
choice of the temperature variationrate. To this end, a temperature
cycle
is made on agelatin
sample (with concentration 1.5% by weight) prepared
with ferrofluids. We record thebirefringence
level versus T -
Tg. Tg
is determinedby
the sudden988
Fig. 3. - Birefringence function of T -
T g
for two tem-perature variation rates.
variation (or stabilization) of the
birefringence
levelstarting
from the sol(or
thegel) phase. By
examination offigure
3, the critical variations of thebirefringence
presents no detectable difference
(exact overlap)
when the temperature is lowered or increased at a
rate smaller or equal to 3 x 10-4
K/s.
However, with such a rate, theTg
value determination variesby
5 Kdepending
on which is the initialphase.
Thisis due to the fact that the
gelation
processdepends
on the whole
history
of thesample
from the origin(sol
orgel).
5. Critical variation of the elastic constant,
To get the critical variation of the elastic constant,
we
proceed
in thefollowing
way.5 .1 EXPERIMENT. - The
sample (gelatin
+ ferro- fluids) isquenched
at T = 5 OC under ahigh
magneticfield
(Ho
= 5 000 G) in order to line up all the ferro- fluidparticles
in the direction of the laser beam(Fig.
2) ;then this field is turned off. We impose a rotation of the
magnetic particle by applying
amagnetic
field Hperpendicular
to the initial orientation. For each temperature, weadjust
the value of the magnetic field in order tokeep
thebirefringence
level Onconstant The variation of the field H is
given in figure
4 versus temperature. When H is switched off,An relaxes because of the
restoring
force due to the! IFig. 4. - In the gel phase, we adjust the value of the magnetic field H(G) in order to keep the birefringence level constant (An is here equal to 0.11 x 10-2) for each temperature.
When increasing T, the network comes loose, and the field
necessary to get the same birefringence level becomes smaller and smaller.
gel elasticity; the relaxing
birefringence signal
isalso recorded The
advantage
of thisexperimental
procedure is that, close toTg,
H is so small that themagnetic energy J-lH and the elastic
energy 2
Cø2 are ofthe same order of
magnitude
as kT and therefore the gel is notdestroyed by
the small rotation of themagnetic
probes.
Another important
point
is thatTg
cannot bededuced from this
experiment.
In themagnetic
fieldvariation observed there is no great variation near
Tg.
Thus we need another
experiment
to determineTg.
5.2 Tg DETERMINATION. -Experiment : The
following experiment
is performed; thesample
isprepared
inthe same way as in 5. l, but we
keep
the magneticfield constant
during
theexperiment
We record thebirefringence
level On and its relaxation time asfunction of temperature.
Observation :
Figure
5a shows thetypical experi-
mental variation of An as a function of temperature.
The remarkable feature is that we observe near
Tg
a maximum in the
birefringence
level. This maximum ispredicted by
the limitedexpansion
of the theoretical value of An(Eq.
3), but thephysical explanation
ishot simple.
At the field cut off, the
birefringence
relaxationtime
T(T)
isplotted
versus T(Fig. 5a2).
We see thatthe maximum of the relaxation curve coincides with
a temperature T1 for which the
birefringence
levelFig. 5at. - Experiment « An(T), H = constant ». Bire-
fringence level variation as a function of temperature, H remaining constant. The maximum is predicted by the
theoretical value of An (Eq. 3).
Fig. 5a2. - Experimental decrease of the relaxation time
as a function of temperature, when H = constant Fig. 5b. - Experiment « An = constant, H(T»). Decrease
of the magnetic field H(T) as a function of temperature.
measured is
equal
to that ofTg ; ðn(T1)
=An(Tg).
We found
experimentally
thatTg -
T1 = 0.5 ± 0.1 K with quitegood reproductibility.
Thus we haveobtained
aninteresting
method for the determination ofTg ;
in the case(5.2),
where, in order to get thecritical variation of the elastic constant, we measure
simultaneously
H and thebirefringence
relaxationtime as a function of temperature, we
just
need tomake a translation of 0.5 K from the maximum of the
birefringence
relaxation time curve to getTg. Tg
islocated 0.5 K above
T1,
whichcorresponds
to themaximum of the curve T(7).
5. 3 EXPERIMENTAL RESULTS. - Now we look at
figure
3 giving
H(T)
for An = cost The theoreticalexpression
of thebirefringence
level isgiven
by equation 2. For each value of the field(H)
we get thecorresponding
elastic constant C. Figure 6 shows a log-log plot of elastic constant as a function of T -Tg.
We obtain almost a
straight
line over one decade inT -
Tg.
We have fitted the curveC(T - Tg)
forthree different values of the magnetic moment of the
agglomerate (the
three kinds ofsymbols
observedon
Fig. 6).
If we consider that the mean value of the moment is about 5.0 x 10-16erg/G,
we have to noticethat a relative
dispersion
in the value of that moment is irrelevant; no variation in theslope
of the curvecan be observed The mean value of this slope
give
the exponent t,
corresponding
to C -Tg - Tit,
t = 1.7 but if we consider the
asymptotic
slope, thevalue of t is near 2. So a reasonable value of the elastic critical exponent is t = 1.8 ± 0.2.
6. Critical variation of the friction coefficient f.
Now, we try to
explain
thedivergence
of the bire-fringence
relaxation time -r obtained in theexperiments
described above in the gel
phase.
Fig. 6. - Elastic constant variation as a function of T - T g
in a log-log plot (+) J.l = 10-is erg/G; (A) It = 2.5 x 10-16 erg/G; (0) u = 10-16 erg/G. The straightline repre-
sents t = 1.7 and the dash-line t = 2’0.
6.1 RELAXATION PROCESSES. - Two different relaxa- tion processes are known in a two medium system
(network
+solvent)
of this type. We consider the shear movementproduced
by the rotation of theprobe.
We introduce two transversedisplacement
vectors from this
equilibrium
position, one for the network, u(r, t), the other for the solvent,v(r,
t). Thecoupled
motion of thegel
network and the solvent is described byp, G and
f
arerespectively
thedensity
of the network,its shear elastic constant and the friction coefficient between the network and the solvent. There are two
simple
solutions ofequation
4. If the network and the solvent are moving inphase,
u = v, and the return toequilibrium
is due to adamped (because
of viscousterms not considered in
Eq.
4) sinusoidal motion [8]we did not observe
experimentally.
If the network ismoving alone, v = 0; at low
frequencies, equation
4becomes V’u =
f/Gu.
And the relaxation time -r is found to beproportional to fr2 / G (or fr2 / C
as C oc G)where r refers to the
hydrodynamical
radius of the ferrofluid agglomerate.6.2 EXPERIMENTAL RESULTS. - We define a critical exponent for r
(T
-(Tg - T)’").
Thus, the critical, variation off
is obtained : it goes to zero atT g
likeC-r. From a
log-log plot (Fig. 7)
we find x = 0.8 + 0.1.7. Discussion.
Two kinds of results have been obtained for the elastic constant and the relaxation time, near
T g’
inthe
gel phase.
The
experimental
exponent of the shear elastic constant C is centred on the value t = 1.8 + 0.2. This value is ingood
agreement with the theoretical valueusing
theanalogy
between themacroscopic
conduc-tivity
of 3d-dimensional lattice of randomconducting
bonds
[9]
and the elastic constant. On the other hand,it is very different from the classical result t = 3
[10].
Only
a fewexperiments
have beenperformed
in rela-Fig. 7. - Birefringence relaxation time in the gel phase as
a function of T - Tg on a log-log plot..
990
tion to the measurement of the elastic constant critical behaviour in
gelatin.
As far as we know, there is one,due to Peniche-Covas et al. [11] (the initial purpose of which was to find the correct
multiplicity
of thehelical crosslinked zone) which leads to the same
exponent value t = 1.7
[3].
We note that ourexperi-
ment was
performed
with a 1.5% gelatin
system whereas the Peniche-Covasexperiment
was done witha 5.7
% quenched
sample.(In
their case, theexperi-
mental set-up was a
sphere rheometer). Comparing
these results with those in chemical
gels,
we find thatthe exponents t obtained are all
higher
than those of thegelatin
system. As anexample,
for a system madeby
radicalcopolymerization
of styrene-metadivinyl
benzene with a solvent, t was found
equal
to 2.1[12].
In another system obtained
by polycondensation
ofhexamethyl di-isocyanate, t
was foundequal
to 3.2[13].
Theoretically,
the critical variations of the friction coefficient is not well established But onepossibility
is that
f
can be related to thepermeability
of thegel
as
’1/,2 (Darcy’s
law) where, is the correlationlength
of the system (the mean distance between two reticu- lation
points)
and ?I is theviscosity
of the fluidphase
(solvant and finite clusters) [14, 15].If we assume
that q
has a critical behaviour r ~ DTI-s’,
we obtainf -
I ATI2v-s’.
In our
experiment
the relaxation time in thegel phase
is T _fr2/G.
We can suppose that the elastic constant G in adynamic experiment
does not havethe same critical exponent as that measured in a static
experiment.
G =I AT It’.
Theentanglements
increasethe value of the static elastic constant (t’
t).
Thecritical form of the relaxation time is : s =
I AT I-x
with x = s’ + t’ - 2 v. The
experimental
value of xis 0.8 ± 0.1. In
3d-percolation theory
v = 0.88 andwe deduce that s’ + t’ = 2.56 ± 0.1. One
hypothesis
is that the
viscosity
has the same critical exponent in the sol andgel phase
(s =s’).
Thus we need s. Anexperiment quite
similar to thatpreviously reported [4]
wasperformed
in the solphase
where the birefrin- gence relaxation time i isproportional
to theviscosity
of the sample. i was recorded as a function of T. A
log-log plot
is shown infigure
8. Theslope
isdirectly
the exponent s = 0.72 ± 0.1. Then
according
to theprevious hypothesis t’
= 1.84 ± 0.2. This value of the critical exponent of the elastic constant obtained from the relaxation time is very near to the value obtainedFig. 8. - Log-log plot of the birefringence relaxation time
as a function of the temperature difference T - T g in the
sol phase. The slope is s = 0.72 ± 0.1. T is proportional to
the viscosity of the polymeric solution T oc n oc 111 T I-s.
in the static
experiment
t = 1.8 + 0.2. This last feature shows that theentanglements
do not affect the elastic constant in the relaxationexperiment.
8 Conclusion
In
gelatin
(1.5 % inweight)
the critical behaviour of the shear elastic constant, the friction coefficient in thegel phase,
and thedivergence
of theviscosity
inthe sol
phase
have been measured. We have used anoriginal experimental
method which enables the shear elastic constant to be measured very close toTg ;
itis
possible
to have nearTg
an elastic energy(induced by
themagnetic field)
of the same order as kT. Thetime
dependence phenomena
are veryimportant
ingelatin
but we have found areproducibility
criterionfor a defined temperature rate. With these
experimen-
tal conditions, the critical exponents found are very close to those of
3d-percolation theory.
References
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