64 Chapter 4 Classification of Planar Systems
A couple of remarks are in order. First, the trace-determinant plane is a
two-dimensional representation of what is really a four-dimensional space,
since 2 × 2 matrices are determined by four parameters, the entries of the
matrix. Thus there are infinitely many different matrices corresponding to each
point in the TD–plane. While all of these matrices share the same eigenvalue
configuration, there may be subtle differences in the phase portraits, such as the
direction of rotation for centers and spiral sinks and sources, or the possibility
of one or two independent eigenvectors in the repeated eigenvalue case.
We also think of the trace-determinant plane as the analog of the bifurcation
diagram for planar linear systems. A one-parameter family of linear systems
corresponds to a curve in the TD–plane. When this curve crosses the T -axis,
the positive D-axis, or the parabola T
2
− 4D = 0, the phase portrait of the
linear system undergoes a bifurcation: A major change occurs in the geometry
of the phase portrait.
Finally, note that we may obtain quite a bit of information about the system
from D and T without ever computing the eigenvalues. For example, if D<0,
we know that we have a saddle at the origin. Similarly, if both D and T are
positive, then we have a source at the origin.
4.2 Dynamical Classification
In this section we give a different, more dynamical classification of planar linear
systems. From a dynamical systems point of view, we are usually interested
primarily in the long-term behavior of solutions of differential equations.
Thus two systems are equivalent if their solutions share the same fate. To
make this precise we recall some terminology introduced in Section 1.5 of
Chapter 1.
To emphasize the dependence of solutions on both time and the initial con-
ditions X
0
, we let φ
t
(X
0
) denote the solution that satisfies the initial condition
X
0
. That is, φ
0
(X
0
) = X
0
. The function φ(t , X
0
) = φ
t
(X
0
) is called the flow of
the differential equation, whereas φ
t
is called the time t map of the flow.
For example, let
X
=
20
03
X.
Then the time t map is given by
φ
t
(x
0
, y
0
) =
x
0
e
2t
, y
0
e
3t
.
Thus the flow is a function that depends on both time and the initial values.