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The Solar System consists of eight major planets (Mercury to Neptune) moving around the Sun in slightly elliptical orbits which are approximately
co-planar with one another. According to Sect. 6, if we neglect the relatively weak interplanetary
gravitational interactions then the perihelia of the various planets (i.e., the points on their orbits at which they are closest to the Sun) remain fixed in space. However, once these
interactions are taken into account, it turns out that the planetary perihelia all
slowly precess around the Sun. We can calculate the approximate rate of perihelion precession
of a given planet by treating the other planets as uniform concentric rings, centered on the Sun, of mass equal to the planetary mass, and
radius equal to the mean orbital radius. This is equivalent to averaging the interplanetary gravitational interactions
over the orbits of the other planets. It is reasonable to do this, since the precession period in question is
very much longer than the orbital period of any planet in the Solar System. Thus, by treating the other planets as
rings, we can calculate the mean gravitational perturbation due to these planets, and, thereby, determine the
desired precession rate.
We can conveniently index the planets in the Solar System such that Mercury is planet 1, and Neptune planet 8. Let the
and the
, for
, be the planetary masses and orbital radii, respectively. Furthermore, let
be the mass of the Sun.
It follows, from the previous subsection, that the gravitational potential generated at the
th planet by the Sun and
the other planets is
Now, the radial force per unit mass acting on the
th planet is written
, giving
Hence, we obtain
where
. It follows that
Thus, according to Eq. (388), the apsidal angle for the
th planet is
Hence, the perihelion of the
th planet advances by
radians per revolution around the Sun. Now, the time for one revolution is
, where
. Thus, the rate of perihelion precession, in arc seconds per year, is given by
Table 1:
Solar-system data giving the planetary masses relative to that
of the Sun, the orbital periods in years, and the mean orbital
radii relative to that of the Earth.
| Planet |
 |
 |
R( au) |
| Mercury |
 |
 |
 |
| Venus |
 |
 |
 |
| Earth |
 |
 |
 |
| Mars |
 |
 |
 |
| Jupiter |
 |
 |
 |
| Saturn |
 |
 |
 |
| Uranus |
 |
 |
 |
| Neptune |
 |
 |
 |
|
Table 2:
The observed perihelion precession rates of the planets (from the JPL Solar System
Dynamics web-site) compared with the theoretical precession rates calculated from Eq. (1056)
and Tab. 1. The precession rates are given in arc seconds per year.
| Planet |
 |
 |
| Mercury |
 |
 |
| Venus |
 |
 |
| Earth |
 |
 |
| Mars |
 |
 |
| Jupiter |
 |
 |
| Saturn |
 |
 |
| Uranus |
 |
 |
| Neptune |
 |
 |
|
Figure 60:
The triangular points show the observed perihelion precession rates of the
major planets in the Solar System, whereas the square points show the theoretical
rates calculated above. All precession rates are in arc seconds per
year.
 |
Table 2 and Fig. 60 compare the observed perihelion precession rates
with the theoretical rates calculated from Eq. (1056)
and the planetary data given in Tab. 1. It can be seen that there is excellent agreement
between the two, except for the planet Venus. The main reason for this is because Venus
has an unusually low eccentricity (
), which renders its perihelion point extremely sensitive to small perturbations.
Next: Perihelion Precession of Mercury
Up: Gravitational Potential Theory
Previous: Potential Due to a
Contents
Richard Fitzpatrick
2008-01-13