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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�

(2)

DECOUPLED-MODE DYNAMICAL SCALING THEORY

OF THE FERROMAGNETIC PHASE TRANSITION (*)

Richard A. FERRELL

University

of

Maryland, College Park, Maryland (Reçu

le 14

septembre 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 temperature

dependence

can be

expressed

as a function of the correlation

length K-1.

When x-1 becomes greater than a

particular

wave-

length

under

Consideration,

say

k-l, K

is to be

replaced by

k. In this way, for

example,

the temperature-

dependent

linear

dispersion

relation for second sound in

superfluid helium,

(Ok oc

(T¡ - T)1’3 k,

becomes at the

lambda

point,

T =

TÂ,

the critical

dispersion

rela-

tion wk

oc

k3’2. Similarly, Halperin

and

Hohenberg [2]

have

applied

the same idea to the

antiferromagnet,

with the same critical

dispersion

relation

ensuing

as

in

superfluid

helium. In a further

application,

the

present author

[3]

has noted that úJk oc

k 5/2

should be

expected

for the critical

dispersion

relation of an

isotropic ferromagnet.

All of the above treatments

begin

with the ordered

phase

of broken symmetry, at temperatures below the critical temperature, and are based upon know-

ledge (by

means of

hydrodynamics

or a sum

rule)

of the temperature

dependence

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 to

alternatively

as

« mode-mode »

[4, 5]

and as

« decoupled-mode theory » [6].

This method can be

applied

to tempera- tures above the critical

point,

which makes it more

direct if this is the

region

of interest. A further advan- tage is that it

provides

a detailed account of how

K-1

becomes

replaced by

k-l as it becomes greater than

K-’.

Calculations of the « mode-mode

coupling »

type have also been carried out

by

Résibois and co-

workers

[7, 8]

and

by Wegner [9]

on

magnetic

systems.

The purpose of the present paper is to demonstrate how the same results for the

ferromagnet

can be obtained in the

decoupled-mode theory,

as well as to

present a

simple physical interpretation

of the main feature of the results.

The

decoupled-mode dynamical scaling theory

is

most

straightforward

for a system in which the order parameter is

conserved,

as is the case in the ferroma- gnet. The relaxation of the order parameter is then studied

by considering

the current which is associated

with the order parameter

by

the

equation

of conti-

nuity.

The form of the current is

readily

determined

in each individual case. A

simple physical

argument suffices for the

ferromagnet.

Consider two

spins S(1)

and

S(2)

at two

points

1 and

2, interacting by

the

Article published online by EDP Sciences and available at http://dx.doi.org/10.1051/jphys:0197100320108500

(3)

86

Heisenberg

energy

S(1).S(2).

The torque exerted

by S(2)

on

S(1) clearly only depends

upon their

difference,

and is

proportional

to the vector cross

product

This torque can be

regarded

as a flow of

angular

momentum from one of the

spins

to the other. Now

passing

to the continuum

picture,

we

replace

S

by

the

spin density

m, and the finite difference

by

the

gradient.

Thus we find for the current

density

of

spin flowing

across a surface

perpendicular

to, say, a cartesian axis « z »,

az

is the z-component of the

gradient

operator and C is a materials constant

depending

upon the

strength

and range of the

Heisenberg interaction,

as well as

on the

density

of

spins.

It is

easily

verified that eq.

(1),

when substituted into the

equation

of

continuity

is

equivalent (in fact, identical)

to the

equation

of

motion for m. Because of the

isotropy,

it suflices to

study

one Cartesian component of

Jz,

which we

write as

J3,. (In

order to avoid confusion in the nota-

tion,

we use different

subscripts

for

denoting

the

directions of

spin

and direction of

flow.)

In terms of

the Cartesian components of m this becomes

Eq. (3)

can be

employed

to determine the relaxation rate of the

spin fluctuations, by

means of the

spin conductivity

À. This transport coefficient expresses the

steady-state spin

current which flows in the pre-

sence of a

gradient

of external

magnetic

field. It is

given by

the Kubo formula

[10, 11 ]

where the

angular

brackets

signify

the thermal

equili-

brium average of the

product

of the current at the

arbitrary space-time points

2 and 1.

Eq. (4)

is a

rigorous expression

for the

conductivity

which

is, however, impossible

to evaluate without the intro- duction of some

approximations.

The most

important

of these is the

decoupling approximation

described

immediately

in the next section. The remainder of Section II is devoted to

exhibiting

the two successful

predictions

of the

dynamical scaling theory ;

i. e.

the critical five-halves

dispersion

relation and the one-

third-power

temperature

dependehce

of the diffusion coefficient. Section III discusses some of the aspects of the more detailed results which can be obtained from the

decoupled-mode theory.

Here we also present

a

general physical

argument

pertinent

to the numerical coefficient which relates the

dynamical

behavior at

k/K

= 0 to that at

k/x

= oo.

Finally,

Section IV

constitutes a brief summary.

II.

Dynamical scaling.

- The substitution

of eq. (3)

into eq.

(4)

leads to

where we have introduced

the time-dependent

order parameter correlation function

The last line of eq.

(5)

is obtained

by

a

decoupling approximation,

where we

replace

the average of the

product

ôf four

magnetizations by

the

product

of two

averages, each of the form of eq.

(6).

The

decay

rate

of a fluctuation of wave number k is

generally (for

an

isotropic ferromagnet

in which there is a

spin

conser-

vation

law)

where the critical

slowing

down of the

spin

diffusion

can be

expressed by

The unknown exponent x is to be determined self-

consistently,

as well as the

scaling

function

Q(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 the

qualitative

rule that x is to be

replaced by

k in the

non-hydrodynamic

limit of

klic -->

oo.

For the

qualitative

purposes of this section we can

set

0’(0)

=

1,

and use the Ornstein-Zernike form for the

equal-time

correlation

function,

Substitution of eq.

(7), (8),

and

(9)

into eq.

(5) gives

The Kubo formula is

easily generalized

to

give

a wave

number

dependent conductivity, by simply including

a factor exp

ikz21

in the

integrand

of eq.

(5). Eq. (10)

then also

applies

in the

non-hydrodynamic region by replacing

K

by k,

so that in the two

limiting

cases

we find

To determine the unknown critical index x it suffices to

study

the

limiting

case

k/x

= oo.

Requiring

that eq.

(11)

in this case should lead to a diffusion coefficient in agreement with eq.

(8),

and

recalling

(4)

that the wave number

dependent susceptibility x(k)

is

proportional

to the correlation function

g(k),

we

obtain

from which it follows that

Substitution of this value back into eq.

(8) gives

in

the two

limits,

with the aid of eq.

(9)

In the

hydrodynamic limit,

if the critical exponent for the correlation

length

is v =

2/3,

we have

D(o)

oc

(T - Tc)1’3

-- a critical

slowing

down of

spin

diffusion which differs

markedly

from the

predic-

tion of mean field

theory.

In the other limit

of klK

= oo

we have the critical

dispersion

relation

III.

Scaling

function. - The discussion in the

preceding

section has concentrated on the behavior of the

spin

relaxation

along

the two lines

k/x

= 0

and

k/x

= oo. This behavior has been studied

quali- tatively, neglecting

numerical constants. But all of the above

equations

which have been put into the form of

proportionality relationships

can as well be written

as direct

equalities, retaining

all of the numerical factors. It is a

straightforward

task to carry this out.

Retaining

also

u(klk)

and

writing

eq.

(5)

for an

arbitrary

value

of k/K,

we arrive at an

integral equation

identical to that solved

numerically by

iteration

by

Résibois and Piette

[8].

The solution of this

integral equation

determines the numerical coefficients of eq.

(14)

not

only along

the lines of the two

limiting

cases k/x = 0 and oo, but also

along

a line of

arbitrary

value of

kjx.

The variation of the coefficient as a

function of

k/x

is

expressed by Q(k/x).

The results of Résibois and Piette

[8]

have been

replotted

in this

form and are exhibited

by

the curve R-P in

figure

1.

It should be noted that this curve is

completely

monotonic and rises

smoothly

from

o-(o)

= 1 to its

asymptotic

value

o-(oo)

= 2.3. The

original

presenta- tion

by

Résibois and Piette

[8]

of their results exhibits

a

minimum,

but it is clear from the present alternative mode of

presentation

that this minimum has no

phy-

sical

significance.

On the other

hand,

the considerable rise of

Q(x)

to

its

asymptotic

value can be understood on the basis of a

simple physical

argument. But before

explaining

this argument it may be useful to report the numerical results in a

different,

but

mathematically

similar

problem

in critical

phenomena.

This is the

phenome-

non of

paraconductivity,

or the onset of

superconduc-

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 the

superconducting

transition

[12, 13, 14].

Just as in the present

problem

of

spin conductivity,

the electrical

conductivity

can be calculated

by

the

Kubo

formula, using

the

factoring approximation.

The behavior of the

conductivity

in the two limits

is

easily

shown to be

This can be written in more

precise

form as

where

Co

is a certain numerical constant and the

scaling

function for the

superconductor

is normalized

by u s( 0)

= 1. The

integration

can be carried out in

closed form

[15]

and exhibits a monotonic rise in

us(x),

with the

asymptotic

value

The exact coincidence of this value with the Résibois- Piette

[8]

value for the

ferromagnet

of

u(oo)

= 2.3

is,

of course,

nothing

other than a numerical accident.

The strong rise in both

scaling

functions

is,

however,

a

qualitative

feature which we believe to be common to

problems

of this type.

The

general

feature is the factor of

g(k)2

which has

entered the

integrand

of eq.

(5)

as a result of the

decoupling approximation.

This factor tends to

dominate in

integrals

of this type, and

corresponds

to

the square of the Ornstein-Zernike correlation function

(5)

88

We now note that the correlation

length

enters the

problem only through

the

quantity

2 K. Thus it

is,

as a

rough

rule

of thumb,

2 x and not

simply K

which we

should

expect to be replaced

in the

non-hydrodynamic limit by k

for

example,

in the

superconducting problem

where in the

hydrodynamic

limit

Âs(O)

=

Co K-1,

we should substitute K

k j2

and obtain

This would lead to the result

Os(oo)

=

2.0,

not far from

the exact value 2.3

quoted

above.

Similarly,

in the

hydrodynamic

limit of the

ferromagnet according

to eq.

(11)

and

(13), Ào

oc

K-3/2. Again using

the rule

of thumb K -->

k/2,

we find in this case

again

not

seriously

removed from the correct value

of 2.3.

Clearly

this

rough

rule of thumb can be

expected

to

give only

a crude indication of the trend of the

scaling

function

Q(x).

But we do believe that it is

qualitatively

correct and that it does

explain 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 function

where we have introduced the

scaling

function

This function is

plotted

in

figure

1 as curve

« Q ».

We note that the

asymptotic

value is

QQ(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 critical

slowing

down in a

binary liquid,

where one of the modes in the decou-

pling approximation

is the non-critical shear mode.

Thus

G(r) only

appears once in the

integrand,

so that

the rule of thumb would

require replacing

x

by k,

without the factor of two. In other

words,

we would expect

O’L( (0)

= 1.0. The actual

scaling

function is

plotted

as curve « L » in

figure

1. The

asymptotic

value in this case is

1.18,

so the rule of thumb under- estimates the rise in this case

by

15

%, [5, 6].

These

examples

demonstrate that the rule of thumb

presented

here can in no way be used to obtain

precise

numerical results for the

scaling

function. But it can

be

expected

to serve as a useful

qualitative guide.

In

particular,

it

explains

the strong rise in the

scaling function,

which is the

principal qualitative

feature of

the Résibois-Piette

[8]

calculations.

IV.

Summary. -

In summary, we have shown how the

study

of the fluctuations in the

spin

current

and the use of the Kubo formula

permits

the

theory

of

dynamical scaling

to be put into a

particularly

sim-

ple

and transparent form. We have furthermore noted

a

rough

rule of thumb which

explains qualitatively

the rise in the

scaling

function outside the

hydrody-

namic

region.

The interested reader is referred to the literature for further discussion of the

theory [16]

as well as for a survey of the

experiment

status of the

subject [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 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-Mode

Dynamical

Scaling Theory of Phase Transitions », Univ. of Md.

Department of Physics and Astronomy Techni- cal Report 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).

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