Next: Lunar Motion
Up: Three-Body Problem
Previous: Zero-Velocity Surfaces
We have seen that the five Lagrange points,
to
, are the equilibrium points
of mass
in the co-rotating frame. Let us now determine whether or not
these equilibrium points are stable to small displacements.
Now, the equations of motion of mass
in the co-rotating frame are
specified in Equations (558)-(560). Note that the motion
in the
-
plane is complicated by presence of the Coriolis acceleration. However, the motion parallel to the
-axis simply
corresponds to motion in the potential
. Hence, the condition for
the stability of the Lagrange points (which all lie at
) to small displacements parallel
to the
-axis is simply (see Section 2.7)
 |
(598) |
This condition is satisfied everywhere in the
-
plane. Hence, the Lagrange points are all
stable to small displacements parallel to the
-axis. It, thus, remains to investigate
their stability to small displacements lying within the
-
plane.
Suppose that a Lagrange point is situated in the
-
plane at coordinates
.
Let us consider small amplitude
-
motion in the vicinity of this point by writing
where
and
are infinitesimal. Expanding
about the Lagrange point as a Taylor series, and retaining terms up to second-order in small
quantities, we obtain
 |
(602) |
where
,
,
,
etc. However, by definition,
at a Lagrange point, so the expansion simplifies to
 |
(603) |
Finally, substitution of Equations (599)-(601), and (603)
into the equations of
-
motion, (558) and (559), yields
since
.
Let us search for a solution of the above pair of equations
of the form
and
. We obtain
![\begin{displaymath}
\left(
\begin{array}{cc}
\gamma^2 + U_{xx}& -2\,\gamma+U_{xy...
... = \left(
\begin{array}{c}
0\\ [0.5ex]
0
\end{array}\right).
\end{displaymath}](img1602.png) |
(606) |
This equation only has a non-trivial solution if the determinant of the
matrix is zero. Hence, we get
 |
(607) |
Now, it is convenient to define
where all terms are evaluated at the point
. It thus follows that
Consider the co-linear Lagrange points,
,
, and
. These all
lie on the
-axis, and are thus characterized by
,
, and
. It follows,
from the above equations, that
and
. Hence,
,
, and
. Equation (607) thus yields
 |
(615) |
where
. Now, in order for a Lagrange point to be stable
to small displacements, all four of the roots,
, of Equation (607) must
be purely imaginary. This, in turn, implies that the two roots of
the above equation,
 |
(616) |
must both be real and negative.
Thus, the stability criterion is
 |
(617) |
Figure 32 shows
calculated at the three co-linear Lagrange points as a function of
, for all
allowed values of this parameter (i.e.,
). It can be seen that
is always greater than unity for all three points. Hence, we conclude that the co-linear
Lagrange points,
,
, and
, are intrinsically unstable equilibrium points in the co-rotating
frame.
Figure 32:
The solid, short-dashed, and long-dashed curves show
as a function of
at the
,
, and
Lagrange points.
 |
Let us now consider the triangular Lagrange points,
and
. These points
are characterized by
. It follows that
,
,
,
and
. Hence,
,
, and
,
where the upper/lower signs corresponds to
and
, respectively.
Equation (607) thus yields
 |
(618) |
for both points,
where
. As before, the stability criterion is that the two roots of the
above equation must both be
real and negative. This is the case provided that
, which
yields the stability criterion
 |
(619) |
In unnormalized units, this criterion becomes
 |
(620) |
We thus conclude that the
and
Lagrange points are stable equilibrium
points, in the co-rotating frame, provided that mass
is less than about
of
mass
. If this is the case then mass
can orbit around these points
indefinitely. In the inertial frame, the mass will share
the orbit of mass
about mass
, but will stay approximately
ahead of
mass
, if it is orbiting the
point, or
behind, if it is orbiting the
point--see Figure 31. This type of behavior has been observed in the Solar System. For instance,
there is a sub-class of asteroids, known as the Trojan asteroids, which are trapped
in the vicinity of the
and
points of the Sun-Jupiter system [which easily
satisfies the stability criterion (620)], and consequently share Jupiter's orbit around the Sun,
staying approximately
ahead of, and
behind, Jupiter, respectively.
Furthermore, the
and
points of the Sun-Earth system are occupied by clouds of dust.
Next: Lunar Motion
Up: Three-Body Problem
Previous: Zero-Velocity Surfaces
Richard Fitzpatrick
2011-04-22