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Decoupled-mode dynamical scaling theory of the ferromagnetic phase transition
Richard A. Ferrell
To cite this version:
Richard A. Ferrell. Decoupled-mode dynamical scaling theory of the ferromagnetic phase transition.
Journal de Physique, 1971, 32 (1), pp.85-88. �10.1051/jphys:0197100320108500�. �jpa-00207027�
DECOUPLED-MODE DYNAMICAL SCALING THEORY
OF THE FERROMAGNETIC PHASE TRANSITION (*)
Richard A. FERRELL
University
ofMaryland, College Park, Maryland (Reçu
le 14septembre 1970)
Résumé. - Le calcul du comportement critique de la diffusion de spin s’effectue par applica-
tion simple de la formule de Kubo. Une approximation de découplage permet l’évaluation de la fonction de corrélation pour le courant de spin, ce qui amène à des résultats identiques à ceux de
Résibois et Piette, obtenus par une autre méthode.
Abstract. - The dynamical scaling theory of phase transitions begins below the phase transi-
tion and extrapolates the frequencies, by means of the temperature continuity at a finite wave number, through the critical point into the temperature region above the transition. Applied to
the ferromagnet, this approach leads to the observed five-halves critical dispersion at the Curie point. In the paramagnetic region it yields the critical slowing down of spin diffusion with a critical exponent of one-third. An alternative approach beginning in the paramagnetic region has been developed from the basic statistical mechanics of spin interaction. In the present paper, we present
a simplified version of this approach, based on the fluctuation-dissipation theorem. The relevant form of this theorem is easily derived along familiar lines and involves obtaining an expression for
the spin current. The spin diffusi on coefficient is then expressed in terms of the ratio of the fluctuations in spin current aud spin density. The correlation function for the current fluctuations
can be evaluated by factoring (decoupled-mode approximation). The results are shown to be equi-
valent of those obtained by the other methods, and a simple explanation is given for the rise of the
scaling function outside of the hydrodynamic region.
1. Introduction. - The
theory of dynamical scaling [1]
of
phase
transitions is based on the observation that any critical temperaturedependence
can beexpressed
as a function of the correlationlength K-1.
When x-1 becomes greater than a
particular
wave-length
underConsideration,
sayk-l, K
is to bereplaced by
k. In this way, forexample,
the temperature-dependent
lineardispersion
relation for second sound insuperfluid helium,
(Ok oc(T¡ - T)1’3 k,
becomes at thelambda
point,
T =TÂ,
the criticaldispersion
rela-tion wk
ock3’2. Similarly, Halperin
andHohenberg [2]
have
applied
the same idea to theantiferromagnet,
with the same critical
dispersion
relationensuing
asin
superfluid
helium. In a furtherapplication,
thepresent author
[3]
has noted that úJk ock 5/2
should beexpected
for the criticaldispersion
relation of anisotropic ferromagnet.
All of the above treatments
begin
with the orderedphase
of broken symmetry, at temperatures below the critical temperature, and are based upon know-ledge (by
means ofhydrodynamics
or a sumrule)
of the temperaturedependence
of the collective modes(*) Research supported in part by the National Science Foun- dation, The Office of Naval Research, and the Air Force Office of Scientific Research. Paper presented at the International Conference on Magnetism, Grenoble, September 1970.
associated with the broken symmetry. Such modes do
not exist in the fluid systems where there has been
developed
a method referred toalternatively
as« mode-mode »
[4, 5]
and as« decoupled-mode theory » [6].
This method can beapplied
to tempera- tures above the criticalpoint,
which makes it moredirect if this is the
region
of interest. A further advan- tage is that itprovides
a detailed account of howK-1
becomesreplaced by
k-l as it becomes greater thanK-’.
Calculations of the « mode-modecoupling »
type have also been carried outby
Résibois and co-workers
[7, 8]
andby Wegner [9]
onmagnetic
systems.The purpose of the present paper is to demonstrate how the same results for the
ferromagnet
can be obtained in thedecoupled-mode theory,
as well as topresent a
simple physical interpretation
of the main feature of the results.The
decoupled-mode dynamical scaling theory
ismost
straightforward
for a system in which the order parameter isconserved,
as is the case in the ferroma- gnet. The relaxation of the order parameter is then studiedby considering
the current which is associatedwith the order parameter
by
theequation
of conti-nuity.
The form of the current isreadily
determinedin each individual case. A
simple physical
argument suffices for theferromagnet.
Consider twospins S(1)
and
S(2)
at twopoints
1 and2, interacting by
theArticle published online by EDP Sciences and available at http://dx.doi.org/10.1051/jphys:0197100320108500
86
Heisenberg
energyS(1).S(2).
The torque exertedby S(2)
onS(1) clearly only depends
upon theirdifference,
and isproportional
to the vector crossproduct
This torque can be
regarded
as a flow ofangular
momentum from one of the
spins
to the other. Nowpassing
to the continuumpicture,
wereplace
Sby
the
spin density
m, and the finite differenceby
thegradient.
Thus we find for the currentdensity
ofspin flowing
across a surfaceperpendicular
to, say, a cartesian axis « z »,az
is the z-component of thegradient
operator and C is a materials constantdepending
upon thestrength
and range of the
Heisenberg interaction,
as well ason the
density
ofspins.
It iseasily
verified that eq.(1),
when substituted into the
equation
ofcontinuity
is
equivalent (in fact, identical)
to theequation
ofmotion for m. Because of the
isotropy,
it suflices tostudy
one Cartesian component ofJz,
which wewrite as
J3,. (In
order to avoid confusion in the nota-tion,
we use differentsubscripts
fordenoting
thedirections of
spin
and direction offlow.)
In terms ofthe Cartesian components of m this becomes
Eq. (3)
can beemployed
to determine the relaxation rate of thespin fluctuations, by
means of thespin conductivity
À. This transport coefficient expresses thesteady-state spin
current which flows in the pre-sence of a
gradient
of externalmagnetic
field. It isgiven by
the Kubo formula[10, 11 ]
where the
angular
bracketssignify
the thermalequili-
brium average of the
product
of the current at thearbitrary space-time points
2 and 1.Eq. (4)
is arigorous expression
for theconductivity
whichis, however, impossible
to evaluate without the intro- duction of someapproximations.
The mostimportant
of these is the
decoupling approximation
describedimmediately
in the next section. The remainder of Section II is devoted toexhibiting
the two successfulpredictions
of thedynamical scaling theory ;
i. e.the critical five-halves
dispersion
relation and the one-third-power
temperaturedependehce
of the diffusion coefficient. Section III discusses some of the aspects of the more detailed results which can be obtained from thedecoupled-mode theory.
Here we also presenta
general physical
argumentpertinent
to the numerical coefficient which relates thedynamical
behavior atk/K
= 0 to that atk/x
= oo.Finally,
Section IVconstitutes a brief summary.
II.
Dynamical scaling.
- The substitutionof eq. (3)
into eq.
(4)
leads towhere we have introduced
the time-dependent
order parameter correlation functionThe last line of eq.
(5)
is obtainedby
adecoupling approximation,
where wereplace
the average of theproduct
ôf fourmagnetizations by
theproduct
of twoaverages, each of the form of eq.
(6).
Thedecay
rateof a fluctuation of wave number k is
generally (for
anisotropic ferromagnet
in which there is aspin
conser-vation
law)
where the critical
slowing
down of thespin
diffusioncan be
expressed by
The unknown exponent x is to be determined self-
consistently,
as well as thescaling
functionQ(x).
This function is normalized in the
hydrodynamic
limit x = 0
by 0’(0)
= 1 and represents for other values of its argument a numerical correction to thequalitative
rule that x is to bereplaced by
k in thenon-hydrodynamic
limit ofklic -->
oo.For the
qualitative
purposes of this section we canset
0’(0)
=1,
and use the Ornstein-Zernike form for theequal-time
correlationfunction,
Substitution of eq.
(7), (8),
and(9)
into eq.(5) gives
The Kubo formula is
easily generalized
togive
a wavenumber
dependent conductivity, by simply including
a factor exp
ikz21
in theintegrand
of eq.(5). Eq. (10)
then also
applies
in thenon-hydrodynamic region by replacing
Kby k,
so that in the twolimiting
caseswe find
To determine the unknown critical index x it suffices to
study
thelimiting
casek/x
= oo.Requiring
that eq.
(11)
in this case should lead to a diffusion coefficient in agreement with eq.(8),
andrecalling
that the wave number
dependent susceptibility x(k)
is
proportional
to the correlation functiong(k),
weobtain
from which it follows that
Substitution of this value back into eq.
(8) gives
inthe two
limits,
with the aid of eq.(9)
In the
hydrodynamic limit,
if the critical exponent for the correlationlength
is v =2/3,
we haveD(o)
oc(T - Tc)1’3
-- a criticalslowing
down ofspin
diffusion which differsmarkedly
from thepredic-
tion of mean fieldtheory.
In the other limitof klK
= oowe have the critical
dispersion
relationIII.
Scaling
function. - The discussion in thepreceding
section has concentrated on the behavior of thespin
relaxationalong
the two linesk/x
= 0and
k/x
= oo. This behavior has been studiedquali- tatively, neglecting
numerical constants. But all of the aboveequations
which have been put into the form ofproportionality relationships
can as well be writtenas direct
equalities, retaining
all of the numerical factors. It is astraightforward
task to carry this out.Retaining
alsou(klk)
andwriting
eq.(5)
for anarbitrary
valueof k/K,
we arrive at anintegral equation
identical to that solved
numerically by
iterationby
Résibois and Piette
[8].
The solution of thisintegral equation
determines the numerical coefficients of eq.(14)
notonly along
the lines of the twolimiting
cases k/x = 0 and oo, but also
along
a line ofarbitrary
value of
kjx.
The variation of the coefficient as afunction of
k/x
isexpressed by Q(k/x).
The results of Résibois and Piette[8]
have beenreplotted
in thisform and are exhibited
by
the curve R-P infigure
1.It should be noted that this curve is
completely
monotonic and rises
smoothly
fromo-(o)
= 1 to itsasymptotic
valueo-(oo)
= 2.3. Theoriginal
presenta- tionby
Résibois and Piette[8]
of their results exhibitsa
minimum,
but it is clear from the present alternative mode ofpresentation
that this minimum has nophy-
sical
significance.
On the other
hand,
the considerable rise ofQ(x)
toits
asymptotic
value can be understood on the basis of asimple physical
argument. But beforeexplaining
this argument it may be useful to report the numerical results in a
different,
butmathematically
similarproblem
in criticalphenomena.
This is thephenome-
non of
paraconductivity,
or the onset ofsuperconduc-
FIG. 1. - Three different scaling functions dx) vs. x = k/K,
the ratio of wave number to inverse correlation length, illus- trating the qualitative validity of the rule of thumb concerning the rise of u(x) outside the hydrodynamic region x « 1. Curve
« L » illustrates the diffusion in a binary liquid, where practi- cally no rise is expected, while a strong rise is expected for
curves « Q » and « R-P ». « Q » corresponds to the Fourier transform of the square of the Orstein-Zernike function, while
« R-P » exhibits the numerical results obtained by Résibois and Piette (reference 8) for the isotropic ferromagnet.
tivity
above thesuperconducting
transition[12, 13, 14].
Just as in the present
problem
ofspin conductivity,
the electrical
conductivity
can be calculatedby
theKubo
formula, using
thefactoring approximation.
The behavior of the
conductivity
in the two limitsis
easily
shown to beThis can be written in more
precise
form aswhere
Co
is a certain numerical constant and thescaling
function for thesuperconductor
is normalizedby u s( 0)
= 1. Theintegration
can be carried out inclosed form
[15]
and exhibits a monotonic rise inus(x),
with theasymptotic
valueThe exact coincidence of this value with the Résibois- Piette
[8]
value for theferromagnet
ofu(oo)
= 2.3is,
of course,nothing
other than a numerical accident.The strong rise in both
scaling
functionsis,
however,a
qualitative
feature which we believe to be common toproblems
of this type.The
general
feature is the factor ofg(k)2
which hasentered the
integrand
of eq.(5)
as a result of thedecoupling approximation.
This factor tends todominate in
integrals
of this type, andcorresponds
tothe square of the Ornstein-Zernike correlation function
88
We now note that the correlation
length
enters theproblem only through
thequantity
2 K. Thus itis,
as a
rough
ruleof thumb,
2 x and notsimply K
which weshould
expect to be replaced
in thenon-hydrodynamic limit by k
forexample,
in thesuperconducting problem
where in thehydrodynamic
limitÂs(O)
=Co K-1,
we should substitute K
k j2
and obtainThis would lead to the result
Os(oo)
=2.0,
not far fromthe exact value 2.3
quoted
above.Similarly,
in thehydrodynamic
limit of theferromagnet according
to eq.
(11)
and(13), Ào
ocK-3/2. Again using
the ruleof thumb K -->
k/2,
we find in this caseagain
notseriously
removed from the correct valueof 2.3.
Clearly
thisrough
rule of thumb can beexpected
to
give only
a crude indication of the trend of thescaling
functionQ(x).
But we do believe that it isqualitatively
correct and that it doesexplain why u(x)
has to increase as x increases. A measure of the error
in the rule of thumb is
given by
the Fourier transform of the square of the Ornstein-Zernike functionwhere we have introduced the
scaling
functionThis function is
plotted
infigure
1 as curve« Q ».
We note that the
asymptotic
value isQQ(oo) = n
so that the rulc of thumb underestimates the rise
by
the factor
2/n,
or 38%.
A further test of the rule of thumb is found in the criticalslowing
down in abinary liquid,
where one of the modes in the decou-pling approximation
is the non-critical shear mode.Thus
G(r) only
appears once in theintegrand,
so thatthe rule of thumb would
require replacing
xby k,
without the factor of two. In otherwords,
we would expectO’L( (0)
= 1.0. The actualscaling
function isplotted
as curve « L » infigure
1. Theasymptotic
value in this case is
1.18,
so the rule of thumb under- estimates the rise in this caseby
15%, [5, 6].
These
examples
demonstrate that the rule of thumbpresented
here can in no way be used to obtainprecise
numerical results for the
scaling
function. But it canbe
expected
to serve as a usefulqualitative guide.
In
particular,
itexplains
the strong rise in thescaling function,
which is theprincipal qualitative
feature ofthe Résibois-Piette
[8]
calculations.IV.
Summary. -
In summary, we have shown how thestudy
of the fluctuations in thespin
currentand the use of the Kubo formula
permits
thetheory
of
dynamical scaling
to be put into aparticularly
sim-ple
and transparent form. We have furthermore noteda
rough
rule of thumb whichexplains qualitatively
the rise in the
scaling
function outside thehydrody-
namic
region.
The interested reader is referred to the literature for further discussion of thetheory [16]
as well as for a survey of the
experiment
status of thesubject [17, 18].
References
[1] FERRELL (R. A.), MÉNYHARD (N.), SCHMIDT (H.), SCHWABL (F.) and SZÉPFALUSY (P.), Phys. Rev.
Letters, 1967, 18, 891 ; Phys. Letters, 1967, 24A, 493, and Ann. Phys. (N. Y.), 1968, 47, 565.
[2] HALPERIN (B. I.) and HOHENBERG (P. C.), Phys. Rev.
Letters, 1967, 19, 700, and Phys. Rev., 1969, 177,
952.
[3] FERRELL (R. A.), « Field Theory of Phase Transitions »,
International Symposium on Contemporary Phy- sics, Trieste, 1, 129, IAEA, Vienna, 1969. Uni-
versity of Maryland Department of Physics and Astronomy Technical Report n° 848
(July
1968).See bibliography for other work in the field.
Proc. of the Eleventh Intern. Conf. on Low Tem- perature Physics, University of St Andrews Prin- ting Department, 1968, p. 27.
[4] SWIFT
(J.)
and KADANOFF (L. P.), Ann. Phys.(N.
Y.), 1968, 50, 312; KADANOFF (L. P.) and SWIFT (J.), Phys. Rev., 1968, 166, 89. See also FIXMAN(M.),
J. Chem. Phys., 1967, 47, 2808.
[5] KAWASAKI (K.), to be published, and Phys. Letters, 1969, 30A, 325.
[6] FERRELL
(R.
A.), Physical Review Letters, 1970, 24, 1169.[7]
RÉSIBOIS (P.)
and DE LEENER (M.), Physics Letters, 1967, 25A, 65.[8] RÉSIBOIS
(P.)
and PIETTE(C.),
Phys. Rev. Letters 1970, 24, 514.[9] WEGNER
(F.),
Zeitschrift fur Physik, 1968, 216, 433 ; 1969, 218, 260.[10] CALLEN
(H.)
and WELTON (T.), Phys. Rev., 1951, 83, 34. KUBO (R.), J. Phys. Soc. Japan, 1957, 12, 570; Lectures in Theoretical Physics, Vol. 1(Interscience,
New York, 1959), ch. 4.[11] ZWANZIG
(R.),
Ann. Rev. Phys. Chem., 1965, 16, 67.[12] FERRELL (R. A.), J. Low Temp. Phys., 1969, 1, 241.
[13] SCHMIDT
(H.),
Z. Physik, 1968, 216, 336.[14] ASLAMAZOV (L. G.) and LARKIN (A. I.), Phys. Letters, 1968, 26A, 238.
[15] CYROT
(M.)
and FERRELL(R.),
Jour. of Low Temp.Physics (to be
published).
[16] FERRELL
(R.),
« Decoupled-ModeDynamical
Scaling Theory of Phase Transitions », Univ. of Md.Department of Physics and Astronomy Techni- cal Report n° 71-005
(July,
1970) and Procee-dings of a Conference on Dynamics of Critical Phenomena, Fordham Univ., New York, June 1970, Editor J. Budnick.
[17] COLLINS
(M.
F.), MINKIEWICZ (V. J.), NATHANS(R.),
PASSELL (L.) and SHIRANE
(G:),
Phys. Rev., 1969,179, 417.
[18] ALS-NIELSEN (J.), BNL preprint 14783 and Phys.
Rev. Letters (to be published).