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Zeros of covariant vector fields for the point groups : invariant formulation
M.V. Jarić, L. Michel, R.T. Sharp
To cite this version:
M.V. Jarić, L. Michel, R.T. Sharp. Zeros of covariant vector fields for the point groups : invariant
formulation. Journal de Physique, 1984, 45 (1), pp.1-27. �10.1051/jphys:019840045010100�. �jpa-
00209736�
1
LE JOURNAL DE PHYSIQUE
Zeros of covariant vector fields for the point groups : invariant formulation
M. V. Jari0107
(*),
L. Michel and R. T.Sharp (**)
Institut des Hautes Etudes Scientifiques, 35, Route de Chartres, 91440 Bures-sur-Yvette, France (Reçu le 13 avril 1983, accepté le 12 juillet 1983)
Résumé. - Pour tous les groupes
ponctuels (sous-groupes
fermés) finis ou continus des groupes orthogonaux 0(2) et 0(3) nous donnons une based’intégrité 03B8i(x), ~03B2(x) e03C3(x)
pour lespolynômes
invariants et pour leschamps
de vecteurs
polynomiaux,
nous donnons les équations etinégalités
définissant les strates (union des orbites de même type). Finalement, nous écrivons des équations donnant les zéros d’un champ de vecteurs covariants sur une strate donnée; ceséquations
sont linéaires dans les composantes (invariantes) du champ de vecteurs sur lese03C3(x),
les coefficients de ces termes étant eux-mêmes des invariants. Tous ces résultats sont résumés dans des tables et illustrés par un exempled’application
physique desymétrie cubique.
La méthodemathématique
pour obtenirces résultats est
expliquée
de façon à permettre au lecteur del’appliquer
à d’autres groupes.Abstract. 2014 All finite as well as infinite (matrix) point
subgroups
of full orthogonal groups in two and three dimen- sions are considered. For eachpoint
group apolynomial integrity
basis for invariants and the basic polynomialvector fields are first given. Then, the strata are defined via equations and inequalities involving the
integrity
basis.Finally, equations
for zeros of a covariant vector field aregiven
on each stratum in terms of theintegrity
basis,which appears via coefficients in the
expansion
of the vector field on the vector-field basis. All the resultsare tabulated and an illustration
using
the cubic group is presented. Mathematicalbackground
sufficient for extensions of the results is also given.J. Physique 45 (1984) 1-27 JANVIER 1984,
Classification Physics Abstracts
02.20
1. Introduction
When a
physical
system has a symmetry group g, itsproperties
can be studied in terms of 9-invariant functions defined on theconfiguration
space on which till acts. When the action of 9corresponds
to a linearrepresentation r,
we consider instead of 9 the matrix group G whichrepresents
19.(G
is theimage
oaf 9under
F.)
The matrix groups with which we dealcorrespond
to the actions of closedsubgroups
of fullorthogonal
groups0(l),
1 =1, 2, 3,
on one, two and three dimensional Euclidian(carrier)
spaces describedby
cartesian coordinates. These groups are the ones(*) Freie Universitat Berlin, Institute for Theoretical
Physics.
Present Address :Physics
Dept, Montana StateUniversity,
Bozeman, Montana 59717, U.S.A.(**)
On leave from Physics Department, McGill Uni-versity, Montreal, Quebec, Canada.
most
frequently
met inapplications
tomolecules,
solids(macroscopic
tensors, electronic structure, Lan- dautheory
ofphase transitions, etc.), problems concerning spherical
bodies(earth, stars),
and similarproblems.
We formulate our methods with sufficientgenerality
thatthey
may be used for other finite orcompact
groups.Since Bethe’s famous paper
[1]
on cubic harmonics many papers have been written on theproblem
offinding independent
sets ofcrystal
harmonics.Hop-
field
[2] recognized
that allcrystal
harmonics of agiven symmetry
can be written as linear combinations of a few basic ones, with invariant functions as coeffi-cients ;
this was well known to the mathematicians(see,
e.g.[3], [4]
forreferences). Papers by Meyer [5]
and, later, by Killingbeck [6], Kopsky [7]
and Michel[4]
deal with invariants of
crystallographic point
groups.Other
crystal
harmonics(covariants,
ortensors)
weretreated
by
McLellan[8],
Patera et al.[9]
andKop-
Article published online by EDP Sciences and available at http://dx.doi.org/10.1051/jphys:019840045010100
sky [10, 11 ].
Since the mid-fifties new mathematical results haveappeared (see Stanley [12]. (or
an excellentreview)
which aredirectly applicable
to these pro-blems ;
these results have been used and reviewedby
Michel et al.
[4, 13-15].
This paper has several motivations. Not the
least,
we
hope
toacquaint
solid statephysicists
with themathematical methods mentioned
above; they
pro- vide apowerful
tool inproblems involving
invariantsand covariants of space and
point
groups. Refe-rences 4 and 13 written with a similar
perspective,
dealonly
withpolynomial
invariants. Here we focus onpolynomial
covariant vector fields. Wedevelop
anew method for
finding
their zeros associated with agiven
symmetry. The method involvesonly
invariantsof the
relevant
matrix group G. Such aproblem
mustbe solved in many
physical applications,
such asfinding
minima of the Landau free energy inphase transitions,
minima of aHiggs potential
in gaugetheories,
fixedpoints
ofrenormalization-group
equa-tions,
bifurcationpoints
of a nonlinearproblem,
etc.For each group
G,
wegive
canonicalequations,
interms of
invariants,
for zeros of covariant vector fields at each type of symmetrypoint by
G. We also collectresults,
someknown,
somegiven
for the firsttime, concerning subgroups
of0(l),
I =1, 2,
3. Inparticu- lar,
we list little groups of G andgive
invariant des-criptions
for associated strata. We tabulateexplicitly
the basic
polynomial
invariants and covariant vector fields.In the next
section,
we summarize the mathematicalbackground
which would be useful inextending
ourresults to
subgroups
of0(l),
I >4,
or to other repre- sentations of relevantphysical
groups.Physicists
interested
only
insubgroups
of0(3) (and
not in 4-and 5-dimensional irreductible
representations
of theicosahedral
groups)
needonly
to familiarize themselves with the definitions and notations beforeproceeding
to section 3 where the relevant results are
presented.
2. Mathematical
background.
2.1 GROUP ACTIONS. - We consider actions of a
unitary
matrix group G on an n-dimensional vector spaceEn.
Later on, we shall restrict ourselves to theparticular
case ofreal, therefore, orthogonal,
repre- sentations on real vector spaces. G isgiven
as therepresentation
r of aphysical symmetry group 9;
that
is,
G is theimage
of 19 under r(or
G = Im9).
We
emphasize
that invariants and covariantson En depend only
on theimage.
Since different represen- tations of different groups, orinequivalent
represen- tations of the same group, may have the same orequivalent [in U(n) !] images,
it isadvantageous,
as
pointed
out in references4, 16,
toclassify
andstudy
group
representations according
to theirimages.
We denote an
arbitrary
element(a matrix)
of Gby g
and a vectorfrom En by
r. The transformof r by g
is written g. r which in a
given
basis reads xi --->gij Xj
with a summation overrepeated indices;
r may be aconfiguration
space vectorand g
maybe,
forexample,
a rotation matrix.
It is well-known that G defines in
En
certain geo-metric structures, such as rotation axes and reflection
planes,
whosepoints
are left invariantby
certainelements of G. This leads to the
study
of little(iso- tropy) subgroups
L of G.By
definition the little groupL(r)
of a vector rof En
contains all elements of G which leave r invariantsBy
the definition ofL(r)
anelement g
of G not inL(r)
transforms r into9. r :0
r. The set of all distinct g. r, as g runsthrough G,
is called a G-orbit. SinceL(g.r)
=gL(r) g-1
it follows that the little groups of vectors on the same orbit areconjugated;
thereforewe may label an orbit
by Q([L], r)
where[L]
is theconjugacy
class of its little groups and r is one of its vectors.Furthermore,
two different orbits may share little groups; an obviousexample
is thepair Q([L], r)
and
Q([L], Ar)
where A is a non-zero real number.The union of orbits with the same
[L]
is called astratum, denoted
by E [L].
Strata may be viewed in the
following
way. Given alittle group L we may construct the linear
subspace
of
En,
denotedE; (the
notation Fix L is sometimesused), spanned by
all vectors invariant under L. For finite groups the dimensioni(L)
ofE;
isgiven
interms of characters
x of T :
Symmetry subspaces En
are a naturalgeneralization
of symmetry axes and reflection
planes.
It can be seenthat L’ > L if
E;’
cEn (incidentally,
this relationcan be
incorporated
into an efficientalgorithm
fordetermination of all little groups of a discrete group
[17, 18]). Therefore,
a stratum isgiven by
We remark that the
topological
closure of the stratum is the union of thesubspaces E;
for L E[L].
As an
example
consider the groupSO(3)
of three-dimensional rotations
around
theorigin.
A vectorr 0 ¥-
0 is invariant under all rotations around the axis{ Â.r 0 }
and its little group isSO(2).
The otherrotations of
SO(3) acting
on rogenerate
thesphere II r112 = II ro 112,
the orbit of ro. The little group of theorigin
is the whole groupSO(3). Thus,
there aretwo strata, the
origin
and the rest of space, associated with the classes[SO(3)]
and[SO(2)] respectively.
For a
compact
or finite group there is a naturalordering
among classes of little groups.[L] [L’] if, by definition,
there are L E[L]
and L’ E[L’]
such thatL . L’. There is a
theorem,
not trivial to prove[33],
that there is a minimal class[Lo]
whose stratum, thegeneric
stratum, is open dense. In the case of afinite
matrix groupG, Lo
containsonly
theidentity
element.
Z . 2 INVARIANTS AND COVARIANT VECTOR FIELDS. -
Let
D( g)
be a linear n’-dimensionalrepresentation
ofG carried
by
the vector spaceEn,.
A functionf (r)
defined
on En
and valued inEn,,
is called a G-covariantor tensor if for every g E G
In this paper, we are
mainly
interested in twospecial
cases :1 ) En,
carries the trivial one-dimensional repre- sentation ofG,
andD( g)
--_1;
thenf (r)
is called aninvariant
function;
2) En,
carries the samerepresentation
asEn,
soD( g)
= g ; thenf (r)
is called a covariant vectorfield,
which we write as
f(r).
In the case of
SO(3)
discussedabove, f (r)
=II r II 2
is an invariant and
f(r) = II
r112
r is a covariant vectorfield.
Z . 3 POLYNOMIALS ON THE REPRESENTATION
(CARRIER)
SPACE
En.
- To describe theproperties
of aphysical
system, we may have to use distributions or functions which are not smooth
(infinitely differentiable),
butusually
smooth functions(which
include inparticular analytic functions)
are sufficient. For acompact (or finite)
group Schwarz[19]
has shown that G- invariant smooth functions are smooth functions of invariantpolynomials.
Moregenerally,
as we shallsee, smooth invariant and covariant vector fields can
be
expanded
on thepolynomial
basis(which
we willintroduce for
polynomial fields)
with smooth func- tions ofpolynomial
invariants as coefficients. This isour
justification
forrestricting
this paper to thestudy
of
polynomial
invariants and vector fields. In thissection,
we consideronly
finite groups and shall say later how the resultsgeneralize
to the case of infinite compact groups.Denote
by
P the(infinite dimensional)
vector space of allpolynomials
in r EEn.
It is also aring.
There aretwo natural
compatible decompositions
of P as adirect sum. One is
- B.
where
P(’)
is the vector space of allhomogeneous pqlynomials
ofdegree
m. Since the action of G on Ppreserves the
degree,
eachP (m)
carries a linear repre-sentation of G. The character
X(m)(g)
of theG-repre-
sentation on P(-) is
given by
thegenerating
functionwhere t is a
dummy
variable.Let a label the different
equivalence
classes ofirreducible
representations ra.
of the group G. We recall that anisotypical (also
calledfactorial)
repre- sentation of G is a direct sum ofequivalent
irreduciblerepresentations.
The second naturaldecomposition
of P is into the direct sum of spaces
spanning isoty- pical representations
Pa
is the vector space of a-covariantpolynomials.
Weuse a = 0 to label the trivial
representation,
soPo
is the
ring
of G-invariantpolynomials.
Apolynomial p E P
may beprojected
onPa. by
anorthogonal
projector J,,, given by
The
multiplicity c7
of the irreduciblerepresentation Ta
on the space_1_B 1-1 - -’_"IIr.
is
given by
thegenerating
functionMa.(t)
obtainedby forming
the Hermitian scalarproduct
of the charac- tersxa( g)
andXIMI(9)
-- -
Note that
[11]
For invariant
polynomials,
the functionMo(t)
wasfirst
computed by
Molien[20].
In the mathematical literatureM«(t)
is often called the Poincare series.2.4 CASE OF
(PSEUDO-)
REFLECTION GROUPS. - Apseudo-reflection on En
is aunitary operator
u, of whose neigenvalues n -1
areequal
to one while thenth eigenvalue
is a root ofunity
different from one.The space left invariant
by
u is called a reflectionplane.
When thenth eigenvalue
isequal
to minus one uis
equivalent
to anorthogonal operator
and issimply
called a reflection. A group R
generated by (pseudo-)
reflections is called a
(pseudo-)
reflection group.Any
such matrix group can be
decomposed
into irreducible groups and the list of irreduciblepseudo-reflection
groups was determined
by
Coxeter[21]
andShephard
and Todd
[22]. They
also showed that the Molien functionMo(t)
for an irreducible(pseudo-)
reflectiongroup can be written in a
unique
way asn
Mo(t) = 1/D(t) - n (1
-t di)- 1 (12)
;= 1
They computed
thecorresponding exponents dim
and showed that
they satisfy
the relationAs
suggested by equations
12 and13,
one can findn
algebraically independent homogeneous polyno-
mials
Oi(r) of respective degrees di
such that every R- invariantpolynomial
is apolynomial e C[01,
...,On],
the
ring
ofpolynomials
inB 1, 0,,
withcomplex
coefficients. One also says that
Po
is apolynomial ring.
Let us recall a well known
example.
Let R be thegroup 1tn of n x n
permutations
matrices whose all entries are zeroexcept
one in each row and each column which isequal
to one. The matrix group 1tn is a reducibleorthogonal representation
of the sym- metric groupSm
the group of allpermutations
of nobjects.
Indeed the one dimensional space of vectors with all coordinatesequal
is invariant. The ortho-gonal
space of vectors the sum of whose coordi- nates vanishes carries an(n - 1)
dimensional irreduciblerepresentation
ofS..
The reflections in 1tn are matricespermuting just
two coor-dinates axes. Since these
permutations generate it,
1tn is a reflection group. It is well known that anysymmetric polynomial
in the coordinates xl, ..., xnChevalley [23]
fororthogonal
groups andShephard
and Todd
[22]
forunitary
groupsproved :
Theorem 2.4.1 The
ring Po
of G-invariantpoly-
nomials is a
polynomial ring
if andonly
if G is apseudo-reflection
group.Chevalley
alsoproved :
Theorem 2. 4. 2 For any reflection group
R,
P is aI R dimensional
free module overPo
which transforms under R as theregular representation.
The last theorem extends to
pseudo-reflection
groups. It is a
generalization
of aneasy-to-prove property :
everypolynomial
in one(real)
variable has aunique decomposition
where qo and q 1 are
polynomials
in1
Here, n
= 1 and R is the two element group0(1).
One can also
specify
thedegrees
of the basicpoly-
nomials of the module P over the
polynomial ring Po :
the number of basicpolynomials
ofdegree s
is the coefficient of ts in the
polynomial
The
expression free
module means that the expan- sion of anyp(r)
E P as a linear combination of thebasic
polynomials br(r),
r =1, ...,
R1,
with coeffi-cients in
Po
=C[O 1,
...,0J
isunique
We
give
anothersimple example.
The four elementI- -1 1 - -B
is a reflection group. It is
Abelian,
so it has fourinequi-
valent irreducible
representations
of dimension one.Its Molien function is
(1 - t2)-2,
one can take for01
and
02, x2 and y2, respectively.
SoPo
is thering
of alltwo variable
polynomials q (X2, y2)
and the other threePa’s
arexPo, yPo
andxyPo. Thus,
for this groupequation
16 isexplicitly
In the
tables,
section4,
moreinteresting examples
aregiven.
It is a
simple corollary
of theorem 2.4.2 that differentsubspaces Pa
are free modules overPo
each ofdimension
(dim ra)2.
Inparticular
for the vectorfields
(a
= v, may bereducible)
there aren2
compo- nents of n basic vector fields ofdegrees (did
-1).
One can take for the basic vector fields the
gradients O9i
of the invariants0i,
i =1,...,
n. So every R-cova-riant vector field
v(r)
has aunique expansion
Z . S FINITE GROUPS NOT GENERATED BY REFLECTIONS.
- In this case it can be shown that there exists a
polynomial ring C[81, ..., 0n]
of nalgebraically
inde-pendent homogeneous
G-invariantpolynomials Oi(r)
such that the
ring
P ofpolynomials on En
is a finite free module overC[O 1,
...,of :
see for instanceStanley [ 12].
This author shows that one can
always
choose thedegrees
of eachOi(r)
smaller than orequal to ) I G I.
Moreover,
thesedegrees satisfy
ageneralization
ofequation
13where k is an
integer
greater than one. The module Pover
C[01,..., OJ transforms as
a direct sum of kregular representations
of G.Similarly,
thePa’s
are free modules over
C[91, ..., On]
of dimensionk(dim Ta)2.
Forinstance,
thering Po
isgenerated by (n
+ k -1)
basicpolynomials Oi(r),
i =1,...,
n, and([Jp(r), f3
=1,..., k -
1 andPo
is a freeC101, ..., On]
module of dimension k. That
is,
every G-invariantpolynomial po(r)
has aunique decomposition
where
wo(r)
* I. The basic invariantpolynomials 8i
and qJ p form anintegrity
basis forPo.
For each
qJp, P
>0,
there is aninteger power vp
> 1 such thatw§°
eC[0i,..., 0J.
If6p
=degree CfJp(r),
the
corresponding
NTolien function iswhere
D(t)
andQ(t)
are definedby
theequation 15,
same as in the case of
(pseudo-)
reflection groups, withC[81, ..., 0,,]
inplace of Po. Using (10) :
We shall call the basic invariants
8i(r)
and(fJp(r)
the denominator and numerator
invariants, respectively.
Unfortunately,
there is no efficientalgorithm
todetermine the minimal
integrity basis,
i.e. the one withthe smallest k or, cf.
equation 23,
with the smallestdegrees dim.
It does notcorrespond necessarily
to thecase
N(t)
andD(t) relatively prime (see Stanley [12]
for
examples).
In order to illustrate a difference between a free and a non-free module we consider a
simple example,
the two-element group
{I, - 1 }
in n = 2 dimen- sions. Since it leaves no vector r # 0 invariant, andsince G I
=2,
thepossible
0’s areX2, y2
and xy. The Molien function is(1
+t2)/(1 - t2)2.
In this casethe minimal
integrity
basiscorresponds
to k = 2 and81
=x2, 02 = y2
and wi i = xy.Hence,
every inva- riantpolynomial po(x, y)
EPo
can be written asIn that case P is a free
C[x2, y2 module
of dimensionk I G I
= 4 and the basicpolynomials
are1,
xy, x and y.Thus,
apolynomial p(x, y)
E P can beuniquely
written as
P is also a
Po module,
but it is not afree Po
module.Indeed,
togenerate
allpolynomials
with coefficients q EPo it
is sufficient to take as a basis1,. x
and y.So,
P is a
Po
module. It is not free because the decom-position
is notunique;
e.g.for p(x,.y)
=x2 y
one haswith
either q
= xy EPo or q’ = x2
EPo.
Since thegroup is Abelian the vector
representation
is reducibleand the four
(k. dim F,
= nk =4)
basic vector fieldsIn the
following section,
we will treat the casesG R. In a more
general
case, inconstructing
thebasic
fields,
one must use a brute force method.Namely,
one chooses monomials ofsystematically higher
andhigher degree,
notexceeding I G 1,
andapplies
anappropriate projection
operatorto find
the ith
component( j
iskept fixed)
of an a-covariant field.
Checking
forindependence
withpreviously
found fields andusing
the functionsM«(t)
one
eventually
constructs an a-covariant basis.2.6 SUBGROUPS OF FINITE REFLECTION GROUPS. -
If G is not a reflection group but is a
subgroup
of areflection group
R,
GR,
we can choose for the denominator invariantsOi(r)
those of R.Then,
cfequation 23, k = I R 1/1 G I.
As we have seen, P is anI
R1-dimensional
free module overC[01,..., 0J
whichtransforms like the
regular representation
of R. Whenrestricted to G this
representation yields
k-times theregular representation
of G. The basicpolynomials br(x), equation 16,
areexactly
the same for both R and G but their covarianceproperties
differ between Rand G.
However,
it is notguaranteed
that this methodyields
the minimalk, except when I R 1/1 G I
= 2.As shown also
by Stanley [3], [12] (the preprint
wasused and
explained
in[4])
there is an efficient methodwhen
where R’ is the group
generated by
the commutators of R(i.e. by
the elements of the formaba-1 b-1).
R’ is the smallest invariant
subgroup
of R such thatthe
quotient R/R’
is an Abelian group.Consequently,
irreducible
representations
ofR/R’ yield
allinequiva-
lent one dimensional
representations
of R.Polyno-
mials which transform
according
to such representa- tions areusually
calledquasi-invariants
of R. Allquasi
invariant
polynomials,
which transformby
a one-dimensional
representation x«
ofR,
form a one-dimensional
Po
moduleP., = t/Jcx(r) Po. Stanley [3], [12]
gave an
explicit
construction for basicpolynomials t/Ja.(r).
Since we will need this constructiononly
forreflection groups, we
explain
thisslightly simpler
case.For any reflection u E
R, U2
= 1 we havex«(u) _ ± l.
Stanley’s
rule iswhere
lu(r)
is the linear form of thehyperplane
of thereflection u. As a
particular
case we can consider therepresentation x(g)
= det g. For any reflection u ER,
det u = -1,
and in that caseIt was
already
known thatIndeed,
sinceJ(r)
is the determinant of the n compo- nents of n vectorsVOi
it is apseudoscalar
whichchanges sign
when one crosses a reflectionplane (and only then,
as can be seen from theorem 3.1 of the nextsection). Incidentally, equations
31 and 32yield
for the number of reflections in R :’
n
All
quasi
invariants of R arequasi
invariants of everysubgroup
of R. When G satisfies(29)
then allinvariants of G are obtained from the
quasi
invariantstjJ a(r) Po
of R such that GKer xa (kernel
ofXa)’
i.e.Xa(g)
= I for every g E G. HenceStanley’s
theorem :pG,
the space of G-invariantpolynomials,
is a freePo
=C[e1,
...,Bn]
module with basis0,,,(r),
GKer xa
(here
we used asuperscript
G in order to dis-tinguish
betweenPo
andPo,
therings
of G- and R-invariant
polynomials, respectively).
Thatis,
forevery
p(r)
EPo
where
t/1o(r)
--- 1and qa E Po.
The dimension k of the modulepG,
is the numberoft/1a
inequation
34 and thenumerator invariants for G are
(p,,,(r)
=t/1 a(r).
Such
explicit algorithms
forfinding
nk basic G- covariantpolynomial
vector fields are not known.First,
one takes(n
+ k -1) gradients
of theintegrity
basis but one should also look among
quasi-vector
fields
of R(their components
arepolynomials
whichtransform like the
product
of anR-quasi-invariant
andan R-covariant vector
field),
which are G-covariant vector fields. Note thatalthough
the number of basicR-quasi-vector
fields isprecisely
knthey
are not, ingeneral,
basic G-covariant vector fields.We recall a
general
method forobtaining
from agiven covariant,
the sametype
of covariant but of smallerdegree : if po(r) E P 0 ’, operate
on the covariant with the operatorpo(V).
In three-dimensions aquasi
vector field may be obtained
by taking
a curl(V x ) 6f a
vector field or
by forming
the crossproduct
of two(quasi)
vector fields.Finally,
when G is irreducibleon the
real,
but becomes reducible on thecomplex
there is a real
orthogonal
matrix J which commuteswith G and which satisfies
Therefore,
ifv(r)
is a G-covariant vectorfield,
Jv isanother one
orthogonal
to v, i.e.(v, Jv)
= 0, wherewe use
( , )
to denote theorthogonal
scalarproduct.
Z) ORBIT SPACE. - The
integrity
basis for a group G defines a map(function),
which we will denoteby
a)or
m(r), from En
intoEn+k-1
The whole space
En
ismapped
onto an n-dimensional(semi-algebraic)
surface inEn+k-1.
We will call this surface the orbit space and we will denote itby w(En).
The usefulness of this concept arises from the fact that
m is constant on any
given
orbitQ([L], ro),
and that it separates orbits
[24, 25]. Consequently,
all G-invariant structures in
Eft’
such as orbits and strata, appear also in the orbit spacecv(En).
Severalpapers were
recently
devoted to the relations determin-ing
both the surfaceOJ(En)
inEn+k-1
and theimage
of the strata in the same space
[26-28].
A
physical problem
which possesses a symmetry Galways
has« degenerate»
solutions which fall on an orbit.Therefore,
it is sometimesadvantageous
toformulate the
problem
interms
of invariants so that asolution
(5-1, ..., k, -1, (P ...1 Wk- 1)
inEn+k-1
i is found first.Only
the solutions which fall on the surfaceOJ(En), i.e.,
ones from the orbit space, arephysical
ones.
Corresponding
orbits0([L], r)
of solutions inEn
can then be foundby employing
the inverse mapw-1
,The inverse
map w-’
1depends only
on G and isindependent
of thephysical problem
inquestion.
Therefore,
for agiven G, OJ - 1
can be determined oncefor all. As an
illustration, o)-’
will begiven
in section 4 for the cubic groupoh-
2.8 EXTENSION TO COMPACT GROUPS. - For
(con- tinuous)
compact reflection groups we cancompute
the Poincare function for invariants : it is of the formMo(t)
=1 /D(t)
and thering
of invariantpolynomials
is a
polynomial ring. However,
theChevalley
theo-rem 2.4.2 does not
apply. Also,
compact groups other than reflection groups can haveMop)
=1 /D(t).
So theproblems
we wish to solve are more difficult forcompact groups in
general.
Theseproblems happen
to be very
simple
for0(3)
and for one-parameter groups, theonly
compact groups westudy
here.Let us
again
quote the Schwarz theorem[19]
whichis
applicable
tocompact
as well as finite groups : for acompact
groupG,
the G-invariant smooth functions are smooth functions of G-invariantpoly-
nomials. With the use of the
Malgrange
divisiontheorem
[29]
one canjustify expansion
of any G- invariant smooth functions(r)
intowhere
sp’s
are smooth functions of the denominator invariants(however,
not anymoreunique)
while({Jp’s
are the numerator invariants. From an identifi- cation of the spaces of smooth mapsSM(E, E’)
andSM(E* 0 E’, R), equation
39 can be extended to any type of smooth G-covariant field.3. Zeros of covariant vector fields.
We consider a finite
orthogonal
group Gacting
on areal
En.
Given apolynomial
vector fieldv(r),
we want to find its zeros. That
is,
we want to solve for r the system ofequations
We recall that a covariant
polynomial
vector field canbe
expanded
where
ea(r)
are basic(for C[Ol,
...,9n] module)
cova-riant
polynomial
fields.At a
point
ro,by using (40) for g
EL(ro)
and thedefinition of
E;(ro),
we haveimplying v(ro)
is inELn(ro)
and thus in the closure ofE[L(ro)]’ Hence,
at agiven particular point
ro of an m-dimensional stratum there cannot be more than mlinearly independent
basic fieldsea(r 0) (since
G isfinite,
thetopological
dimension m of the stratum isequal
to the dimension of thesubspace E,,L(ro)).
Alsothere cannot be fewer than m. For a
proof,
let n be anarbitrary
unit vector inE;(ro).
Then we can constructa covariant
polynomial
vector field which isalong n
at ro. Such a field is the
gradient
ofF(r), VF(r),
withwhere a is any real number
and
p r p 2 - (r, r).
Since n may be in any one of the mlinearly independent
directions and since each cor-responding
fieldVF(r)
can beexpanded
like equa- tion 42 theproof
iscomplete. Thus,
Theorem 3. 1 Values of basic G-covariant vector fields
(and
also ofgradients
of theintegrity basis)
at rspan
E;(r),
thetangent plane
at r to the stratuml:[L(r)].
The theorem extends to compact groups ifone
replaces EL(r) by
the o invariant slice »(see
e.g.Ref.
26).
Let us denote the m basic vector fields whose/values
are
linearly independent
at r EE;(r) by el(r),..., em(r),
m = dim
E;(r).
Ingeneral, e’(r)
cannot be chosen sothat
they
form aglobal
basis onE[L(r)],
i.e. alinearly independent
set of vectors notonly
at r but every- where onE[L(r)].
Forexample,
in the tables of sec-tion
4,
aglobal
basis does not exist for some strata of the groupsS2m n >
1. Additional discussion of theglobal
basis isgiven
inappendix
A.As
explained
in section 2. 7 ourgoal
is toreplace (41) by
conditions in terms of theintegrity
basisonly.
The rational is that
by going
to the orbit space notonly
do we remove unnecessarydegeneracy
but wesometimes obtain
equations
of lowerdegree
than thosefound
directly
inEn using
e.g. a recent methodby
Jaric
[30].
In order to achieve ourgoal
we first needequations
andinequalities describing
each stratum2;[L]
in orbit space.They
can be foundusing
a methodby
Jaric[28]. Second,
on each stratum the basic fieldse§(r)
need to be determined(we always
choose a basisof the lowest
possible degree). Equation
41 is thenreplaced,
on agiven
stratumE [L], by m
= dimE;
equations
These
equations
can be writtenexplicitly
in terms ofthe
integrity
basisby using (42)
andby calculating explicitly
the nk x nk matrixM(O 1, ..., 8",
({Jl, ...,(Pk - 1)
For closed
subgroups
of0(2)
and0(3)
calculations of the matrix M are illustrated inappendices B,
C and D. The system ofequations
46 can often besimplified
and we
give
in the tables its lowestdegree equivalent.
4. Tables for closed
subgroups
of0(2)
and0(3).
The closed
subgroups
of0(2)
are the Lie groupSO(2)
and the two families of finite groups,
C.
andCnV’
which are
isomorphic
tocyclic
and dihedral groupsZn
andDn.
We use here the usual notation of thephy-
sical and chemical literature
(see
e.g.[31]).
Forinstance, C
andCoot
stand forSO(2)
and0(2), respectively.
Lie
subgroups of SO(3)
areCoo
andD.,
whereas the finitesubgroups
areC,,, Dm T,
0 and Y. The last three are irreducible and leave invariant someregular polyhedra :
tetrahedron forT,
cube and octahedron for0,
icosahedron and dodecahedron for Y. It is well known thatsubgroups
of0(3)
can be obtainedfrom those of
SO(3) by adding
thespatial
inversion( - I)
in one of two ways :Table Ia. - Two-dimensional
point
groups(G) :
Denominator
(0i)
and numerator(¡Jp)
invariants and basic vectorfields (eO’).
Cartesian coordinates x and yare chosen so that the
origin
is afixed point
and thex-axis is a
reflection
axis.i and j
denote the unit vectors in the x and y directionsrespectively.
The radius vector is p =xi
+yj, p2
=X2
+y2.
Otherquantities
enter-ing
the table aredefined as follows :
yn = Re(x
+iy)n ;
U n = 1m
(x
+iy)n ; Jp = - yi
+xl
Table lb. - Two-dimensional
point
groups(G) :
Classes
of
little groups([L]),
relationsdetermining corresponding
stratum(2:[LI)
and theglobal
basis onE’ (ea).
The relations aregiven
in termsof
invariants;the relations necessary in orbit space, but redundant in the carrier space, are enclosed in
curly
brackets. Forthe group
Cn,
the last rowgives
analgebraic
relationsatisfied
on each stratumby
the non-trivial numerator invariant. See table Iafor definitions of
the invariantsand the
vector fields.
(Q)
For n odd the two classes,[CS(+]
and[Cs(-)],
coincide;for n even they are
disjoint
and ’ correspond to02
=on/2.
(b)
dim 2;[L], when different from dimE2,
is given inparentheses.
.0
Table Ic. - Two-dimensional
point
groups(G) :
Zeros
of
ageneral
vectorfield
v =1’(1 Q(1(O)
e(1 at eachstratum
1’[L].
The basicfields
and relations determin-ing
the strata aregiven
in tables la and Ibrespectively.
A dash in the last column indicates that v = 0 reduces
to an
identity.
i)
From a group HSO(3), generate
G = H u(- I)
H0(3)
which isisomorphic
to H xZ2.
Inthis fashion one finds
Coo’" D ooh, S2n
andDnd (n odd), Cnh
andDnh (n even), Th, Oh
andYh.
ii)
From a group HSO(3)
which has asubgroup
K
of
index two generate a group G0(3) isomorphic
to H