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Structure induced in suspensions by a magnetic field
Y. Grasselli, G. Bossis, E. Lemaire
To cite this version:
Y. Grasselli, G. Bossis, E. Lemaire. Structure induced in suspensions by a magnetic field. Journal de
Physique II, EDP Sciences, 1994, 4 (2), pp.253-263. �10.1051/jp2:1994127�. �jpa-00247959�
Classification Physics Abstracts
75.30 64,75 82.70D 46.60
Structure induced in suspensions by
amagnetic field
Y.
Grasselli,
G. Bossis and E. LemaireLaboratoire de Physique de la Matikre Condensde (*), Universitd de Nice
Sophia Antipolis,
Parc Valrose, 06108 Nice Cedex 2. France(Receii>ed 3
February
J993, revised J9 October J993,accepted
9 November J993)Abstract. Magnetorheological as well as electrorheological fluids exhibit a phase separation when a field is
applied
to thesuspension.
We observe the formation of aggregateselongated
in the direction of the field and whose length L is fixed by the thickness of the cell. The average radiusb of these aggregates has been measured for L between 100 ~m and 700 ~m for two volume
fractions 4l 5 % and 4l 10 %. In this range we find for a magnetorheological fluid composed of micronic superparamagnetic panicles an experimental law b cc a(Lla)~ with an exponent
n m 0.67 = 0.04. We can recover this experimental law and predict the characteristic size of the aggregates from the knowledge of the
magnetic permeability
of theparticles
with a model based onthe hypothesis of close
packed
aggregates. The agreement with theexperiments
isgood especially
at the lower volume fraction.
Actually
on alarger
range of thicknesses our model predicts acontinuous increase of this exponent towards a final value of one for large values of
Lla.
1. Introduction.
Magnetorheological suspensions
arecomposed
ofmagnetic panicles
whose size, in the micronic range, is at least two orders ofmagnitude larger
than in the better knownmagnetic suspensions,
called ferrofluids. The inducedmagnetostatic
force between twopanicles being proportional
to the square of the radii of thepanicles,
it is muchlarger
for M. R. fluids than for ferrofluids. As a counterpart, sedimentation is nolonger prevented by
Brownian motion and the micronic range represents anoptimum
size. Under theapplication
of amagnetic
field[of
a fewOersted]
we observe a transition from ahomogeneous liquid suspension
to a solid one I].
This transition from a
liquid
to an apparent solid state is due to the formation ofelongated
aggregates ofparticles
which arealigned parallel
to themagnetic
field andjoin
theopposite
sides of the cell
containing
thesuspension.
These links areresponsible
for the apparent solid behaviorsince,
for instance, if the field isperpendicular
to the two disks of a rheometer, we need to increase theimposed
torque above a critical value in order to break these aggregates(*) CNRS URA 190.
and obtain a continuous rotation of the upper disk. The onset of a
yield
stressstrongly
modifies therheological
behavior and opens thepossibility
to realizehydraulic
devices where theviscosity
iselectronically
controlled. Thiseffect,
due to themagnetization
of the solidpanicles by
amagnetic
field can, as well, be obtained with dielectricparticles polarized by
theapplication
of an electric field. Theseelectrorheological
fluids are theobject
of arising
interest both for theirpotential applications
and for theinteresting underlying physics [2-41. Clearly
weneed to obtain a
good knowledge
of the structure of thesesuspensions
theshape
of theaggregates, the distance between them, the internal arrangement of the
particles
if we want to be able topredict
thechange
of theirrheological properties
in the presence of a field.For
monodisperse
dielectricpanicles,
Tao et al.[5,
61Predict
and observe an internal structure for these aggregatescomposed
of chains ofspheres (of
radiusa)
with agiven
chain surroundedby
four other ones at a distance a/
witha shift of a radius in the direction of the
applied
field and four next-nearestneighbors
at a distance a/,
but without shift. Sucha
configuration
called B.C.T.(body
centeredtetragonal) gives
the lowest internal energy. In arecent paper,
Halsey
and Toor [71 model the aggregate as aspheroidal droplet
and calculate theintemal energy on the basis of electrostatics of continuous media.
They
furthermore introducea surface energy
U~ proponional
to the square of theapplied
field EU~
> 0.Ip
~E~ aS~
withp
=
~ l)
S~ is the surface of the aggregate, a the radius of a
panicle
and s the ratio of thepermittivity
of the solidparticle
to that of thesuspending
fluid. In thisapproximation U~
isindependent
of theshape
of the aggregate.Minimizing
the total energythey obtain,
in the limit where the ratio of theequatorial
semi-axis to the totallength
b/L tends to zero, adependence represented by
b cc a
(Lla
)~'~. In this model the energy of interaction between different aggregates is not takeninto account.
Actually
when the aggregates fill the gap between theelectrodes,
the existence ofimage dipoles
whichimpose
thepotential
on the electrodes isequivalent
to the introduction of aggregates of infinitelength.
Then, at this last stage ofaggregation,
thedepolarization
field andconsequently
therepulsive
interaction between the aggregatesdissappears.
We expect the surface energy to be
given by
the sameexpression
formagnetic
and fordielectric
panicles:
wejust
have toreplace
sby
p, themagnetic permeability,
andE
by
H, the averagemagnetic
field inside thesample.
This will be true aslong
as thepermeability
does not vary too much with themagnetic
field. In aprevious
work[I]
we havereponed experimental
results about the average size of these aggregates i>ersus the initial volume fraction 4~ of thesuspension
and found a linear law which we were able toexplain
witha model
taking
into account the balance between the volume energy and therepulsive
energybetween aggregates, without
introducing
a surface energy. In thefollowing
section of this paper we propose a modelincluding
both therepulsive
energy between the aggregates and the surface energy whichpredicts
the average size of the aggregatesby
a minimization of the totalmagnetic
energyanalogous
to the one used for the determination of the deformation of ferrofluidsdroplets [8-101.
In section3,
we present someexperimental
results and compare them with the theoreticalpredictions.
We concludeby
a discussion of thevalidity
of this model and of itsapplication
toelectrorheological suspensions.
2. Theoretical model.
We consider the case of a
magnetic suspension
submitted to an extemalmagnetic
fieldHo
muchhigher
than the fieldcorresponding
to the transition and we model the structure of thesuspension by
ahexagonal
array ofellipsoids
of transverse semi-axis b and oflength
L
(cf. Fig, I).
In thedipolar approximation
the ratio A of themagnetic
energy toptical(
axis
/~
2bd
~ ~ ~ ~
ri i. . . ,
,~ ~ ~ ~ ~
L i~ ~ ~ ~ ~
~ ~ ~ ~ ~
i
Ho
@ @
Fig. I. Schematic
diagram
of the structure A top view B side view. The aggregates are assimilated toprolate spheroids
of semi-axes b and f, L=
2 f is the thickness of the cell,
kT is
given by
A=
(4
VPo pi p~
H~/
(4kT)
wherep = I is the
magnetic permeability
of theliquid phase.
In ourexperimental
case we find A=
2.63
H~
(De ). For the terminal fieldwe
have used
(50 Oersted)
we obtain A=
6 500.
Owing
to thishigh
value of A we canneglect
thethermodynamic
forces and suppose that the internal structure of the aggregates is the B.C.T.equilibrium
structure with adensity
~P~=
2 w/9. This is also
only
under these conditions thatwe can use an
equation
similar to(I)
which assumes that the surface energy is localized on the lastlayer
ofparticles.
On the other hand themagnetic
field is still lowenough
so that we canconsider that the
magnetic permeability
p is almost constant, then themagnetic
energy isgiven by ii II1
N~ M~ Ho
U~ (2)
with N
~
the number of aggregates and
M~
themagnetic
moment of an aggregate. If we considera
spheroidal (prolate)
aggregate (cf.Fig.
I) of semi-axes b andI,
withbli
< I,
composed
of anhomogeneous magnetic
medium of averagepermeability
p~, the internalmagnetic
field isconstant inside the aggregate and the
homogeneous magnetic
moment isgiven by (in
e-m-u-~ p~ I
Ho
M~
= V~(3)
4 " +
n~(p~ 1)
where
V~
is the volume of the aggregate and n~ thedemagnetizing
factor which for anellipsoid
of
excentricity
e= (I
b~li~)~'~
isgiven by
n~ =
~~
~~
(In ~
2ej (4)
2e -e
If the ratio of the two axes of the
ellipsoid
K =2b/L is very small, we haven~ 4
(1
+log
K K ~, andminimizing
the surface energy(Eq. (I)) plus
the volume energy(Eqs. (2)
and(3))
with respect to bgives
the behavior b cc a(Lla
)~'~reported
in[7].
Let us seemore
precisely
thephysical
mechanism.H~ H~
Fig. 2, The local field, H~, on a
spherical
panicle located on the surface is lower than the local field, H~, on a panicle in the bulk.As the
ellipsoid elongates
thedemagnetizing
factor tends to zero, then themagnetic
moment and the absolute value of the energy increasecontinuously
so we could expect that the averageradius,
b, of the aggregate will tend to the radius of aparticle. Actually
we have to take intoaccount two other
energies which,
on the contrary are favorable to thegrowth
ofb. One is the
repulsive
energy, U~, between the aggregates and has been discussed in aprevious
paperill,
and the other,U~
is a correction to the volume energy calculated on the basis of a continuous medium,coming
from the finite size of theparticles.
This contributioncan be understood as a surface energy which can be calculated
numerically
anddepends
on theconfiguration
of the first two or threelayers
ofpanicles
below the surface[121.
In order to understand theorigin
of this energy and tosimply
estimate its value in a mean fieldapproach,
let us compare the local
magnetic
field on aspherical panicle
inside the aggregateH~
to the local fieldH~
on aparticle
located on the surface(cf. Fig. 2).
For ahomogeneous ellipsoid
whose main axis isaligned
with the field in the = direction we haveH~=Ho+~"~-4wn~P.
The field 4 wP/3 where P
=
M)/V~
comes from the inner surface formedby
thespherical cavity
which represents the exclusion volume of aparticle (Fig. 2)
and 4wn~P
is thedemagnetizing
fieldcoming
from the external surface of theellipsoid.
For aparticle
on the surface, if we assume that thepolarization
P remains constant inside theellipsoid,
the difference with the former case will come from the absence ofpolarization
on a halfspherical
surface which will
give
for the surface fieldH~mHo+~"~-4wn~P.
The local field on the
particles
situated on the surface is then lowerby
a factor2 wP/3
relatively
to the bulk local field. Then the realmagnetic
moment of the aggregate,M~,
will be lower than that,M),
calculated for ahomogeneous ellipsoid
M~
=M) Ni &mj (5)
where
&mi
= a P2 wP/3 is the difference between thedipolar
moment of apanicle
inside the aggregate and the one on thesurface;
aP=a~p,
withp
=(p~ I)/(p~ +2),
is thepolarizability
of aspherical panicle. Ni
is the number ofpanicles
on the surface of theellipsoid.
With thiscavity
model&m,
ispositive
andcorresponds
to a surface tension since it decreases the totaldipole
of the aggregate and so increases the electrostatic energy.Actually
the value of
&mi
isquite
sensitive to theprecise
structure on the surface. With the notation of 112]
we have moregenerally &m~
= m
(M~
I where m is the bulkdipole
of apanicle
inside the aggregate andM~
=
m~/m
the normalizeddipole
of thelayer
v(v
= Ibeing
the surfacelayer). Using
for the bulkdipole
m=
M)/N~
whereN~
is the number ofparticles
inside the aggregate we cangeneralize (5) by writing
M~
=M)(I n~)
with n~=
zN~,(ji~ 1). (6)
~P
v
In the
homogeneous cavity
modelonly
the surfacelayer
is concerned and we have(Mi
I=
(a
P2 wP/3 )/m, orusing
P=
N
~
m/V~
anda P
=
pa~,
we obtain(M,
I= p
~P~/2.
In a lattice model we have shown in 1121 that the contribution of the surface
layer
was far greater than all the others, so we can stillkeep only
the firstlayer.
For a B-C-C- lattice andPIP
- oo an exact calculusgives (M, 1)
=
0.3 for ~P
= 0.65 and
(Mi
-1)=
0.37 for
~P
=
0.67. We did not calculate this
quantity
for a B-C-T- lattice but we do not think that the result would be very different. In any way this result is not far fromp
~P~/2 and we shallkeep
this value as agood
estimate of the relativechange
ofdipole
moment on the surface. We have still to estimateNi
the number ofparticles
on thesurface,
S~=
2
wb~
+ 2w
(bile sin~'
e, of the
ellipsoidal
aggregate. If we consider a surface with ahexagonal packing
we find N i = S~/(2 / a~).
Thispacking corresponds
to the denserplanes
of the B. C-T- lattice and weshall take it as the upper realistic limit of
Ni.
With these values ofNi
and of(Mi
I we obtainS~ w
~~ ~
Va
~ 3/
~~~If we introduce the
expression (6)
ofM~
in the totalmagnetic
energy(cf. Eq. (2)),
the term with n~ will represent the contribution of the surface energyU~.
On the otherhand,
we also need to consider therepulsive
interactions between the aggregates. If we assume a structure formedby
a two-dimensional
hexagonal
array ofellipsoidal
aggregates, each onebearing
the same totalmoment
M~,
we can find the momentM)
of agiven
aggregate, I, considered as ahomogeneous
medium,
by writing
M~
=
a~
Ho T[
M(8)
a
I
a
The
quantity T(
is the propagator of the field between two aggregates, andj,
oflength
L whose axes of symmetry are
separated by
a distanced~~. It can be obtained
easily
in thedipolar approximation,
with all thepolarization
located on the revolution axis of each aggregate. In this case the field of oneaggregate
isequivalent
to the field H=
«r/r~
of twocharges
«~= ±
M~/L
located on eachextremity
of the axis of revolution of theellipsoid.
Because of the
cylindrical
symmetry we can consideronly
the z component of the field in thesum over all the aggregates. Then the average
(H~)
=
T[~.M~
over thelength
of theaggregate of the field
coming
from the aggregatej
defines thequantity f~
which will begiven by
rJ ~ )
~~j /~~~/~ l. (9)
Of course, if d,~/L » I, we recover the
dipolar
propagator forparallel dipoles
in the sameplane
fj
=
1/d(.
The
polarizability,
a ~corresponds
to the ratioM)/Ho
for an isolated aggregate and isgiven by equation (3).
The totalmagnetic
energy per unit volume is stillgiven by equation (2)
butwith now
M~
obtained from the solution ofequations (6)
and(8).
We thus obtainU~ ~PH( (p~
)(I n~)
I
~P~ 8 w I +n~(p~
I I +n~(I n~)
~~~~The ratio ~P/~P~ comes from the
equality N~V~/V=
~P/~P~. The values of n= andn~ are
given by equations (4)
and(6) respectively
and n~= a ~
z f~
represents the effect of theJ
repulsive
interaction of one aggregate with all the others. The value of n~ can be calculatedby summing (9)
on atriangular
lattice orby replacing
the sumby
anintegral
: the two results arewithin 2 fl so we shall take the
analytical
result which is(p~-I) jj
~pj~lj d( oj j2~P~
n~ = I + with
do
= b
(l
II +
ii=(p~
I )lPa
L~ L 3 *The
quantity do
is the radius of acylindrical cavity containing
the reference aggregate andsurrounded
by
ahomogeneous
medium of averagedensity
~P instead of thehexagonal
distribution of
figure
I. It is worthnoting
that the use ofequations (6)
and(8)
amounts tointroduce in a self consistent way the surface energy of an aggregate and the
repulsive
interaction with the other aggregates.
3.
Experimental
results andcomparison
with the model.The
experiments
have beenperformed
with asuspension
ofmagnetic particles
at two volume fractions ~P=
lo fl and 4l
=
5 fl. The
panicles
arespherical
butpolydisperse
with an averagediameter of 0.8 ~Lm.
They
arecomposed
of the samegrains
ofmagnetite
whichusually
compose a ferrofluid
but,
instead ofbeing
free in theliquid phase,
thesegrains
areimprisoned
in a
polystyrene
matrix. The size of thegrains
is less than 100I
andeven if these
grains
do not rotate in the matrix theirmagnetic
moment canjump
from one direction of easymagnetization
to another
by
thermal activation since we haveKV~
« kT where K is theanisotropy
constant andV~
the volume of thegrains
ofmagnetite. By measuring
themagnetization
curve on a driedpowder
we have verified that thesepanicles
weresuperparamagnetic
and that we had nohysteresis.
Themagnetic permeability, p~,
of theparticles
has been deduced from themeasurements of the average
magnetization
of thesuspension
at several volume fractions withthe
help
ofBruggeman's theory
1131.
For amagnetic
field of a few tens of Oersteds, we obtain p~ =37. Note that the
permeability
was constant in this low field domain. Thesuspension
wasplaced
between two transparent disks whosedistance,
L, is setby
different spacers from 150 ~Lm to 700 ~Lm. The field isperpendicular
to the disks and is raised veryslowly
to its terminal value(50 Oersted)
in order to get anequilibrium
structure. Thetypical rising
time was 0. I Oersted per minute and we have verified that forlonger
times the results were the same.The terminal value of 50 Oersted
corresponds
to thecompletion
of theaggregation
process asobserved
by light
transmission : above this value there was no further increase of thetransmitted
light ill.
The structure is observed with a
microscope
whoseoptical
axis isparallel
to the field. Theimages
are recorded on a computer and treated with animage analysis
in order to obtain theposition
of the center ofgravity
of each aggregate. Atypical
view of theprojection
of the aggregates on aplane perpendicular
to the field isrepresented
infigure
3A for ~P=
5 fl and in
figure
38 for ~P= lo fl. At the
highest
volume fraction theprojections
do notcorrespond
to anellipsoidal shape
for theaggregates.
This branchedshape
has somesimilarity
with the Patterns observed in the ferrofluids when theinitially ellipsoidal droplet
bends and distorts in acomplicated
pattern whichdepends
on theintensity
and on the rate of increase of themagnetic
field
i141.
Thedependence
of theshapes
of the aggregates on the finalamplitude
of the fieldyf-~Wj*m&~
, -, o
z,~«
~,
M ~j~ I&~
_~r
* ~
i
~i
a)
b)
Fig. 3. real stricture observed by
optical
microscopy. The view corresponds to aprojection
on aplane
perpendicular to the magnetic field (which is along the axis of observation) 3a Volume fraction of 5 %3b Volume fraction of 10 %.
and on the time
history
of itsapplication
has also been observedrecently
on micronicdroplets
of ferrofluids
[lsl.
On the other hand, on another device where the upper disk can translate[191,
we canexperimentally
see that all the aggregates connect the two walls of the cell.We can measure
experimentally by image analysis
the averagedistance, d,
between thecenters of
gravity
of the aggregates. This ispossible
aslong
as these aggregates remain wellindividualized even if their
projections
are notsimple
disks (cf.Fig. 3).
We obtaind
by taking
the maximum of thepair
correlation function g(r)
of theseparations
between the aggregatesill.
In order to relate thisexperimental
distance to the semi-axis b of our idealizedellipsoidal
aggregate we represent the structuredsuspension
as shown infigure
I. In this situation we haveb=dl~~~ (12)
4w~a
where ~P~ = 0.69 is the volume fraction inside the aggregates.
The
log-log plot
of theexperimental
values ofb,
versus the thickness of the cell, isrepresented
infigure
4 (solidcircles)
for a volume fraction of lo fl and infigure
5 (samesymbols)
for a volume fraction of 5 fl. These values can be fittedby
astraight
line with aslope
of 0.67 = 0.04 and of 0.68 = 0.04
respectively.
On the samefigures
areplotted
the valuesobtained
by
the minimization of the totalmagnetic
energy (cf.Eq. (lo)
withrespect
tob for the same values of L
(empty circles).
We see that thepredictions
are 40 fl too low for the volume fraction of lo fl but are very close to theexperimental
values for 5 fl. Thediscrepancy
at ~P
=
lo % is not so
unexpected
in view of thenon-ellipsoidal shape
of the aggregates. We also have toemphasize
that the intemalpermeability
of the aggregates isdirectly
obtained fromBruggeman's theory
:(with
p~=
37 and
~~
=
0.69 we obtain p~ =
22)
so we have no free parameter in this model.~2
b
I O w
~~o
loo 300 500 700 IOOO
L
Fig. 4.
Log-Log
plot of the transverse ~emi-axis of the aggregates versus the thickness of thesample
for a magnetic suspension of initial volume fraction ~fi =10%.(o)Theoreticil prediction
fromequation
(10) (Slope 0.7 ). j.) Experimental results(Slope
0.67 = 0.04) obtained by imageanalysis
with thehelp
ofequation
(12) to relate h and d.~i
b
~~o
~~~
L
~~~ ~~~Fig.
5.-Same as forfigure4
with a volume fraction: 4l 5§F. (o)Theoreticalprediction
fromequation (10)
(Slope
0.68). (.)Experimental
results obtainedby
imageanalysis (Slope
0.68 = 0.04).It appears that this model is
quite
efficient inpredicting
the average size of the aggregates if the volume fraction is not toohigh.
We have calculated for the samemagnetic suspension
at avolume fraction of 5 % the size of the aggregates for a much
larger
range of cell thicknesses : lo < L< lo 000 ~Lm. The results are
presented
infigure
6(solid curve)
on alog-log plot.
We first notice that we do not have astraight
line there is no well defined power law defined for the whole range of distances. For low values of L 10 ~Lm< L < 50 ~Lm we find an exponent of
0.35,
for the intermediate range where we have done someexperiments,
we find anexponent close to
2/3
and in the range lo 000 ~Lm< L
< 20 000 ~Lm we find 0.85.
Ultimately
when the effect of the surface tension becomes
totally negligible
the exponent will tendtowards
unity
since in this case all the terms in the energyonly depend
on the ratiob/L. This is the case for the dotted curve in
figure
6 which represents theprediction
of the model without the surface energy(n~
=0).
The other limit where weneglect
therepulsive
oo
/
i o
b
, /, , , , , / / / /
O-1 '
Fig.
6. Theoretical prediction of the transverse semi-axis, b, of the aggregates versus the thickness L of the sample for a volume fraction of 59b. Fulltheory
equation (10).Equation
(10) with n~ = 0 no surface tension.Equation
(10) with n~= 0 : no
repulsion
between aggregates.energy (n~ = 0
)
andonly
take into account the surface energy isrepresented by
the dash-dottedcurve. For
large
thicknesses we tend to an exponent 2/3 in the range loo~Lm-700
~Lm we havea
slope
of 0.57 and at thebeginning
of the curve aslope
of 0.33. Notethat,
with the value of the surface tensiongiven by [71,
the surface effect is dominant at low thicknesses and in ourexperimental
range the values areonly
20-30 §b too low. This would not appear if we take thedipolar approximation
for the surface energyequation (I)
whichgives
much lower values of b.Other
experiments
with alarger
range of thicknesses would be useful toverify
thepredictions
of the model and we aredesigning
a new sealed cell which operate in alarger
range. Some similar
experiments
have also been carried outrecently by
Liu et al.[lsl
on asuspension
ofrigid
ferrotluiddroplets. They
haveexplored
the range of thicknesses between lo and 500 ~Lm and found the samequalitative
behavior as wepredict
: there is no constantexponent
for the variation of b with L and at low thicknesses we tend to an exponent close to1/3.
4. Conclusion.
We have shown that it was
possible
topredict
theequilibrium
structure inducedby
amagnetic
field in amagnetic suspension
if we introduce both therepulsive
interactions between the aggregates and the surface energy due to the finite size of thepanicles.
Thisstudy
wasperformed
with amagnetic suspension mainly
because we haveprecise
measurements of themagnetic permeability
which furthermore is much easier to obtain than thepermittivity
of asuspension (in
the latter case,problems
are met due to the ionic cloudssurrounding
theparticles
and to thecharge
on theelectrodes).
We have made somepreliminary experiments
with an
electrorheological suspension composed
of silicapanicles
activatedby
water in a lowviscosity
silicone oil. The cell was formed of twoglass
disks coated with transparent electrodes.Unfortunately
ourparticles slightly
aggregate under the effect of electrostatic forcesthey disintegrate
undermixing
but when the field is turned off, the Brownian motionitself does not allow to recover a
homogeneous
state. In these conditions we have someirreversible
aggregation
and the model based on a minimization of the electrostatic energy alone willprobably
fail. On the other hand the aggregates were not so well defined and theuncenainty
on the distance waslarger.
Nevertheless we have tried somepreliminary experiments
on thissuspension
and we have found that in the same range of thicknesses 100< L
< 700 ~Lm the size of the aggregates was
increasing
with an exponent close to 0.6. Asalready
said in the introduction the electrostatic case is different because thecharges brought by
the electrodes cancel thedepolarizing
field of each aggregate. Then, at firstsight,
the modelshould
apply
if we set therepulsive
interaction to zero (n~ = 0 inEq. (9))
and indeed the exponent of 0.6 isquite compatible
with a surface tension effect(cf. Fig. 6).
Nevenhelessexperiments
withpanicles
which do not sticktogether
or on the electrodes should be made in order to getequilibrium
structures in the presence of an electric field.A
systematic investigation
with differentparticle sizes,
differentpermittivities (which
can be variedby changing
thefrequency
of theapplied field),
should enable us to decide if this model allows the size of the structures in electro andmagnetorheological
fluids to bepredicted
or if it is restricted to some set ofparameters.
Theprediction
of the structure induced inquiescent
suspensions by
an external field is the first step in thestudy
of a broader class ofordering phenomena,
inpanicular,
shear inducedordering
which is found incomplex
fluids like micellar fluids, nematics,suspensions [16,
171 andelectrorheological suspensions.
In theselast ones we have observed the formation of
stripes
ofparticles aligned parallel
orperpendicular
to the flow[18, 19]
in the presence of to an electric field and of a sinusoidal shear.Actually,
these E-R- or M-R- fluids are very convenient for thestudy
of shear inducedordering
since we can veryeasily modify
the energy of interactions between the solidparticles by changing
theapplied
field. Such systems shouldhelp
to the elaboration of atheory
able toexplain
shear inducedordering.
Acknowledgments.
This work was realized with the financial
suppon
of Rh6ne Poulenc. We are also verygrateful
to A.
Audoly
and B.Gay-Para
for their technical support.References
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