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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�
Microscopic
theory
for the
orbital
hydrodynamics
of
3HeA
R. CombescotGroupe 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 ladynamique
orbitale de laphase
A de l’hélium 3 en régime linéaire. Des désaccords importants existent avec les résultats de précédentes théoriesphénoménologiques,
mais également avec certaines relations del’hydrodynamique
formelle. Abstract. 2014 Amicroscopic
theory is presented for the orbital dynamics of 3HeA. There are somesignificant
disagreements with purely hydrodynamic theories as well as with
phenomenological
approaches. ClassificationPhysics Abstracts 67.50
Most of the recent interest in
superfluid
3He
hasbeen focused on the
hydrodynamic properties
of3HeA.
This is afascinating
problem
since3HeA
is the first
superfluid
todisplay
orbitalanisotropy [1].
This
gives
rise to agreat
deal ofinteresting properties
linked to the
topological properties
of the orderparameter
[2].
Of main interest has been also therelated
question
ofhydrodynamic stability
of super-flow in3HeA,
where it appears that3HeA
could be a rather weak form ofsuperfluid [3].
In order to treat all thesequestions properly,
it isnaturally
useful tohave a full
description
of thedynamics.
With someexceptions [4],
all the treatments to date have been static ones, where astability analysis
of thesystem
has beenperformed starting
from the free energy. But in order to know whathappens
in unstablesituations,
the fullhydrodynamics
isrequired.
Wewill
actually
restrict our scope to the orbitalhydro-dynamics
sincespin dynamics
is well understood. A full set ofequations
for orbitalhydrodynamics
has been derivedby
Graham[5]
and amendedby
Liu[6].
Theseequations
have theadvantage
ofbeing
derived on arigourous
basis. On the otherhand,
they
introduce many unknownparameters
andactually
are difficult to use in detailed calculations. There is therefore a need for amicroscopic
derivationof these
equations
which wouldprovide
values for the unknown coefficients.Although
severalattempts
have been
made,
phenomenological
[7]
orpurely
microscopic [8],
asatisfactory
derivation does notexist
[9].
(*) Laboratoire associe au Centre National de la Recherche
Scientifique.
Here we
present
the firstcomplete microscopic
derivation of orbitalhydrodynamics.
Theresulting
equations
are ingeneral
agreement
with the Graham-Liuequations,
andsatisfy
all the relations due to theno-growth
of theentropy
by
reactive terms or toOnsager
relations.However,
we obtain a non sym-metric stress tensor. Itsexpression
agrees with thegeneral
formproposed by
Hu and Saslow[10],
butnot with the relations
they
obtainedby
enforcing
theangular
momentum conservation law. Our resultsdisagree
also in someimportant
respects
with thephenomenological
treatments[7]
on the difficultpoints
related to theangular
momentum conservation law or theexpression
of the stress tensor. Ourequations provide
also, naturally,
a muchsimpler
form for thehydrodynamics
becausethey
arepartly
expressed
in terms of the time derivative of the orderparameter,
rather than in terms of thespatial
derivative.Finally,
our treatment is restricted tolinear
hydrodynamics
where the orderparameter
hasonly
small deviations from aglobal equilibrium
value. But it
actually
gives
anexpression
forbasicajly
all the coefficients
coming
into non linearhydro-dynamics
[10],
sincethey
already
appear in linearhydrodynamics.
A first
point
we want to make is that it is natural torequire
that,
in the limit where thetemperature
T goes to zero, thehydrodynamics
should reduce toequations
describing
the motion of thesuperfluid
alone.This
implies
that the normalvelocity
vD shoulddrop
naturally
out of theequations.
This is not anentirely
obvious condition since sometransport
coefficients mayactually
not go to zero because therelaxation time
diverges
when T -~ 0. But if this timeL- 208 JOURNAL DE PHYSIQUE - LETTRES is
kept
constant(which
willhappen
anyway becauseof the finite size of the
sample),
the normalvelocity
shoulddisappear
at T = 0 since it characterizes thenormal
fluid,
and there is no normal fluid at T = 0.This
property
is satisfiedby
ourequations (this
isnaturally
a result of thetheory,
not aninput).
But it isnot shared
by
somephenomenological
theories[7].
It is also in
disagreement
with the term(1i/4 m) 1.
curl vnintroduced
by
Liu[6]
in the rate ofchange
of thephase,
since this term does not
disappear
at T = 0[20].
This term has been derived on thegrounds
that thecharacteristic vectors of the A
phase,
Å1
andA2,
have to follow a solidbody
rotation around an axisperpendicular
toAi
andA2.
But thismerely
corresponds
to achange
in thephase
of the orderparameter and,
as insuperfluid 4He,
thephase
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 anangular
momentum conservationlaw,
by
combining
theequation
of motion for theangular
momentum with an intrinsic
angular
momentumconservation law. But this does not
bring
any further condition on coefficients.Let us now turn to our results. Our first
equation
is the intrinsicangular
momentum conservation law whichprovides
theequation
of motion for1.
Instead ofal/at,
we use the instantaneous rotation0,
linked to0110t
by :
allat
= nx ~
or n =I
xallat
since we are interestedonly
in the components of nper-pendicular
to theequilibrium
1.
We have :Here
Ls
is thesuperfluid
intrinsicangular
momentum[11], a
is the orbitalviscosity [12], DEd
is thedipole
torque
[1]
andFi = (2
m/~)
V~[~/’~/~(V/J] =
VjqJij
with Graham’s notations[5].
f °
is the free energy in the reference frame where the normalvelocity
if is zero.Explicitly
we have :where
b2
=maxk
I A k
12,f’
=~/7~ where f is
the Fermidistribution,
r is a relaxationtime,
No
thedensity
ofstates at the Fermi
surface ; l is
along
the zaxis,
the other notations are standard.The tensor Cijk has the most
general
form allowedby
symmetry and isgiven
by
[13]
(with
i = x ory) :
where :
In eq.
(4),
ZJ2
isalways
negligible
and has beengiven only
forconsistency.
X(T)
goes topn/4 m
when T -~ 0(p
is the massdensity
and m is the bare mass of3He).
For T -~Tc,
in weak
coupling.
The second term in eq.(3)
iscompletely
new. It is the dominant term in Cijk nearT~,
whereas atlow
temperature
the last two terms take over because of thegrowth
of the relaxation timeT(T,)
when thetempe-rature is lowered. In eq.
(3),
thequantity
b(T)
isgiven
by :
This term is non zero
only
because ofparticle-hole
asymmetry,
but it is of the same order ofmagnitude
asa(T).
It is difficult to evaluateprecisely
becauseNo’ EF/No
is notprecisely
known,
though
it isclearly
of order 1.How-ever, it behaves like
L(T)
T4
at lowtemperature
and is smaller thana(T)
which goes likei(T)
T2.
On the otherhand,
b(T) -
(1
-r/FJ
nearTc
and dominates overa(T).
The first and third terms in cijk may
conveniently
berearranged
with the first two terms of eq.(1)
whichcan be rewritten as :
constant, all the terms
containing
VOdrop
out of eq.(1).
To see this up to orderZ~,
one needs theprecise
expression
for the C tensorcoming [5]
in F. Inparticular,
at T =0,
C 1.
=p/2
whileCII
= -p/2
+ 2mLS/~C.
Now
by inverting-
eq.(1),
we find anexpression
for0110t
which is incomplete
agreement withhydrodynamics
[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 iseasily
deduced from eq.(6).
Theapproximation
ofneglecting Ls
isalways
verygood
except
when one looks at the T -~ 0 limit.Turning
to thedissipative
coefficients,
we have :Next we consider the stress tensor. We obtain :
where
c*k
isgiven by
eq.(3)
except
that thedissipative
terms(i.e.
the last twoterms)
have theirsign changed ;
qJ is the
phase
of the orderparameter
and we have set :It is clear from eq.
(9)
that most of the contribution to (Jij is ofdynamical
origin.
-We can see
that,
because of the first term in eq.(9),
6~~ is notsymmetric,
and therefore theangular
momentum L = r x g is notdirectly
conserved. Moreprecisely,
we have :where
cDk
is thedissipative
part
of ci~k. The first term in theright-hand
side is the contribution of thesuperfluid
intrinsicangular
momentum toSL/~
while the other terms arecorresponding
quasi
particles
contributions. Now if we add the intrinsicangular
momentum conservation law eq.(1)
to eq.(11),
we obtain agood
conservationlaw for the
angular
momentumnamely :
where
c~
is the reactivepart
of cijk.The_stress
tensor eq.(9)
may be transformed if we use theequation
[21]
for thephase
qJ :where
f (T) = f
(dS~/4 lI) dç( - f ’)
(~/E)2 ,
andby
=No
bp
is the fluctuation of the chemicalpotential.
From eq.
(13)
we have[15]
for Graham’scoefficients (
and~~~ :
In eq.
(13),
as well as in eq.(9),
small thermal terms of order(7~/Fp)~
have beenneglected.
The stress tensorbecomes :
where
v°p9
=(p2
i/m2
No)
[ f ~i~ ~pg - f ~ f~pg - f p9 8~~
+~.pj,
theviscosity
tensor in the absence ofemotion,
hasalready
been studied[16].
We note from eq.(15)
that vndrops
out when T goes to zero.L- 210 JOURNAL DE PHYSIQUE - LETTRES
To make contact with
hydrodynamics,
weonly
need toreplace
Qk
in eq.(15) by
its value obtained from eq.(1).
We first obtain for Uij a contribution :which agrees
exactly
with thehydrodynamic
result[10]. (Note
that it is notsymmetrized.)
Next we have the reactive contribution from
V~ :
where $ =
X(l
+b/a)
ifLs
isneglected
andSiki
= 4
b~
+ii
~.
Finally,
for thedissipative
part, theanti-symmetric
contribution fromcjj~
Qk
andV°pq
V pV;
cancel(at
least in the relaxation timeapproximation)
and weobtain :
-where .ae ~
(x2/a) -
(a
+b)2/4
a. Therefore (Jij is made of the first and the third terms of eq.(15), plus
thecontributions
(16), (17)
and(18).
The reactive and
dissipative
terms(17)
and(18)
agree with thegeneral
formproposed by
Hu and Saslow[10],
but not with the restrictionsput
on the reactive coefficients. Indeed wehave,
using
their notations :Finally
we obtain[15] :
for the thermal
conductivity
but no terml
x VT inthe
entropy
current.Let us now
briefly
[17]
outline themicroscopic
derivation. It is a naturalgeneralization
of aprevious
treatment for the
homogeneous
case[11].
We startwith the matrix kinetic
equation
for thequasi
particle
distribution. Then the motion of the orderparameter
is taken care of
by
aspace-time dependent
rotation,
which allows one to obtain a scalar kineticequation
forBogoliubov quasi particles.
Collisions are then handledby
a relaxation timeapproximation,
though
exact treatment of the collisions arenaturally possible.
However,
in contrastto
a firstattempt
[11],
we do notlet the
quasi particles
relax to anequilibrium
distri-bution with energy shiftedby
the orbitalJosephson
effect - (~/2 E) 11(k
xVk9O
(CPk
is thephase
of theorder
parameter)
because this shift does notcorrespond
to achange
in a conservedquantity [18] :
the orbital
Josephson
effect isthere,
butquasi particles
do not relax toward thecorresponding
localequili-brium. All the
quantities
are theneasily
calculated from theirmicroscopic expressions.
Animportant
point
here is the contribution of the normalvelocity
to the intrinsic
angular
momentum conservation law eq.(1).
This is mosteasily
deduced from Galilean invariance.But,
contrary
to thesuperfluid velocity,
the normalvelocity
does not affect the structure of thequasi particles
and thereforeonly
the contributioncoming
from thechange
in thequasi particle
distri-bution should be retained.Acknowledgments.
- Part of this work has been doneduring
a verypleasant
stay at theUniversity
ofSussex,
where I benefited from verystimulating
conversations with A. J.Leggett.
I am also verygrateful
to C. R. Hu forstimulating
discussions,
and I thank very much N. B.
Kopnin
and K.Nagai
for
sending
mepreprints
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] 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 producesa 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