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Applications of topology to the study of ordered systems
R. Shankar
To cite this version:
R. Shankar. Applications of topology to the study of ordered systems. Journal de Physique, 1977, 38
(11), pp.1405-1412. �10.1051/jphys:0197700380110140500�. �jpa-00208711�
APPLICATIONS OF TOPOLOGY TO THE STUDY OF ORDERED SYSTEMS (*)
R. SHANKAR
(**)
Lyman Laboratory
ofPhysics,
HarvardUniversity, Cambridge, Massachusetts, 02138,
U.S.A.(Reçu
le 14 avril1977, accepté
le 22juillet 1977)
Résumé. 2014 Cet article est une version détaillée d’un
preprint
récent danslequel le
problème étaitanalysé
d’une manière très concise. On donne ici d’abord une introductionpédagogique
à la théorie del’homotopie
puis sesapplications
à l’étude deconfigurations
nonsingulières
dans les systèmesordonnés tels que
3He-A,
les cristaux liquides nématiques, etc. On examine aussi brièvement le rôle de l’hamiltonien pour décider de l’observabilité et de la stabilité de ces configurations.Abstract. - This paper is a detailed version of a recent preprint wherein the above
topic
wasanalysed
rather concisely. Apedagogical
introduction tohomotopy
theory is followed by itsapplica-
tions to the
study
ofnon-singular configurations
in ordered systems such as3He-A,
nematicliquid
crystals etc. The role of the hamiltonian in deciding theobservability
andstability
of theseconfigura-
tions is
briefly
examined.Classification
Physics Abstracts
02.40 - 64.60 - 61.30
1. Introduction. - Several years ago Finkelstein
[ 1 ] pointed
out and illustrated with severalexamples,
how a branch of
topology,
calledhomotopy theory
could be
profitably
usedby physicists. Only recently, following
the invention ofmonopoles,
instantons etc.have
particle
theorists come toappreciate
this fact.Even more recent is the work of Blaha
[2]
and Thou-louse and Kléman
[3]
whereinhomotopy theory
wasused to
classify singularities
or defects in orderedsystems
such asferromagnets,
nematics etc. In arecent and somewhat concise
preprint [4]
1 hadreverted to the
approach pioneered by Finkelstein, namely
to thestudy
oftopology
stable but non-singular configurations
in ordered systems and discuss- ed the conditions on the energy functional R for theirobservability.
Thepresent
work is anexpanded
version of reference
[4]
and contains several details omittedtherein,
in addition to an introduction tohomotopy theory provided
fornonexperts.
2. Introduction to
homotopy theory.
- The ordered systems inquestion
will be describedby
a fieldy(x)
defined over the
points
x of somespatial
domain X.The
symbol y
can stand for a unitspin
vector s, if the system is aferromagnet,
the director n, if it isa nematic etc. Let us denote
by Y,
the manifold of(*) Research supported in part by the National Science Foun-
dation
under Grant No. PHY 75-20427.(**)
Junior Fellow, Harvard Society of Fellows.possible
values for y. Forexample
Y =S1,
acircle, if y is a
twocomponent
vector of fixedlength ;
Y =S2
a
2-sphere, if y
is a threecomponent
vector of fixedlength ;
Y = solidsphere
of radius 2 7rif y
is a 3-vectorof
length 5
2 TE and so on.Let us
begin
withX,
a one dimensionalinterval, parametrised by
0 x , 2 n. Consider some fielddistribution
y(x).
So eachpoint xi e X,
there is animage point y(xi)
in Y. As x varies from 0 to 2 n, theimage point
traces out a curve in Ystarting
aty(O)
andending
aty(2 n).
Let us restrict ourselves to fieldsobeying y(O)
=y(2 7r)
= yo, where yo is called the basepoint.
A compact way to write this isy(DX)
= yo, where DX denotes theboundary points
of X. In this case the
image point
traces out a closedcurve anchored at yo. In every
configuration
of thesystem
there exists such animage loop
and vice versa.The
study
of thesystem
thus reduces to thestudy
of the
corresponding
closedloop
in Y.Suspending
for a while thequestion why,
letconsider the classification of the
configurations
ofthe
loop
into classes such that :i)
any twoloops belonging
to the same class canbe
continuously
distorted into eachother,
andii) loops belonging
to different classes cannot becontinuously
distorted to each other. The classesare called
homotopy
classes and members of agiven
class are said to be
homotopic
to each other.Consider for
example
the case where Y =E’
the two dimensional Euclidean space which we may
Article published online by EDP Sciences and available at http://dx.doi.org/10.1051/jphys:0197700380110140500
1406
take to be the x y
plane. Let yo
be anypoint,
say(1,1).
It is evident that there is
only
onehomotopy
class :any
loop
can be deformed into any other and inparticular
to apoint loop
at yo. In terms of the fieldy(x),
it means that anyconfiguration y(x)
can becontinuously
deformed to the constant mapy(x)
= yo.Consider next Y =
E2 - (0, 0). (The
exclusion1 of
the null vector from the allowed values can occurfor
example if y
is themagnetic
field in aplasma,
see Finkelstein and Weil
[5].)
Let yo be anypoint
in Y.It is clear that while any
loop
notenclosing
theorigin
can be
collapsed
to yo, those which do enclose theorigin
cannot be. The latter can be further classifiedby
means of aninteger
m, whosemagnitude
andsign specify
the number of times and the sense in which theorigin
is encircled. It is also clear that mapsbelonging
to distinct values of m arenon-homotopic.
Consider the set
{yO, y 1 y2,
...1,
whereym
standsfor all maps in which the
loop
encircles(0, 0)
m times.It turns out that this set forms a group, that is to say, there exists a law of combination of the
éléments
which
obeys
the group axioms. The group is called the firsthomotopy
group ofY,
and denotedby Hi(Y).
Thesubscript
1 tells us that Xacquires
theform of a closed one dimensional
surface, i.e.,
aloop,
which
topologically
isequivalent
to a circle of 1-sphere SI.
Our interest here will be limited to the set of elements inH,(Y)
and not involve their group structure. For an introduction to thelatter,
see forexample
reference[6]
and additional references contained therein.Now,
we have seen that the elements ofH,[E’ - (0, 0)]
are in one to onecorrespondence
with the
integers
m. Astudy
of the group also reveals that their law of combination is identical to the addition of thecorresponding integers.
One denotesby Zoo
the set of allintegers forming
a group under addition. These results may be summarized asNotice that the choice of base
point
yoplays
a very minor role. It will not beexplicitly
discussed in the future. If ourregion
X is two dimensional and allpoints
on theperimeter
ôX map onto asingle point yo,
X will assume the form of a closed two-dimensional
surface, topologically equivalent
to a2-sphere S2.
The group in
question
isil2(Y).
Likewise if X were a three dimensionalregion
of space, the group tostudy
isI13(y)-
A word about the condition
y(ôX)
= yo. For infinitesystems,
therequirement that y - a
constantyo at
infinity
ensures the finiteness of the energy,assuming
the existence ofgradient
terms. In finitesystems
thisboundary
condition may be forcedby
an external field or the walls of a container. In any event it is
only
with this condition that X becomesa closed surface in Y and the groups become the well studied
il n(Y)’
We now turn to the
question
that has no doubttested the
patience
of the reader :why
thehomotopy
classification ? There are two reasons as far as we are concerned :
i)
Aslong
as the time evolution is a smooth and continuouschange,
it follows that thehomotopy index,
such as theinteger
m, is a constant of the motion. We thus have a conservation law withoutdiscussing
the hamiltonian in anydetail,
except toassume it
produces
smoothchanges
in the state ofthe system.
ii)
We cananticipate
afamily
of metastableconfigu-
rations one from each class. Consider the energy
functional,
which we shall refer to as the hamilto- nian X. In eachclass,
there must be someconfigu-
ration that minimizes it. This is a metastable state : it’s
stability
within the class is a result of itsbeing
a
minimum,
while passage to other classes istopolo- gically
forbidden. We are reminded of thefollowing
situation in one dimensional quantum mechanics : while
finding
the absolute minimum of the energyyields
thegrounds
state, we can get the first excited stateby minimising
in the oddparity
sector(assuming
Je is
parity invariant).
With this motivation we
proceed
tostudy
someof the groups that will interest us.
3. The groups
nm(sn)
andnm(pn).
- We will beinterested here
only
in the groupsllm(sn)
andIlm(P"),
where P" is the
projective n-sphere,
that is then-sphere
S" with
diametrically opposite points
identified.Both m and n will be less than or
equal
to three.Although
the elements of these groups are listed in textbooks,
let us consider one concreteexample
that is amenable to intuitive
analysis :
the groupH,(S,).
The aim is to map a closed
loop
X onto a circleY =
S’
which is alsoparametrised by 0 y
2 n.There are first of all maps in which X never
completes
a tum around Y. An
example
isgiven
infigure
1.All such
loops
may be deformed to apoint,
say at y = 0. We label these mapsby
aninteger m
= 0which counts the number of times X covers or wraps around
Y.
There is anotherequivalent
definitionof m. Pick any
point y
of Y and consider all theFIG. 1. - a) This map is not a constant, but is homotopic to the
constant map y(x) = yo. It has m = 0 ; b) This map has m = 1.
The identity map y = x is a special case.
points
xe X
that map onto it. To each oneassign
a number ±
1,
thissign being
that ofdyldx
at thatpoint.
Then m is thealgebraic
sum of these numbers.Yet another definition is
It is a very
practical
way offinding m
when ourintuition breaks down.
(These recipes
areeasily generalised
to the case where X and Y aren-spheres,
with
dy/dx being replaced by
the JacobianJ( y/x).
If Y is
Pn ;
the rule can beapplied
afterdisregarding
the identification of
antipodal points).
Infigure la,
if we choose a
point y
untouchedby
theloop X,
m is
clearly 0,
while if we choose apoint
to whichtwo
points
of X aremapped,
theopposite signs
ofdy/dx
cancell togive m
= 0.Consider next the case where X goes around Y
once clockwise
(Fig. 1 b).
Aspecial
case called theidentity
map, isy(x)
= x. It is clear m =1, following
any of the three definitions.
(Note
that theidentity
map y = x is a nontrivial map and must not be confused with the
identity
element of the group whichcorresponds
to trivial m = 0map.)
Likewisem = - 1 if X goes around Y counterclockwise.
Clearly m
can be anyinteger
and maps labelledby
different m are
nonhomotopic.
We may summarizeour results as :
Strictly speaking
what we have established is not theequality
of the two groups, butonly
the corres-ponding
sets.It can be
similarly shown
thatll2(S2)
=Zoo’
For
example
in theidentity (m
=1)
map, X covers Yas the skin of an orange covers it. If m >
0,
X wraps around Y m times.Having
illustrated thegeneral principles by
meansof the
preceeding discussion,
let usaccept
withoutproof
thefollowing
results true for n > 2 :where 1 is the trivial group with
just
theidentity
element. The
exception
to therule, n
=1,
will notbe discussed in any detail here.
Among
the maps with n > m ; theonly
nontrivialone with n 3 is
il 3(S2). Hopf [7]
showed thatand
provided representative
maps from each class calledHopf
maps. Since X and Y arespheres
ofdifferent
dimensionality,
theinteger m
has a some-what
complicated interpretation,
which we will discuss in due course.Our mathematical
preparation
iscomplete.
We nowtum to the
applications.
4.
Applications
toconfiguration
withsingularities
or defects. - A
singular point
x E X is characterizedby
the fact that as weapproach
x from many direc- tions we get manylimiting
values for y.Although singular
maps are not oursubject,
we reviewbriefly
the
interesting
work of Thoulouse and Kléman[3]
because our
machinery
makes it easy to do so and because therelationship
between this work and theirs is worthunderstanding.
Let X be a two dimensional
region.
Let us sur-round it
by
a closedloop
or circleS 1
andstudy
thevariation
of y
on it. If the map onSI
is a nontrivial element oflll(Y), (that is,
nothomotopic
to theconstant
map)
a defect orsingular point
lies within.To see
this, imagine slowly shrinking
theloop SI
in size. The map on it must also
change smoothly,
and hence remain in the same class.
Ultimately
theloop
must shrink to an infinitésimal onesurrounding
a
point.
The distribution on this infinitesimalloop
is non constant
by assumption.
As aresult, y approaches
different values as weapproach
thispoint
from different directions. If X is a three dimen- sionalregion
a similaranalysis
in terms of112(y)
is
applicable.
Notice the
analogy
between the way in which adefect in the interior manifests itself via the map
on the
boundary
andi)
Gauss’law,
which relates thecharge
in a volumeto the flux
leaving
asurrounding
surface andii) Cauchy’s theorem, relating
theintegral
of ananalytic
function on a closed contour to the residues to thesingularities
within.Now, just
asopposite charges
orpoles
withopposite
residues may neutralize each other at the
boundary,
so may two
(or more)
defects annul each other toproduce
a trivial map on theboundary.
To see howthis
happens however,
we must know how to combinethe maps, that
is,
the group structure, which is unfortu-nately
behond the scope of this paper.Although
defectanalysis
also involveshomotopy theory,
there ends thesimilarity
with our presentanalysis.
A defect theorist is interested in maps with nontrivial behaviour at theboundary
and adefect
inside,
while we deal with maps trivial atthe boundary y(DX)
= yo, with no defect orsingularity
inside. We now turn to our
subject
proper.5. The nematic
liquid crystal
in two space dimen- sions. - Let us first take as the two dimensionalregion
X the entire x-yplane.
The order parameter is the director n which weparametrize
asn =
(nx,
ny,nz) = (sin j8
cos a,sin fl
sin a, cosP),
where a and
p
are the azimuthal andpolar angles
on
S2.
Since n = - nphysically,
Y =P2
and notS2.
This distinction is however irrelevant for thetopological
group we will consider. Weimpose
thecondition that at
spatial infinity
n =(0, 0, 1),
thatis fl
= 0. This makes the relevant groupH2 (p2)
=Zoo’
1408
Given an energy functional or hamiltonian Je, one metastable
configuration
from each class may be foundby minimising
within that class. This non-trivial task has been done
by
Belavin andPolya-
kov
[8] (here-after
referred to asBP)
for the casewhich describes a nematic with all three elastic cons-
tants
equal.
It was shownby
BP that :a)
in each class JC >, 8na 1 m 1
b)
the minimum is attainedby
theconfigurations
where z = x +
iy ;
and  is anarbitrary
scale para- meter. The restrictionL mi > Y, ni
ensures that as1 z 1 -+ 00 ; P
--+ 0. Thehomotopy
index is m= E mi
and it measures the number of
points
in the zplane
that
yields
the same w. Woo[9]
has shown that these minima are theonly
metastableconfigurations.
Consider next the more realistic case of the nematic in a
cylinder
of radius R, axisperpendicular
to thex-y
plane,
and walls such that n likes to beparallel
to
them,
that is n =(0, 0, 1)
at the walls. Thetopo- logical
classification is then the same as in the BPcase. One
hopes
that there will exist a one to onecorrespondence
between the BPconfigurations
andthe metastable
configurations
in the finitecylinder.
The
reasoning
is that as oneadiabatically
shrinksthe infinite
cylinder (the
x-yplane)
theconfigurations
within will evolve
adiabatically.
But uponexamining
the
equations
1 find that allconfigurations
arepoint- like,
unlike in the BP case. Suchconfigurations
areof no
physical
interest. We are thus faced with animportant
fact : even if theconfiguration
space ofa system admits
interesting homotopy classes, thè configurations
that minimise Je in each class may bephysically
unobservable or even non existant. We would now like to trace theorigin
of this disaster in the case of thé je in eq.(5.1).
Our
analysis
followsclosely
that of Derrick[10]
and is dimensional in nature. We start with the fact that in eq.
(5.1)
is scaleinvariant,
that is to say, twoconfigurations n(x)
andn(x/Â),
relatedby
ascale transformation have the same energy. That is
Consequently,
the minimum in each class isattained,
not
by
oneconfiguration,
but afamily
relatedby
scale parameter Â
(see
eq.(5 . 2)). (The family
isactually
even
bigger,
but that does not concern ushere.)
The BP solutions thus
represent
a system in neutralequilibrium
with respect to scalechanges.
This iswhy
the adiabatic arguments are invalid : no matter howsmoothly
the walls of thecylinder
arebrought
in
(from infinity
toR)
the BPconfigurations collapse
under the
push
to zerosize,
with norestraining
forces.
What we need is an Je with terms that grow as the
configuration
shrinks. One suchexample
isThe
(grad)4
term averts thecomplete collaps,
sinceit grows as
1/d2,
dbeing
the size of theconfiguration,
where
by
size 1 mean thespatial
distance over whichthe field differs
appreciably
from yo. With the wallspushing
in and the b termpushing
out, there will besome size
do
which minimises the energy. Several remarks are in order :i)
Since thesystem
is inreality discrete,
there isa
fundamental length 10,
which is of order moleculardimensions ;
the sizedo
of the continuum solution should be much greater than10
for it to have a sensiblecounterpart in the discrete case.
ii)
The(grad)4
term isonly
anexample
and any term of thatdimensionality,
such as(Ox n)4
isequally good.
These will be referred to as b-terms.iii)
The domain X must be a finitecylinder.
Butfor the
walls,
the1/d2
nature of the b-term willcause the
configuration
toexpand
without limit in the process ofminimising
its energy.iv)
If X were a 3-dimensionalregion,
the a andb terms, which contribute as d and
1/d respectively,
will lead to an
equilibrium
sizedo,
even if X is allof space.
v) Configurations larger
than theequilibrium
onemay also be observed under some conditions. These would of course shrink towards the size
do.
If howeverthe
shrinking
isslow, they
maypossibly
be observed in the process. This is not a far fetchedpossibility.
Certain closed
loop
structures in nematics have beenphotographed
in the process ofcollapse,
which takesa few seconds
[11].
vi)
There are nogeneral principles,
as inquantum
fieldtheory,
that forbid b-terms or evenhigher gradients, though
we cannot vouch for their size.That there must be some b-term can be seen as follows.
Although
we treat thesystem
as acontinuum,
weknow there is an
underlying length 10.
Fields that varyappreciably
over the scale must beexcluded,
that
is,
we mustimpose
a cut off. Theb-terms,
whosecontributions to Je grow
rapidly
for suchconfigura-
tions effect such a cut-off. One cannot say more about the size of the b-terms in
general.
vii)
The abovepoints i)-vi),
dimensional in nature,apply
to othersystems
as well and notjust
nematics.There is one BP
configuration
that can be observed inpart
in a finitecylinder, quite independent
of theb-terms. It is the m = 1 map
p and ç
being cylindrical
coordinates on theplane.
Notice that at p =
/), fl
=7C/2
and ç = a, thatis,
the director lies in the x-yplane
and iseverywhere
radial. It is clear that the introduction of a
cylinder,
whose axis is
along
thez-direction,
and whose walls lie on p =/L,
will not disturb theconfiguration within, provided
n likes to be normal to the walls. Such aconfiguration
has in fact been observed and studiedby
Cladis and Kléman[12], William,
Pieranski and Cladis[13]
andMeyer [14].
To the best of my know-ledge
none of the other BPconfigurations
can beobserved in this manner.
6. The nematic
liquid
in three space dimensions. - Let X be all of three space,parametrised by
thespherical
coordinates r, 0 and (p. Given thatn -
(0, 0, 1)
as r -+ oo, X becomesequivalent
toS3
and the relevant group is113(P’)
=Z,,,,.
Let usdiscuss
briefly
howrepresentative
maps from eachclass,
calledHopf
maps, are obtained and thesignifi-
cance of the index m.
Let us first trade the coordinates r, 0
and ç
forthose
describing S3.
Rather than use theangular
coordinates that span the surface of
S3,
weprefer
four cartesian coordinates xl, x2, X3
and X4
cons-trained
by
We have chosen the radius of the
sphere S3
repre-senting X
to beunity.
The relation between the two sets of coordinates isNote that the north and south
poles
ofS3,
xi = ± 1respectively,
go to r = oo and 0respectively.
Ourmap is the three dimensional version of the familiar
stereographic projections
ofS2
on to aplane.
Themaps
W(Xl,
X2, X3,X4),
where w = e"’ cot(flf2)
aremore
easily
described in terms ofcomplex
coordi-nates Zl = xi +
ix2
and Z2 = X3 +ix4
constrainedby 1 Zl 12 +1
z212
= 1. TheHopf
maps have the featureIt can
easily
be verified that the allowed range for the variable z is the entirecomplex plane. Now,
we
already
know that if X is the entire x-yplane
and Y = p2
(or S2),
there exist maps which fall into classed labelledby
aninteger
m, the BPconfigu-
rations
being representative
elements from each class.In fact the
Hopf
map ofdegree
m,is
just
the BP function of index m with nopoles
andall m zeros at the
origin. Retracing
oursteps
back to r,0,
and ç, weget
The broad features of wm are as follows. Centered at the
origin
is a circle of unit radiuslying
in thex-y
plane
called the core onwhich fi = n
and aroundwhich the field varies most and the energy is most concertrated. The core is surrounded
by
tori ofincreasing
size anddecreasing fi.
Their cross sectionsin the half
plane
(p = ço arecircles,
whose centersmove away from the core as
they
grow in size(Fig. 2).
The cross sections are like the closed lines
of magnetic
field that would
surroûnd
the core if it were a currentcarrying loop.
Thelargest
of these toriwith p = 0
is bounded
by
the x-axis and thesphere
atinfinity.
If we move once around the circular cross section of the
torus fl
=Po in the ç
= 0plane,
am will range between 0 and 2 nm(see Fig. 2).
In otherwords,
as one describes this circle in space, the
image point completes m
turns around thesphere
Y =P2 starting
at the
point
a =0, B = Po
andstaying
on the lati-tude
fl
=B0.
In any otherplane
a = (po, theonly
FIG. 2. - A cross section in the (p = 0 half plane of the Hopf
map. The core (fi = 1t) comes out of the paper as a point. Each
circle corresponds to a given fi. On any one circle fl = Po; a varies from 0 to 2 xm.
1410
difference is that the
image point
starts out at a = mqJo,fl
=Po
andcompletes m
terms around the latitudefl
=Po.
The natural coordinates for these mapsare the toriodal ones, /1, 11
and ç [15],
in terms ofwhich
The
Hopf
maps aremerely representatives
fromeach class. To find metastable
configurations
onemust find the minima of R within each class. If a and b terms are
present
and b islarge enough
obser-vable metastable
configurations
can beexpected.
Thetheory
alsopredicts
thatHopf
mapslarger
than thestable one may be observed
collapsing
if the process is slowenough.
Now suchconfigurations
with a core,have been seen in nematic
liquids [11]. Although they
start out with
arbitrary shapes they
become circularas
they
shrink. It istempting
toidentify
these withHopf
maps or moregenerally
with mapshomotopic
to them. A more detailed
experimental study
isneeded, especially
near the core, to confirm thishypothesis.
On the theoretical side remains thequestion
ofminimising X
in the presence of a and b terms. Enz[16]
has solved theproblem approximately
and obtains maps
homotopic
to theHopf
map,following
a route very different form ours.7. 3 He-A in three space dimensions. - Let X be
once
again
all of3-space.
The order parameter is a triad of orthonormal vectors1,
x, and x2, where 1 is the orbitalangular
momentum, while x 1 and x2 determine thecomplex phase
in theplane perpendi-
cular to 1. Our
boundary
condition is that atspatial infinity
the triad assumes a standard form with xl, x2 and 1pointing along
the x, y and z axesrespectively.
The triad at any interior
point
withposition
vector rmay be obtained
by performing
anSO(3)
rotationon the standard triad at
infinity.
Let the vectorangle n(r) specify by
itsmagnitude
anddirection,
theangle
and axis of the rotation. Since n is a vector of arbi-
trary
orientation andmagnitude 5
2 n, Y = solidsphere
of radius 2 n. Since allpoints
at theboundary
refer to the same
(identity) element,
thetopology
of Y is
S3.
The careful reader would have noticed that our Yactually
double counts the elements ofSO(3),
in thefollowing
sense.Although
theSO(3)
rotation
angle
can range from 0-2 n about anyaxis,
a rotation
by
an amount 0 about any axis isphysically equivalent
to a rotationby
2 n - 0 with the axis reversed. Thus we needonly
a solidsphere
of radius n.Our
sphere S3
thusrepresents SU(2),
for which0 , 1 Q 1
4 n. It can bereadily
shown that Y forSO(3)
isequivalent
top3 (see appendix).
Weshall continue to use Y =
S3
since the distinction isinconsequential : H3 (p3)
=il 3(S3).
Notice that the manifolds X and Y are both solid
spheres
withpoints
on the surfaceidentified,
andare thus
equivalent
to S3. At least one nontrivialmap
suggests
itselfreadily :
we rescale X to asphere
of radius 2 n, and then do the
identity mapping
on to Y. The
general
solution to thisproblem
isOne
specific example
of the smoothfunction f(r)
is :where  is an
arbitrary
scale. Thehomotopy
index ism = 1 for this
identity
map, since to eachpoint
ofY ;
therecorresponds just
onepoint
of X. For thesame reason, we can
get
a map of index mby taking
a
sphere
Y of radius 2 nm(wherein
each distinct element ofSU(2)
appears mtimes)
andmapping
Xon to it :
The
configuration
may be visualised as follows.At the
origin
since fi =0,
the triad is in standard form. As we move away in somedirection ;
the triadrotates about an axis
parallel
to thatdirection,
andby
anangle
that goes from 0 to 2 nm as r goes from 0 to oo.Figure
3 shows the situationalong
somespecial
directions for the case m = 1.FIG. 3. - The m = 1 identity map in 3He-A. As we leave the
origin along any ray, the triad twists along that axis and completes
a 2 x revolution as we reach infinity.
As
always
we haveonly presented examples
fromeach class. The determination of metastable states involves
minimising
the hamiltonian in each class.8. A word of caution. - We conclude our dis- cussion with the
following
words of caution : the entirepreceeding analysis
is anapproximation.
Thisis a reflection of the fact that
although
werepresent
our media as
continuum, they
are inreality discrete,
characterisedby
somelength 1.,
which may be alattice
spacing,
molecular dimension etc. Recall that the continuum fieldy(x)
isusually
defined asthe average of a
microscopic
variable over a smallbut
macroscopic
volumesurrounding
thepoint
x.This volume is much
larger
than10.
If the fieldy(x)
so defined varies very
smoothly,
thatis,
its scalefor variations is much
larger
than10,
the medium may bereliably
described as acontinuum,
and ourtopo- logical analysis applied
to it. If however thesystem
wanders off intoconfigurations
where it cannot berepresented meaningfully by
a continuumfunction,
we must abandon our
analysis,
and inparticular
the
topological
conservation laws.Consider the
following example. Imagine
aconfigu-
ration that is very
large
and smooth and is describedby
a continuum functiony(x)
thatbelongs
to a classdistinct from the vacuum.
Imagine rescaling
thisconfiguration
to smaller and smaller sizes. The continuumapproximation
will break down at onepoint.
If wekeep going
tillonly
a few lattice sitesor molecules are involved we have
essentially
reachedthe vacuum.
(This
would nothappen
in a real conti- nuum, for aconfiguration,
howevermuch reduced inscale,
will contain all the details of theoriginal
map and hence the
homotopy index.)
The fact that thehomotopy
index may thus bedestroyed
is a fatalblow to our
analysis
inprinciple,
but notnecessarily
so in
practice
if one of twothings happens : i)
In the course ofperforming
the aboverescaling,
we encounter states of very
high
energy. This is what wouldhappen
if we had asufficiently large
b-term : once we scale down to a size
do,
furtherreduction in size would cost a lot of energy,
thereby presenting
an effective barrier. It is of course necessary thatdo
be muchlarger
than1.
for ourarguments,
based on the continuum estimate of energy, to be valid.ii)
Eventhough
there is nobarrier,
the time taken for the system to gothrough
the above mentioned stages islarge.
In such a case we have anapproximate
conservation law and a
homotopy
classification valid over sizeableperiods.
The
shrinking configuration
is aspecial
case ofa
general phenomenon
of the systemgoing
intoconfigurations
that vary sorapidly
that the conti-nuum
description
breaks down. Ourtopological analysis
is useful if such excursions are either slowor
suppressed by
energy barriers due to thegradient
terms in je. Even if one
picks
on aspecific
system with a well definedhamiltonian, estimating
the timescales for these processes is a very difficult task.
The purpose of this
digression
is not to attack thisproblem
butonly
topoint
out its existence and theassumptions implicit
in ouranalysis.
9.
Summary
and discussions. - Weemployed homotopy theory
toclassify
thepossible configu-
rations of several ordered systems in two and three space
dimensions,
since theanalysis yields
infor-mation on metastable
configurations
andtopological
conservation laws. But we saw that our
analysis
was
only
asgood
as the continuumapproximation
to the
system.
Thus a staticconfiguration
of sizedo anticipated by
the continuumtheory
had anybearing
on the real
system only
ifdo > 10,
which in turndepended
on the b-term in the hamiltonian.Similarly
the
topological
index was seen to be conservedonly
as
long
as thesystem
did not wander off into arapidly varying configuration
where the continuum des-cription
failed. Thegeneral analysis
was thus inte-resting only
if the excursion into such states waseither inhibited
by
an energy barrier or for someother reason, slow.
Although
we studiedonly
nematicsand
3He-A,
ourtopological analysis
can beapplied
verbatim to any system in two or three space dimen- sions for which Y = P" or
S", n
=2,
3. Forexample
we can expeçt a
Hopf
map in aferromagnet
if Xis two dimensional. Even for a different
Y,
once thegroup
nn(Y)
is found(say by referring
to abook)
the rest of the
analysis
is the same.Acknowledgments.
- 1acknowledge
my indeb- tedness to Professors D.Mumford,
B.Halperin,
and R.
Meyer,
and R.Rajaraman
for theirguidance during
the course of this work. 1 amparticularly grateful
to mycolleagues
David Nelson and Gordon Woo for numerousprofitable
discussions.Appendix.
- We shall prove here thatY[SO(3)]=p2.
Let us
begin by considering Y[SU(2)].
If we startwith an
arbitrary
2 x 2complex
matrixand
require
that it beunitary (UU ’
=I)
and hasdet = + 1 we get the
general
element ofThus the elements of
SU(2)
can be visualized aspoints
on a unitsphere S3. Now,
to every two elements ofSU(2) differing by
asign,
therecorresponds
oneelement of