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Microscopic theory for the orbital hydrodynamics of

3HeA

R. Combescot

To cite this version:

R. Combescot. Microscopic theory for the orbital hydrodynamics of 3HeA. Journal de Physique

Lettres, Edp sciences, 1980, 41 (9), pp.207-211. �10.1051/jphyslet:01980004109020700�. �jpa-00231761�

(2)

Microscopic

theory

for the

orbital

hydrodynamics

of

3HeA

R. Combescot

Groupe de Physique des Solides de l’Ecole Normale Supérieure (*), 24 rue Lhomond, 75231 Paris 05, France

(Reçu le 18 decembre 1979, revise le 14 février, accepte le 10 mars 1980)

Résumé. 2014

Nous présentons les résultats d’une théorie

microscopique

de la

dynamique

orbitale de la

phase

A de l’hélium 3 en régime linéaire. Des désaccords importants existent avec les résultats de précédentes théories

phénoménologiques,

mais également avec certaines relations de

l’hydrodynamique

formelle. Abstract. 2014 A

microscopic

theory is presented for the orbital dynamics of 3HeA. There are some

significant

disagreements with purely hydrodynamic theories as well as with

phenomenological

approaches. Classification

Physics Abstracts 67.50

Most of the recent interest in

superfluid

3He

has

been focused on the

hydrodynamic properties

of

3HeA.

This is a

fascinating

problem

since

3HeA

is the first

superfluid

to

display

orbital

anisotropy [1].

This

gives

rise to a

great

deal of

interesting properties

linked to the

topological properties

of the order

parameter

[2].

Of main interest has been also the

related

question

of

hydrodynamic stability

of super-flow in

3HeA,

where it appears that

3HeA

could be a rather weak form of

superfluid [3].

In order to treat all these

questions properly,

it is

naturally

useful to

have a full

description

of the

dynamics.

With some

exceptions [4],

all the treatments to date have been static ones, where a

stability analysis

of the

system

has been

performed starting

from the free energy. But in order to know what

happens

in unstable

situations,

the full

hydrodynamics

is

required.

We

will

actually

restrict our scope to the orbital

hydro-dynamics

since

spin dynamics

is well understood. A full set of

equations

for orbital

hydrodynamics

has been derived

by

Graham

[5]

and amended

by

Liu

[6].

These

equations

have the

advantage

of

being

derived on a

rigourous

basis. On the other

hand,

they

introduce many unknown

parameters

and

actually

are difficult to use in detailed calculations. There is therefore a need for a

microscopic

derivation

of these

equations

which would

provide

values for the unknown coefficients.

Although

several

attempts

have been

made,

phenomenological

[7]

or

purely

microscopic [8],

a

satisfactory

derivation does not

exist

[9].

(*) Laboratoire associe au Centre National de la Recherche

Scientifique.

Here we

present

the first

complete microscopic

derivation of orbital

hydrodynamics.

The

resulting

equations

are in

general

agreement

with the Graham-Liu

equations,

and

satisfy

all the relations due to the

no-growth

of the

entropy

by

reactive terms or to

Onsager

relations.

However,

we obtain a non sym-metric stress tensor. Its

expression

agrees with the

general

form

proposed by

Hu and Saslow

[10],

but

not with the relations

they

obtained

by

enforcing

the

angular

momentum conservation law. Our results

disagree

also in some

important

respects

with the

phenomenological

treatments

[7]

on the difficult

points

related to the

angular

momentum conservation law or the

expression

of the stress tensor. Our

equations provide

also, naturally,

a much

simpler

form for the

hydrodynamics

because

they

are

partly

expressed

in terms of the time derivative of the order

parameter,

rather than in terms of the

spatial

derivative.

Finally,

our treatment is restricted to

linear

hydrodynamics

where the order

parameter

has

only

small deviations from a

global equilibrium

value. But it

actually

gives

an

expression

for

basicajly

all the coefficients

coming

into non linear

hydro-dynamics

[10],

since

they

already

appear in linear

hydrodynamics.

A first

point

we want to make is that it is natural to

require

that,

in the limit where the

temperature

T goes to zero, the

hydrodynamics

should reduce to

equations

describing

the motion of the

superfluid

alone.

This

implies

that the normal

velocity

vD should

drop

naturally

out of the

equations.

This is not an

entirely

obvious condition since some

transport

coefficients may

actually

not go to zero because the

relaxation time

diverges

when T -~ 0. But if this time

(3)

L- 208 JOURNAL DE PHYSIQUE - LETTRES is

kept

constant

(which

will

happen

anyway because

of the finite size of the

sample),

the normal

velocity

should

disappear

at T = 0 since it characterizes the

normal

fluid,

and there is no normal fluid at T = 0.

This

property

is satisfied

by

our

equations (this

is

naturally

a result of the

theory,

not an

input).

But it is

not shared

by

some

phenomenological

theories

[7].

It is also in

disagreement

with the term

(1i/4 m) 1.

curl vn

introduced

by

Liu

[6]

in the rate of

change

of the

phase,

since this term does not

disappear

at T = 0

[20].

This term has been derived on the

grounds

that the

characteristic vectors of the A

phase,

Å1

and

A2,

have to follow a solid

body

rotation around an axis

perpendicular

to

Ai

and

A2.

But this

merely

corresponds

to a

change

in the

phase

of the order

parameter and,

as in

superfluid 4He,

the

phase

should not be

directly

coupled

to a rotation of the normal fluid.

This term has also been rederived

[10] by requiring

that the

angular

momentum is conserved. We indeed find an

angular

momentum conservation

law,

by

combining

the

equation

of motion for the

angular

momentum with an intrinsic

angular

momentum

conservation law. But this does not

bring

any further condition on coefficients.

Let us now turn to our results. Our first

equation

is the intrinsic

angular

momentum conservation law which

provides

the

equation

of motion for

1.

Instead of

al/at,

we use the instantaneous rotation

0,

linked to

0110t

by :

allat

= n

x ~

or n =

I

x

allat

since we are interested

only

in the components of n

per-pendicular

to the

equilibrium

1.

We have :

Here

Ls

is the

superfluid

intrinsic

angular

momentum

[11], a

is the orbital

viscosity [12], DEd

is the

dipole

torque

[1]

and

Fi = (2

m/~)

V~[~/’~/~(V/J] =

VjqJij

with Graham’s notations

[5].

f °

is the free energy in the reference frame where the normal

velocity

if is zero.

Explicitly

we have :

where

b2

=

maxk

I A k

12,f’

=

~/7~ where f is

the Fermi

distribution,

r is a relaxation

time,

No

the

density

of

states at the Fermi

surface ; l is

along

the z

axis,

the other notations are standard.

The tensor Cijk has the most

general

form allowed

by

symmetry and is

given

by

[13]

(with

i = x or

y) :

where :

In eq.

(4),

ZJ2

is

always

negligible

and has been

given only

for

consistency.

X(T)

goes to

pn/4 m

when T -~ 0

(p

is the mass

density

and m is the bare mass of

3He).

For T -~

Tc,

in weak

coupling.

The second term in eq.

(3)

is

completely

new. It is the dominant term in Cijk near

T~,

whereas at

low

temperature

the last two terms take over because of the

growth

of the relaxation time

T(T,)

when the

tempe-rature is lowered. In eq.

(3),

the

quantity

b(T)

is

given

by :

This term is non zero

only

because of

particle-hole

asymmetry,

but it is of the same order of

magnitude

as

a(T).

It is difficult to evaluate

precisely

because

No’ EF/No

is not

precisely

known,

though

it is

clearly

of order 1.

How-ever, it behaves like

L(T)

T4

at low

temperature

and is smaller than

a(T)

which goes like

i(T)

T2.

On the other

hand,

b(T) -

(1

-

r/FJ

near

Tc

and dominates over

a(T).

The first and third terms in cijk may

conveniently

be

rearranged

with the first two terms of eq.

(1)

which

can be rewritten as :

(4)

constant, all the terms

containing

VO

drop

out of eq.

(1).

To see this up to order

Z~,

one needs the

precise

expression

for the C tensor

coming [5]

in F. In

particular,

at T =

0,

C 1.

=

p/2

while

CII

= -

p/2

+ 2

mLS/~C.

Now

by inverting-

eq.

(1),

we find an

expression

for

0110t

which is in

complete

agreement with

hydrodynamics

[5].

We obtain for the reactive coefficients :

The result for x~ 2013

a2 is

in agreement with Graham and Pleiner

[14],

and Hu and Saslow

[10].

It is

easily

deduced from eq.

(6).

The

approximation

of

neglecting Ls

is

always

very

good

except

when one looks at the T -~ 0 limit.

Turning

to the

dissipative

coefficients,

we have :

Next we consider the stress tensor. We obtain :

where

c*k

is

given by

eq.

(3)

except

that the

dissipative

terms

(i.e.

the last two

terms)

have their

sign changed ;

qJ is the

phase

of the order

parameter

and we have set :

It is clear from eq.

(9)

that most of the contribution to (Jij is of

dynamical

origin.

-We can see

that,

because of the first term in eq.

(9),

6~~ is not

symmetric,

and therefore the

angular

momentum L = r x g is not

directly

conserved. More

precisely,

we have :

where

cDk

is the

dissipative

part

of ci~k. The first term in the

right-hand

side is the contribution of the

superfluid

intrinsic

angular

momentum to

SL/~

while the other terms are

corresponding

quasi

particles

contributions. Now if we add the intrinsic

angular

momentum conservation law eq.

(1)

to eq.

(11),

we obtain a

good

conservation

law for the

angular

momentum

namely :

where

c~

is the reactive

part

of cijk.

The_stress

tensor eq.

(9)

may be transformed if we use the

equation

[21]

for the

phase

qJ :

where

f (T) = f

(dS~/4 lI) dç( - f ’)

(~/E)2 ,

and

by

=

No

bp

is the fluctuation of the chemical

potential.

From eq.

(13)

we have

[15]

for Graham’s

coefficients (

and

~~~ :

In eq.

(13),

as well as in eq.

(9),

small thermal terms of order

(7~/Fp)~

have been

neglected.

The stress tensor

becomes :

where

v°p9

=

(p2

i/m2

No)

[ f ~i~ ~pg - f ~ f~pg - f p9 8~~

+

~.pj,

the

viscosity

tensor in the absence of

emotion,

has

already

been studied

[16].

We note from eq.

(15)

that vn

drops

out when T goes to zero.

(5)

L- 210 JOURNAL DE PHYSIQUE - LETTRES

To make contact with

hydrodynamics,

we

only

need to

replace

Qk

in eq.

(15) by

its value obtained from eq.

(1).

We first obtain for Uij a contribution :

which agrees

exactly

with the

hydrodynamic

result

[10]. (Note

that it is not

symmetrized.)

Next we have the reactive contribution from

V~ :

where $ =

X(l

+

b/a)

if

Ls

is

neglected

and

Siki

= 4

b~

+

ii

~.

Finally,

for the

dissipative

part, the

anti-symmetric

contribution from

cjj~

Qk

and

V°pq

V pV;

cancel

(at

least in the relaxation time

approximation)

and we

obtain :

-where .ae ~

(x2/a) -

(a

+

b)2/4

a. Therefore (Jij is made of the first and the third terms of eq.

(15), plus

the

contributions

(16), (17)

and

(18).

The reactive and

dissipative

terms

(17)

and

(18)

agree with the

general

form

proposed by

Hu and Saslow

[10],

but not with the restrictions

put

on the reactive coefficients. Indeed we

have,

using

their notations :

Finally

we obtain

[15] :

for the thermal

conductivity

but no term

l

x VT in

the

entropy

current.

Let us now

briefly

[17]

outline the

microscopic

derivation. It is a natural

generalization

of a

previous

treatment for the

homogeneous

case

[11].

We start

with the matrix kinetic

equation

for the

quasi

particle

distribution. Then the motion of the order

parameter

is taken care of

by

a

space-time dependent

rotation,

which allows one to obtain a scalar kinetic

equation

for

Bogoliubov quasi particles.

Collisions are then handled

by

a relaxation time

approximation,

though

exact treatment of the collisions are

naturally possible.

However,

in contrast

to

a first

attempt

[11],

we do not

let the

quasi particles

relax to an

equilibrium

distri-bution with energy shifted

by

the orbital

Josephson

effect - (~/2 E) 11(k

x

Vk9O

(CPk

is the

phase

of the

order

parameter)

because this shift does not

correspond

to a

change

in a conserved

quantity [18] :

the orbital

Josephson

effect is

there,

but

quasi particles

do not relax toward the

corresponding

local

equili-brium. All the

quantities

are then

easily

calculated from their

microscopic expressions.

An

important

point

here is the contribution of the normal

velocity

to the intrinsic

angular

momentum conservation law eq.

(1).

This is most

easily

deduced from Galilean invariance.

But,

contrary

to the

superfluid velocity,

the normal

velocity

does not affect the structure of the

quasi particles

and therefore

only

the contribution

coming

from the

change

in the

quasi particle

distri-bution should be retained.

Acknowledgments.

- Part of this work has been done

during

a very

pleasant

stay at the

University

of

Sussex,

where I benefited from very

stimulating

conversations with A. J.

Leggett.

I am also very

grateful

to C. R. Hu for

stimulating

discussions,

and I thank very much N. B.

Kopnin

and K.

Nagai

for

sending

me

preprints

of their work.

References

[1] For a theoretical review, see LEGGETT, A. J., Rev. Mod. Phys. 47 (1975) 331.

[2] TOULOUSE, G. and KLÉMAN, M., J. Physique Lett. 37 (1976)

L-149.

VOLOVIK, G. E. and MINEEV, V. P., Pis’ma Zh. Eksp. Teor. Fiz. 24 (1976) 605.

[3] BHATTACHARYYA, P., Ho, T.-L. and MERMIN, N. D., Phys. Rev. Lett. 39 (1977) 1290.

FETTER, A. L., Phys. Rev. Lett. 40 (1978) 1656.

KLEINERT, H., LIN-LIU, Y. R. and MAKI, K., Proceedings of LT 15, J. Physique Colloq. 39 (1978) C6-59.

SASLOW, W. M. and Hu, C. R., preprint.

[4] HALL, H. E. and HOOK, J. R., J. Phys. C 10 (1977) L-91.

HOOK, J. R., Proceedings of LT 15, J. Physique Colloq. 39

(1978) C6-17.

(6)

[6] LIU, M., Phys. Rev. B 13 (1976) 4174.

[7] VOLOVIK, G. E. and MINEEV, V. P., Zh. Eksp. Teor. Fiz. 71 (1976) 1129; [Sov. Phys. JETP 44 (1976) 591].

CROSS, M. C., J. Low Temp. Phys. 26 (1977) 165.

[8] KOPNIN, N. B., preprint.

[9] For a review of orbital dynamics, see BRINKHAM, W. F. and CROSS, M. C., to be published in Prog. Low Temp. Phys. [10] Hu, C. R. and SASLOW, W., Phys. Rev. Lett. 38 (1977) 605.

Ho, T.-L., Sanibel Symposium (1977).

LHUILLIER, D., J. Physique Lett. 38 (1977) L-121.

[11] COMBESCOT, R., to be published in Phys. Rev. B.

[12] CROSS, M. C. and ANDERSON, P. W., Proceedings of LT 14,

M. Krusius and M. Vuorio, Eds. (North-Holland,

Amsterdam) 1975.

COMBESCOT, R., Phys. Rev. Lett. 35 (1975) 1646.

[13] The last two terms have been found by Volovik and Mineev in their semi phenomenological approach, and also

proposed by Cross in his phenomenological treatment.

[14] GRAHAM, R. and PLEINER, H., Phys. Rev. Lett. 34 (1975) 792.

[15] This is agreement with Volovik and Mineev (Ref. [7]).

[16] COMBESCOT, R., Phys. Rev. B 12 (1975) 4839.

[17] The details of this derivation will be published elsewhere.

[18] This is also in agreement with a recent treatment of the collision

integral by K. Nagaï (preprint).

[19] They merely relax towards the standard local equilibrium

corresponding to the shifted chemical potential (due to the ordinary Josephson effect), the normal velocity and the shifted temperature. These correspond to the

conser-vation of particle number, momentum and energy. On the other hand, it is easy to check that a quasi particle

distribution shifted by the orbital Josephson effect

03B4vk = f’ x (2014 03BE/2 E) 03A9. k x ~k~k does not correspond

to a change in particle number, momentum or energy

because of its symmetries. Therefore, nothing of it can

survive collisions.

[20] Since the time of this writing, things have somewhat evolved. We have shown (R. Combescot and T. Dombre, to be

published) that one has to modify non linear

hydrodyna-mics [10], by considering an additional term in the current. At T = 0, this term is - (0127/4

m) 013E

x Vp. This produces

a contribution in 03BC which cancels exactly the

(0127/4 m) 013E.curl vn term. This brings non linear

hydro-dynamics in agreement with the present theory at T = 0

with respect to this term.

[21] There is a disagreement on this equation with a paper on the

same problem by Nagai (to be published). Though both theories agree that vn disappears at T = 0, Nagai finds

an additional term (0127/4 m) Y(T) 013E.curl vn where Y(T)

is the Yoshida function. Since the methods are rather different, it is difficult to know the origin of the disagree-ment. But it is probably not superficial and is rather linked to the approximations made in the theories. It is worthwhile noting that the term in question is

quantitati-vely very small anyway, though it is important for the

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