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Domain structures in thin layers of a ferrocolloid
Yu. Buyevich, A. Zubarev
To cite this version:
Yu. Buyevich, A. Zubarev. Domain structures in thin layers of a ferrocolloid. Journal de Physique
II, EDP Sciences, 1993, 3 (11), pp.1633-1645. �10.1051/jp2:1993223�. �jpa-00247930�
Classification Physics Abstracts
75.50M 75.70K 82.70
Domain structures in thin layers of
aferrocolloid
Yu. A.
Buyevich
(~,~) and A.Yu. Zubarev (~)(~) Mod41isation
en M4canique, Universit4 Pierre et Marie Curie, 75252 Paris, France
(~) Department of Mathematical Physics, Urals State University, 620083 Ekaterinburg, Russia
(Received
16 March 1993, revised 15 July1993, accepted 5 August1993)
Abstract We consider the problem offormation ofstructures composed ofidentical domains
in a ferrocolloid that fills a space between two closely situated parallel planes under action of
a normal external magnetic field. Those structures begin to arise under conditions favouring the phase separation of the ferrocolloid. An inhomogeneous system
including
two equivalentcolloidal phases would ultimately evolve due to Ostwald ripening, but for
a scaling effect of the
planes that stops the evolution at a certain level and makes for the resulting domain structure being stable. A method to find out main characteristics of the domains, such as their size and
concentration, is developed for both chaotic and regular
(ordered)
structures.1 Introduction.
Numerous
experiments,
among which those in [1-5] should becited,
evidence a ferrocolloidlayer
betweenparallel
boundaries to lose itsthermodynamic stability
if thestrength
of anexternally applied
normalmagnetic
field exceeds some critical value. As aresult,
a system ofcylindrical
domainsdevelops,
the concentration ofmagnetic particles
inside the domainsbeing
considerably higher
than that in the ambient parent colloidalphase.
Such a transformation from anoriginal homogeneous
state to that with a stable domain arrangement resembles to all appearances aphase
transition of the first type. A similarphenomenon
of the emergence of domains is alsospecific
to thinlayers
of anelectrorheological suspension
under action ofa constant electrostatic field [6].
Visually,
the mentioned domains are like domains in solidmagnetics
or vortice structures that are sometimesgenerated
insuperconductors
of the second type.The authors are aware of the
only
attempt totheoretically explain
theorigination
of the domainsby assuming
the reason of thisphenomenon
to be due to the break ofthermodynamic stability
of ferrocolloids insufficiently
strong fields and to anensuing
process ofspinodal
decomposition
[7, 8]. Thetheory
of these papersleads, however,
to a conclusion that theparticle
concentration has to varysmoothly,
almostsinusoidally, along
thelayer plane.
Such a conclusion does not
correspond
in the least to availableexperimental evidence,
accord-ing
to which all the domains arepractically
of acylindrical shape
and possesseasily
discerniblesharp
boundaries. This cannot beexplained
with the aid of almostsinusoidally varying
concen-trational fields.
Moreover,
it has been shown in [4] that there ismerely
acomparatively
small number ofrandomly positioned
domains if the external field is either weak or ofreasonably
moderate
intensity,
so that the domainassemblage surely
reminds of a two-dimensional ideal gas. The domains becomecapable
offorming
an ordered latticeonly
at a condition of their concentrationbeing sufficiently high,
what demands a ratherstrong
field. Atlast,
it has beenrigorously proved
[9] that thelayer
boundaries cannot exert astabilizing
influence on anearly
stage ofspinodal decomposition
whichhappens
to be relevant to thetheory
of [7, 8].A main
physical
reason for theorigination
of domain systems seems to be clearenough.
The
dipole interparticle
interaction inmagnetic dispersions
results in an effective attraction between theparticles
whichsignificantly
increases as thestrength
of an externalorienting magnetic
field adispersion
isexposed
to grow [10, 11]. The attraction tends to cause con-densation of the
particles
whereas theparticle
thermal motion opposes this process. If thedispersion
concentration issufficiently high and/or
its temperature issufficiently low,
the dis-persion thermodynamic stability
cannot bemaintained,
and a process ofphase separation
of thedispersion
into twophases
with different concentrations of theparticles
evolves. Such a process isquite
similar to thatcommonly
observed in molecular systemsundergoing
a first typephase
transition[10-13]. Examples
of transformations of the same nature in colloids inwhich the
interparticle
attraction is of anotherphysical origin
can be found in[14, 15].
A constant external
magnetic
field intensifies attraction ofparticles
of a ferrocolloid and so favours itsseparation
into two colloidalphases.
The process ofphase separation
starts with the formation of initial critical nuclei of a newphase
thatgive
rise todropwise
aggregateswhich are
elongated
in the external field direction[12].
If the ferrocolloid wereunbounded,
theaggregates
wouldincessantly
grow till Ostwaldripening begins
to dominate the newphase evolution,
whenlarger
aggregate continue to increase in size at the expense of smaller ones.A finite distance between the
layer
boundaries sets,however,
a limit to such a process ascompared
with that in the bulk. When the aggregate size comes toequal
thisdistance,
any aggregate can continue to growonly
in the radialdirection,
that is, in thelayer
plane. Then theaggregate
radiuseventually
grows under a condition of constantlength,
and the aggregatevirtually
transforms into a domain. Thisresults,
of course, instrengthening
of the aggregatedemagnetization
field andultimately
causes an energyexpenditure
to become toohigh
toprovide
for the domaingrowth
over a certain critical size.In what
follows,
thisqualitative picture
isproved
to be correct and mainproperties
ofresulting
stable domain arrangements are found out and discussed at somelength.
2» Chaotic
arrangements.
Consider an
assemblage
ofnearly cylindrical
domains of radius a in a ferrocolloidlayer
of thickness 21 betweenparallel plates,
The ferrocolloid issubject
to an externalmagnetic
field ofstrength
Ho which is directednormally
to theplates,
Let us introduce the volume concentration#d
ofmagnetic particles
in eachdomain,
also a surface concentration of the domains themselves that represents the fractionoccupied by
domain crossections in thelayer plane
andequals
s =
gra2n,
nbeing
understood as the number of the domains per unit area of thisplane.
In accordance with themajority
ofexperimental
data, we assumeright
away the domains to bethin,
what means the domain radius a to be much smaller than thelayer
thickness I, a < I.Our intended
goal consists, first,
inidentifying
conditions at which there exists a ther-modynamically equilibrium
domain arrangement within the ferrocolloidlayer and, second,
infinding
outproperties
of thearrangement.
Thisimplies
that notonly
the domainshape
and their surface concentration but also themagnetic particle
concentration and themagnetic
fieldstrength
both inside the domains and in interstices between them have to besimultaneously determined,
toincorporate
thefindings
into acomplete
statisticalthermodynamic
model of the system understudy.
Construction of the last model is alsoby
no means an easy task.Although
fundamentals of such a model have beenrecently
disclosed in[11],
one canhardly
hope
to overcome all obstacles and toget
acomplete
solution of the wholeproblem
withoutsome decisive
simplifications,
which we are nowgoing
to enumerate.First of
all,
we presume the domains to beregular
circularcylinders,
and their surface con- centration(which evidently equals
the domain volume concentration within thelayer)
to be small ascompared
withunity.
Then each domain can beregarded
as immersed in a ferrocol- loidal medium whose properties, such as concentration ofparticles by
volumeii,
Pressure piand
magnetic
fieldstrength Hi approximately
coincide far away from the domain with their actual values which can be gotby averaging
overmerely
the interstices. The lastassumption
is madesolely
tosimplify
needed calculation. If it were wrong, anapproximation
based onthe self-consistent field
theory
could beused,
in which case the mentionedquantities
should be looked upon as those obtainedby averaging
over the wholelayer plane. Obviously, quantities ii,
Pi and Hi can beregarded
as uniform.Even
though
the aboveassumptions
hold true, we areagain
faced with a very difficultproblem.
A crucialsimplification
can beattained, nevertheless, by noticing
that themagnetic
field within a thin
cylinder
normal to thelayer
boundariesdepends mostly
on the field H2 near its sidesurface,
and that thedemagnetization
field h vanishes asall
tends to zero. It meansthat we are free to
take,
in the zerothapproximation,
thestrength
of themagnetic
field insidea domain to be
equal
toH2
"
Hi
This field induces a domainmagnetization Md
that has tobe found with the
help
of some model ofmacroscopically
uniform ferrocolloids(e.g.,
seeill] ).
Now,
let us find thedemagnetization
field h causedby
one domain that canjustly
beregarded
as
uniformly magnetized
with aspecific magnetization
Md. This can be doneby summing
up field contributions createdby
infinitesimal parts of the domain. If oneneglects
effects due to possible refraction of h at thelayer boundaries,
which have to be of littlesignificance
because of theaccepted inequality
a < I, one gets for any point ro near the domain surfacefit I-zo a 2W ~2 1
hz izo,
To) =T /~~~ dz£
r dr d@13v v)
R~
=
r~
+r(
2rro cos@ +z~. (2.1)
This
expression
defines a component of hparallel
to the symmetry axis of thedomain,
and zo and To are axial and radial (To >a)
coordinates of ro in thecylindrical
coordinate system withan
origin
at the intersectionpoint
of the donlain symmetry axis and the middleplane
of the ferrocolloidlayer. Quantity ii
is themagnetic permeability
of the ambient ferrocolloid. It is easy to showthat,
at a < I, radial component hr of thedemagnetization
field is much smaller thanhz
almosteverywhere,
so that there is no need to take it into account atall,
and vector h may beregarded
as directednormally
to thelayer plane.
It is convenient to use
further,
instead ofhz(zo,
To),
a value of thisquantity
obtainedby averaging
over thelayer
thicknesshi (T0) "
j /
hz(20,T0) dZ0, (2.2)
without noticeable loss of accuracy. Then one is
always
able to writehi (To) " -MdL
(all, roll), (2.3)
where L is a known function that can be
readily
written out when necessary, inconformity
with the definitions in
(2.I)
and(2.2).
Consider,
next, acylinder
in a field ofstrength H2
= Hi + hi directed
along
thecylinder
axis and introduce#2
and p2 as theparticle
volume concentration and pressure at the sidecylinder
surface outside the
cylinder.
Similarquantities pertaining
to the interior of thecylinder
aremarked with a
subscript
d. All thethermodynamic potentials
of the uniform ferrocolloidalphases
areadmittedly
functions of the above-introduced variables. Furthermore we shall con- sider chemicalpotentials pip, #, H)
andpo(P, #, H)
of themagnetic particles
and of molecules of thesuspending liquid, respectively.
Conditions of
thermodynamic equilibrium require
the chemicalpotentials
inside andjust
outside the
cylinder
to coincide.Also,
mechanicalequilibrium
demands the pressures at both sides of thecylinder
to bedistinguished by
the surface pressure~la,
where ~ is understood as the surface tension coefficient. Thus we have@d " @2 , @0d " @02
, Pd P2 " ~
la,
Pj =
(vj, #j,
Hi + hi, Poj = Po
(vj, #j,
Hi + hi,
j = d, 2.
(2.4)
Simple
evaluation shows pd P2 to berelatively
small.By accounting
for this and forthermodynamic
identifiesdp/dp
= u and
dpo lap
= uo, u and uostanding
for the volumes ofa
particle
and of amolecule, respectively,
we get from equation(2.4) (PI, ~d, lfl
+~dhl
"(PI, ~2, HI
+ ~2hi
~Ula,
PO
(Pi, ~d,
Hi +godhi
" @o
(Pi, ~d,
Hi +go2hi
~uola,
gj =
~/~
Pi Ii,
Hi, goj =
~/~°
~ji(J,
Hi,
j
=d,
~,hi
«Hi. j~.~~
Further,
the ambient ferrocolloidphase
between thecylinders
is atequilibrium
if the chemicalpotentials
are uniformthroughout
interstices. Hence we arrive at new equationsyielding
necessary conditions of the
equilibrium,
in much the same manner as whengetting equation (2.5),
@(i'l,~2,lfl)+~2/l1"@(Pl,~l,lfl)+U(pl ~P2),
@0
(PI,
~2 HI + ~02hi" @0
(PI,
~l, HI + U0(PI P2) (2.6)
Equations (2.5)
and(2.6) together
with thatdefining
the pressure difference in equation(2.4)
form a set of five equations to determineid, #2,
Pi P2, a andhi
at any fixedii.
Itcan be
solved,
after which all the indicated variables become knownfunctions,
ofii,
within a certain range of the lastquantity
where a solutionexists,
if ever. In such a case, a alsochanges
when
ii
ispermitted
to vary. Theparticle
chemicalpotential
in the interstitial spacedepends only
onii,
Pi and Hi and isindependent
of a, whereas that of theparticles
inside the domainsmay now be
regarded
as a function of a under otherwise identical conditions.The situation is
schematically
illustrated infigure
I. If the domain radius is smaller than al, say, a domain is bound toeventually disappear.
If the radius exceeds another criticalvalue,
a2,the domain also dissolves, but
merely
down to a = a2, when the dissolution ceases. Domains/Ld
lLe '
'
0 al ae a2 a
Fig. I. -Sketch of dependence of particle chemical potential in both domains and interstices on domain radius. Explanations are given in the text.
where radii lie within the range from ai to a2 may either grown but
only
till the value of a2 isreached,
or diminish to a= ai
and,
next, vanish at a =0, depending
on whatphase trajectory corresponds
to a monotonousapproach
of Ad to pi Characteristic trends of thedevelopment
of a
single
domain areconventionally
indicated infigure
I with arrows, from which it is not difficult to see that the domains underquestion
can be stabilizedmerely
at a = a2.Spontaneous
fluctuationalorigination
of new domains resultsinevitably
in a decrease in theparticle
concentration within the interstitial spaceand, consequently,
in a fall of pi This iswhy
the whole system evolution causes a line p= pi = Cte. to come
gradually downward,
until the line touches the curve of p=
pd(a)
at apoint
a = a~ where pi = Ad " @e. The lastequation
determines also a critical concentrationiie
ofparticles
outside the domains. The state thatcorresponds
to this criticalpoint
can be shown to be stable since a further increase in the total amount ofmagnetic particles
within the domains reducesii
belowiie,
and so thewhole line p
= pi = Cte. is
displaced
down with respect to p =pd(a).
Itcompels,
in its turn,an excessive amount of the domain
phase
to dissolveand, thereby,
leads toreestablishing
of the criticalparticle
concentrationspecific
to the stableequilibrium
situation. This concentration has to befound,
incompliance
with the above arguments, from anequation
dpd(a) Ida
= 0.
j2.7)
Equations (2.5)
and(2.6) supplemented
withequation (2.7)
serve now to findid, #2, lie,
pi P2, ae and
hi
In order to close theformulation, however,
we need arelationship defining
Hi in terms of the other variables. An evident relation can be put forward
Ho =
(I s)liHi
+ sld(Hi
+h), (2.8)
in which id is the
magnetic permeability
of thedomains,
the surface(or
volume within thelayer)
domain concentration to be derived from a condition of conservation of the overallnumber of the
magnetic particles
which iscertainly
not affectedby
the domain formation.Hence
s =
~°
~~~,
(2.9) Id lie
where
io
stands for an initialparticle
volume concentration in the same ferrocolloid without domains.Thus all the
equations
necessary to resolve theproblem
are stated.They suffice,
inprinciple,
to determine all
equilibrium properties
of a ferrocolloidlayer
with domains atarbitrary io,
I and Ho Whatsolely
remains to be done in order tobring
theanalysis
to acompletion
consists inspecifying expressions
for bothmagnetostatic properties
and chemicalpotentials
on the basis of some reliable model of ferrocolloids.Judging by
agood agreement
withexperiments,
themodel of
ill]
can besuccessfully
used in such acapacity.
ThenM =
~~
(cth
a(l
+8~fi j)
U ° ° s a ,
~ ~
~~'
°
~~'
'~i~~'
~~'~~~and,
further,
P(P, #, H)
=P° Iv)
+VII, H), PolP, #, H)
=
PilP) lUo/U) Uo(#, H), v(j, H)
=
kT# in # #
in(sh ala)
+#(8 5#)(1 #)-2 jj2 #)GjT, H)j
,
vo(#, H)
=
kT# jji
+#
+ #~#~j (1 #)-3 #GjT, H)j
,
G(T, H)
=
4~t(cth
aila)2
+(4/3)~t2. (2.ii)
Here
p°
andp(
are the standard chemicalpotentials
ofparticles
andmolecules, respectively,
m is the
particle dipole magnetic
moment and kT is the temperature in energy units.Although
the relations inequations (2.10)
and(2.ll)
have beenmeticulously
discussed inill],
it would be worthwhile, perhaps,
togive
a shortexplanation
of theirorigin. Equations (2.10)
were obtained on the basis of an approximate version of the hardsphere perturbation
theory
whichhappened
to describeexperimental
databy
various authors inquite
an excellent way. The second contribution within the brackets inequation (2.10)
is called to allow for an effect of theinterpartide dipole
interaction on theequilibrium magnetization
of a crowdedassemblage
ofmagnetic particles being subject
to a constant externalmagnetic
field. In the dilute limitii
<I),
thisspecific magnetization
turns to thatby Langevin
of an ideal super-paramagnetic
gas. Parameters a and ~f reflect the interaction of theparticles
with the external field and betweenthemselves, respectively.
The sum of the first three addendumda in the expression of u in
equation (2.ll)
presents the chemicalpotential
ofparticles
of an idealparamagnetic
gas in an external field of constantstrength
H. The forth addendum takes into account the steric interaction of hardspheres.
It has been evaluated with thehelp
of the equation of state of a gas of hardspheres suggested by
Carnahan and
Starling
[16]. The fifth addendum takes care of thedipole dipole
interaction between theparticles
in the external field which is estimatedby
means of the methodproposed previously by
Brout [17]. It can be seen,by
the way, that interaction parameter G increases withH,
what is indicative of an intensification of theinterparticle
attraction due to themagnetic
interaction between the
particles
when an externalmagnetic
field is present.Quantity
uo coincide with the pressure of a dense gas of hardmagnetic spheres
evaluated within the frames of the method ofill],
a deviation of the first term within the bracketsfrom
unity being
causedby
the steric component of theinterparticle
interaction, whereas the emergence of the second term is due to thedipole dipole
part of the interaction. It is worthnoting
thatequations (2.10)
and(2.ll)
have been derived in [11]by perturbation theory
methods which
ought
to beadequate
if~fi
is of the order ofunity
or smaller. In anopposite
case of
large ~fi, equations (2.10)
and(2.ll)
have to bethought
of as estimates in an order ofmagnitude
ofthermodynamic properties
of ahighly
concentrated ferrocolloid. Such estimatesare
proved
in[11], nevertheless,
to besufficiently
accurate.Conditions at which the ferrocolloid under consideration loses its
thermodynamic stability
in the bulk and
ought
toundergo phase separation
have also beeninvestigated
inill]
atsome
length
on the basis ofequations (2.10)
and(2.ll).
The same conditionspertain
to a domain arrangementbeginning
to occur in a thinlayer
of the ferrocolloid as well.Equations (2.4)
and(2.5) supplied
with expressions(2.8-2.ll)
make sense, of course, if thepoint
thatspecifies
an actual state of the ferrocolloid in theparametrical
space before separation lies within theinstability region,
thatis,
above thephase diagram
curve obtained in[11],
in whichcase those
equations
can well be solved toyield
all the desiredequilibrium
characteristics of the ferrocolloiddisplaying
the domains.Calculation of dimensionless radius and surface
(volume
concentration of the domains with allowance for formulae(2.10)
and(2.ll)
isquite straightforward,
howevertedious,
and sohardly
merits a detailed discussion. Its results are illustrated infigure
2. The surface tension coefficient has been evaluated with thehelp
of aspecial
modeldeveloped
in [18],according
to which~ ~-
7~ (id Ii
)~u~~/~kT. (2.12)
The radius of stable domains decreases and the concentration of domains increases when either the external field
strength
or theparticle magnetic
moment grows, in a fair agreement with theexperimental
conclusions in [1-6].ae ~e~2
1~3
0.04 0.07 ~ ~~
° l
mHo /kT
0 1mHo /kT
a) b)
Fig. 2. Dependence of dimensionless radius
la)
and of number concentration 16) of domains ondimensionless external magnetic field strength. Figures at curves on b give Values of lo-
3. Ordered arrangements.
Chaotic domain structures
commonly
arise in ferrocolloidlayers
incomparatively
weak or mod-erately
intensivemagnetic
fields. When the fieldstrength increases,
a transition to an orderedhexagonal
arrangement of the domains can beforeseen,
which reminds us, in its outward ap- pearances, of a disorder orderphase
transition. Such a transition has beenactually
observed in [4]. Anelementary
cell of thehexagonal
arrangement is shown infigure
3. Below we aregoing
to demonstrate how the
theory developed
for chaotic structures is to begeneralized
to include ordered structures. It should bepointed
out that experiments of [1-6] confirm the concept of the ordered domain arrangementscorresponding
to aregular hexagonal
two-dimensionallattice.
rc
Fig. 3. Representative cell of hexagonal arrangement.
Particle concentration, pressure and
strength
of the externalmagnetic field, ii,
Pi andHi,
in the interstitial space can be
presented
as Fourier transformations with respect to coordinatesx and y chosen in the
layer plane.
Since the harmonic that possess the symmetry of ahexagonal
lattice understudy
must be of maximal amplitude, we are free to take, as a first approximation,2 2
~bl " ~b~ + ~bk
~
C°S
(~nr),
PI" P~ + ilk
£
CDS
(knr)
,
n=0 n=0
where quantities marked with a
degree
as well asamplitudes
#k, Pk and hk are so far unknown.Let us suppose that
~$~ $ ~$k, P~ $ pk,
lf~
$/lk. (3.2)
The
validity
of these stronginequalities
can be checked later on. It should also be noted that thisassumption
is not ofprincipal significance
and can be avoided at the cost ofmaking
calculation somewhat more cumbersome and
unwieldy.
The chemical
potentials
of bothparticles
and molecules must be uniformthroughout
the interstices.By using equation (3.2)
and all the former considerations we canconsequently
write out
2
p =
p° (p()
+ kTu(#[, Hi
+ kT(upk
+uhhk
+u~#k) £
cos(knr)
= Cte.
n=0
@0 " @(
(P~)
kT (U0IV)
U0($, lf~)
kT (U0IV)
(U0Pk + "0h/lk + "0@~k) X2
x
£
cos
(knr)
=
Cte., (3.3)
n=0
are evaluated at #
= #( and
H=
Upk + Uh/lk + U~~$k
" 0, U0i'k + U0h/lk + U0@~k " 0.
(3.5)
Further,
themagnetic
fieldstrength
at the side surface of a domain can beexpressed
as2
Hs =
H(
+ hk£ cos[a(@)k
cos(@grn/3)], (3.6)
n=0
where is an
angular
coordinate of thecylindrical
coordinate system with anorigin
in thecentre of symmetry and a(@) means the distance from this centre to the domain
boundary
along
the line drawn atangle
@.Dependence
of Hs onthrough
cos(@grn/3)
and a(@) violates thecylindrical
symmetry of any domain in favour of thehexagonal
symmetry, and this fact makes calculationextremely complicated.
In order tosimplify
the matter, in what followswe shall make use of a
quantity
fl
=
H(
+hkf, f
"i~ /~
cos(a(@)k
cos@
~")j do, (3.7)
2gr
_~ o 3
in the
capacity
of an effective fieldstrength
at the domain surface. This amounts toneglect
of deviations of the actual domain form from that of a circularcylinder.
Within the scope of thesame
approximation,
we are now able to use anaveraged
domain radius a instead of a(@). It is worthnoting right
away that ifequation (3.6)
were used but not itsangle-averaged
version(3.7),
we should infer domain cross-sections to behexagonal.
This inference agrees with thefindings
of [4].It has also to be underlined that we have used in the above consideration a conclusion that
hk
is almost normal to thelayer plane,
and thus have not retained vector notation whiledealing
with this and other vector
quantities.
The
period
of thehexagonal
lattice cannotapparently
be smaller than the domain radius(see Fig. 3),
so thatsurely
ak < gr. Thisinequality
becomes stronger when the concentrationdecreases. When
expanding
theintegrands
ofequation (3.7)
into aTaylor
series in powers ofak,
we obtainf
=j§(_1)qc2q (~~)~~ ~~
~f
/~
~~~2q@ ~")
~@j~
~)~
(2q)!
' ~ 2gr~ o 3
q" n=
If a < I, a variation of the field
strength
inside a domain can beneglected,
andfl
ofequation (3.7)
withf
fromequation (3.8)
can be identified with thestrength
of anapproximately
uniformmagnetic
fieldHd
inside the domains.The chemical
potentials
ofparticles
and fluid molecules in the domain interior are now to beexpressed
asAd =
P° lpi
+ ulvd vi
+ kT Ivlid, HI
+ Uhhkii
,
@0d " @~
(P~)
+ U0(PdP~) (U0/U)
~i~("0 (~bd,lf~)
+"0hhkfj (3.9)
By equating
thesepotentials
to those inequation (3.3)
we get in anequilibrium
state, afteraveraging
over the domain sidesurface,
u
(pd PI Pkf)
+ kTiv (id, H[
+uhdhkf]
" kTiv (#[, H[
+uhihkf)
,
U0(Pd P~
Pkf)
(U0IV)
kT (U0(~d, H~)
+"0hd/lkfj
"luo
Iv)
kT lUoIll, HI
+Uohihk ii
13.lo)
Here additional
subscripts
d and I at uh and uohsignify
that the derivatives with respect to H inequations (3A)
have to be estimated at#
=id
and#
=
ii, respectively.
Thus we have arrived at four
equilibrium equations (3.5)
and(3.10)
to beemployed
whendetermining
nine unknown variables:k,
pdPi,
Pk,Hi, hk, Id, Ii, #k
and a. Thephysical meaning
of theseequations
isentirely
similar to that ofequations (2.5)
and(2.6),
so that there is no need to dwell upon it in more detail. It is evident that fivesupplementary equations
must bebrought
into action for the purpose ofcompletely defining
the mentionedvariables,
much in the same way asequations (2.7-2.9)
have been put forward in thepreceding
section.One
supplementary equation immediately
follows from a usual condition of mechanicalequi-
libriumimposed
upon a pressurejump
at the domain surface. We getPd
Pi Pkf
"
ala, (3.ll)
wich is
nothing
more than another representation of the similarequation
inequation (2A).
A
requirement
of conservation of the total number ofmagnetic particles
leads to anequation
s =
jio it) (#d 41)~~
,
13.12)
whose
meaning entirely
coincides with that ofequation (2.9).
On the other
hand,
we can derive an expression for s fromconsidering
the unithexagonal
cell of
figure
3. The whole area that isoccupied by
cross-sections of the central domain and of the other domains with centres at apexes of thehexagon
which fall inside the cellequals
3gra~.It means that s
= 3gra~
IS,
S =(3/fl) r] being
the totalarea of the cell.
By definition,
r~ =
2gr/k
whence s=
(2v5gr)~~ (ak)~. By comparing
this withequation (3.12)
weget
~
~jQ~~~~~
~~~#[ #l'
~~'~~~To derive other relevant
equations,
let us present thespecific magnetization
Md inside a domain in the formMd
(Id, Hi
+hkf)
= M
(id, H[)
+(0M/0Hi) hkf. (3.14)
Now, by using equations (2.1-3.3)
that define the domaindemagnetization field,
we arrive next at a formulahi
=-MdL(r), L(r)
=(~/8) (a~/lr). (3.15)
Furthermore,
the nearestneighbour approximation
appears to beapplicable
since the domain arrangement is two-dimensional. Then the field at the domain surface is a vector sum of the inner fieldHi,
that is directednormally
to thelayer plane,
the own field hi of the domain and a fieldhi
causedby
its nearestneighbours.
It is not difficult to evaluate the latter field in ageneral
case. Within theaccepted
accuracy of theapproximation being used, however,
it suffices toreplace
thestrength
of this fieldby
that of the same field at the symmetry axis of the centraldomain,
that is also normal to thelayer plane
due to symmetry. In this case,h[
=-6MdL (r~), (3.16)
r~
being
identified infigure
3,whence,
with allowance forequation (3.7),
hkf
" -Md[L(a)
+ 6L(r~)]
,
(3.17)
what defines Md in accordance with
equation (3.14)
andleads,
next, to an equation~~f
"l +
(d~/(it )jj~(
6L
jr~)j
~i~~' ~i (~'~~~
A further
equation
is to be deduced from acontinuity
condition of themagnetic
induction at the boundaries of a domain with thelayer plates.
It resemblesequation (2.8)
and is of the formHo
=(I s)liH[
+ sld(Hi
+hi
+hkf)
,
(3.19) hi,
hk andf being
definedby equation (3.15,
3.16 and3.7), respectively.
Thus we have succeeded in
deriving
additional equations which are necessary tosupplement equations (3.5)
and(3.10) stemming
from thethermodynamic equilibrium
conditions. All theseequations
whenbeing
closed with the aid ofequations (2.10)
and(2.ll)
enable us to expressvariables
k,
pdPi,
Pk,H[, hk, Id, Ii
andik
as functions ofaveraged
domain radius a.After
that,
the last variable thatonly
remains unknown can be found without muchado,
fromequation (2.7).
The set of
equations (3.5)
and(3.10-3.19)
can begreatly simplified
in view of the fact thatnormally Ho considerably
exceeds fields causedby
themagnetic particles,
so thatHi
mHo Further,
concentrationsii
andid
may alsojustly
be looked upon asquantities
whichinsignificantly
differ from theirequilibrium
values which have to be established at aplane phase boundary,
thatis,
with no account for the domain side surface curvature.Besides, by
virtue of
f deviating
fromunity only slightly,
it may be takenf
m I. As aresult,
we obtain asimplified
version of theequations
which can be resolved even in ananalytical
form. It is not ourintention, however,
to write out either thesimplified
set or its solution in anexplicit
form because of thembeing
ratherunwieldy.
Suffice it to say that resultsconcerning properties
of equilibrium states withhexagonal
domain arrangements, which can be got from this set whenmaking
use of the equations(2.10)
and(2.ll),
arebasically
of the same kind as those derived in the case of chaotic domain structures.4
Concluding
remarks.Because of a number of
comparatively
boldassumptions
made whileevaluating properties
of theequilibrium
system understudy,
the above results should beultimately regarded
assubstantially approximate, pertaining
to rather a crude attempt totheoretically
describe thoseproperties.
Theassumptions help, nevertheless,
to avoid inessential calculation difficulties andare
surely
not of aprincipal
nature, whereas the said attempt toexplain
the very existence of stable domains in thin ferrocolloidlayers
isseemingly
the first one, not to mention that allthe results can
readily
beimproved
at the expense ofmaking
calculation more tedious. At any rate, these assumptions do not violate in the least theprincipal
conclusions that have to bedrawn from the above treatment.
The main inference consists in that the
phase separation
of a ferrocolloid or of amagnetic
fluid does notnecessarily implies
the terminal occurrence of two massive colloidalphases,
as it iscommonly specific
to most of colloidal systems, but leads toestablishing
a stable state with domains of finite size.Moreover,
this has beenproved
to occur, dueexclusively
to apeculiar scaling
effect that is causedby
the finite distance between thelayer
boundaries. It isjust
this effect that isevidently responsible
for the indicated deviation ofphase separation
patterns in thinlayers
of a ferrocolloid from those observed in unbounded systems.It appears to be
important
forgeneration
of the stable domain arrangements thatgrowing droplets
of the new ferrocolloidalphase
must benoticeably elongated
in the direction normal to thelayer plane.
Thishappens
in a system ofdipole particles
under action of acorresponding
normal external
field,
no matter whether thedipoles
are ofmagnetic
or electricorigin.
Such apoint
of view issurely
confirmedby
the mere fact that stable domain structures establish them- selves notonly
in thinlayers
of ferrocolloids with permanentparticulate magnetic
moments but also inlayers
of electrocolloids whenparticle dipoles
are inducedby
anexternally applied
normal electric field [6]. For the same reasons, the occurrence of similar domain patterns
ought
to be
expected
in various otherdispersions
in whichdipole
interactions prove to besignificant,
such as new ferrosmectics
recently synthesized
in [19]. It should be notedthat,
if thelayer
boundaries are
pliant,
the formation of domains ofparticles
with either permanent or induceddipole
moments have to beaccompanied by
distortions of the form of these boundaries.However, if would be unreasonable
and, perhaps,
somewhat preposterous toenvisage
the emergence of domain arrangements of the discussed type in diverse latexlayers
and in thin colloidal films of differentorigins
in cases when there are noparticulate dipoles.
Domain patterns in suchlayers
andfilms,
if any, arehardy unlikely
to beexplained
on the basis of thesame considerations as those
exploited
above.In
conclusion,
we have toemphasize that,
whilekey
reasons of formation and mainproperties
of both chaotic and ordered domain arrangements can be understood and evaluated with sufficient accuracy, a crucial question ofwhy
and at what exact condition an ordered structuresuddenly replaces
a chaotic one remains obscure.Similarly,
there is no answer to a question:why
the ordered structurecorresponds
to ahexagonal
lattice?This
phenomenon
of disorder-order transition in a two-dimensional system of domains iscertainly
not of the type of aliquid-crystal phase
transition in a system ofattracting
moleculesor
particles.
It is far morelikely
to resemblegeneration
of theparticle packing
with along-
range order in a system of identical hard
spheres
ofhigh
concentration due topurely geometrical
reasons [20]. The
ordering
of the domainsreally
seems to be causedby
domainrepulsion
at acondition of the overall volume accessible to the ferrocolloid under consideration
being
limited.In contrast to
[20], however,
both size and interactionpotential
of the domains that aregoing
fo form an ordered lattice are unknown, and thishampers
to a great extent thedevelopment
of ananalysis
to describe thephenomenon.
It may beexpected,
nonetheless, that a domain structureis
likely
to be chaotic if the mean distance between the symmetry axes of twoneighbouring
domains
happens
toconsiderably
exceed the domaindiameter,
and to be ordered otherwise.References
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1209.Proofnot corrected