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Let
be a compact Lie group and suppose that
acts on the finite
dimensional real vector space V as a group of real linear
transformations. In the sequel we refer to
,
or just V,
as a (group) representation.
Remark 2.1
Every closed subgroup

of the orthogonal group
O(
n) defines
an `orthogonal' representation

.
Conversely,
every representation is isomorphic to an orthogonal representation.

Our interest lies in differential equations or vector fields which are defined on
V and which are symmetric relative to the given
-action. Thus if
is a smooth vector field on V, we say that X is
-equivariant if
The assumption of equivariance implies strong restrictions on the phase portrait
of (
).
For example, it follows from the uniqueness of solutions
of ordinary differential equations that if
is an integral curve of (
), then so is
,
all
.
(Thus
acts
on the phase portrait by permuting maximal integral curves.)
The assumption that the group
acts on V, implies that not
all points in V are `equal': some are more symmetric than others. We quantify this
idea of symmetry of a point by defining the isotropy group of the
action at a point of V. Specifically, if
,
we define the isotropy group
at
x by
The isotropy group
is always a closed (therefore Lie)
subgroup of
.
We think of
as measuring the
symmetry of the point x (with respect to the given action of
).
Viewed in this way, the origin always has maximal symmetry since
.
We say that
a point
has trivial symmetry if
consists only of the identity
element of
.
It turns out that for
`most' representations
,
an open and dense set of
points will have only the trivial symmetry. Thus, for a point to have
nontrivial symmetry is exceptional rather than the norm.
Example 2.2
Figure:
Isotropy for action by
D4
 |
In Figure
![[*]](cross_ref_motif.png)
, we show the symmetries of points in the plane for the standard
action of the dihedral group
D4.
The group
D4 consists of reflections in the lines

together with
the cyclic group

generated by rotation through

.
Nonzero points on the
lines

all have isotropy group isomorphic to

.
All other nonzero
points in the plane have trivial isotropy.

Using equivariance,
together with the smooth dependence of integral curves on initial conditions,
it is easy to see that isotropy groups are constant along maximal integral curves of (
).
This apparently innocuous observation about isotropy along integral curves
has the significant and surprising consequence that V contains
subsets which are flow-invariant for all equivariant vector fields.
Example 2.3
Suppose that
X is a smooth
D4-equivariant vector field defined on

,
where
we take the action of
D4 given in Example
![[*]](cross_ref_motif.png)
. Let
Abe the open wedge shaped region shown in Figure
![[*]](cross_ref_motif.png)
and suppose that

.
Let
C be the maximal integral curve through
x0.
Since
x0 has trivial isotropy, all points of
C must have trivial
isotropy. It follows that
C is a subset of
A, for otherwise
Cwould have to contain points on one of the lines
m,
q. Hence
A is a flow-invariant
subset of

for
all
D4-equivariant vector fields on

.
Similar arguments show that the lines

and the origin are also
flow-invariant subspaces.

Next: The flow-invariant subspaces of
Up: Heteroclinic cycles in symmetrically
Previous: Introduction
Mike Field
1998-10-01