next up previous contents
Next: Perihelion Precession of Mercury Up: Gravitational Potential Theory Previous: Potential Due to a   Contents

Perihelion Precession of the Planets

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 $M_i$ and the $R_i$, for $i=1,8$, be the planetary masses and orbital radii, respectively. Furthermore, let $M_0$ be the mass of the Sun. It follows, from the previous subsection, that the gravitational potential generated at the $i$th planet by the Sun and the other planets is

$\displaystyle \Phi(R_i)$ $\textstyle =$ $\displaystyle -\frac{G\,M_0}{R_i}-G \sum_{j< i}\frac{M_j}{R_i}\left[1+\frac{1}{...
...c{R_j}{R_i}\right)^2 + \frac{9}{64}\left(\frac{R_j}{R_i}\right)^4+\cdots\right]$  
    $\displaystyle -G \sum_{j> i}\frac{M_j}{R_j}\left[1+\frac{1}{4}\left(\frac{R_i}{R_j}\right)^2 + \frac{9}{64}\left(\frac{R_i}{R_j}\right)^4+\cdots\right].$ (1049)

Now, the radial force per unit mass acting on the $i$th planet is written $f(R_i) = - d\Phi(R_i)/dr$, giving
$\displaystyle f(R_i)$ $\textstyle =$ $\displaystyle -\frac{G\,M_0}{R_i^{\,2}}-\frac{G}{R_i^{\,2}} \sum_{j< i}M_j\left...
...R_j}{R_i}\right)^2
+ \frac{45}{64}\left(\frac{R_j}{R_i}\right)^4 +\cdots\right]$  
    $\displaystyle +\frac{G}{R_i^{\,2}} \sum_{j> i}M_j\,\left(\frac{R_i}{R_j}\right)...
...c{R_i}{R_j}\right)^2+ \frac{9}{16}\left(\frac{R_i}{R_j}\right)^4+\cdots\right].$ (1050)

Hence, we obtain
$\displaystyle R_i\,f'(R_i)$ $\textstyle =$ $\displaystyle \frac{2\,G\,M_0}{R_i^{\,2}}+\frac{G}{R_i^{\,2}} \sum_{j< i}M_j\le...
...R_j}{R_i}\right)^2
+ \frac{135}{32}\left(\frac{R_j}{R_i}\right)^4+\cdots\right]$  
    $\displaystyle + \frac{G}{R_i^{\,2}}\,\sum_{j> i}M_j\,\left(\frac{R_i}{R_j}\righ...
...{R_i}{R_j}\right)^2+ \frac{27}{16}\left(\frac{R_i}{R_j}\right)^4+\cdots\right],$ (1051)

where $'\equiv d/dr$. It follows that
$\displaystyle \left[3 + \frac{R_i\,f'(R_i)}{f(R_i)}\right]^{-1/2}$ $\textstyle =$ $\displaystyle 1 + \frac{3}{4}\sum_{j<i}\left(\frac{M_j}{M_0}\right)
\left(\frac...
..._j}{R_i}\right)^2 + \frac{175}{64}\left(\frac{R_j}{R_i}
\right)^4+\cdots\right]$  
    $\displaystyle + \frac{3}{4}\sum_{j>i}\left(\frac{M_j}{M_0}\right)
\left(\frac{R...
...i}{R_j}\right)^2 + \frac{175}{64}\left(\frac{R_i}{R_j}
\right)^4+\cdots\right].$  
      (1052)

Thus, according to Eq. (388), the apsidal angle for the $i$th planet is
$\displaystyle \psi_i$ $\textstyle =$ $\displaystyle \pi\left\{1 + \frac{3}{4}\sum_{j<i}\left(\frac{M_j}{M_0}\right)
\...
...}\right)^2 + \frac{175}{64}\left(\frac{R_j}{R_i}
\right)^4+\cdots\right]\right.$  
    $\displaystyle \left.+ \frac{3}{4}\sum_{j>i}\left(\frac{M_j}{M_0}\right)
\left(\...
...right)^2 + \frac{175}{64}\left(\frac{R_i}{R_j}
\right)^4+\cdots\right]\right\}.$  
      (1053)

Hence, the perihelion of the $i$th planet advances by
$\displaystyle \delta\psi_i$ $\textstyle =$ $\displaystyle \frac{3\pi}{2}\sum_{j<i}\left(\frac{M_j}{M_0}\right)
\left(\frac{...
..._j}{R_i}\right)^2 + \frac{175}{64}\left(\frac{R_j}{R_i}
\right)^4+\cdots\right]$  
    $\displaystyle + \frac{3\pi}{2}\sum_{j>i}\left(\frac{M_j}{M_0}\right)
\left(\fra...
..._i}{R_j}\right)^2 + \frac{175}{64}\left(\frac{R_i}{R_j}
\right)^4+\cdots\right]$  
      (1054)

radians per revolution around the Sun. Now, the time for one revolution is $T_i = 2\pi/\omega_i$, where $\omega_i^{\,2} = G\,M_0/R_i^{\,3}$. Thus, the rate of perihelion precession, in arc seconds per year, is given by
$\displaystyle \delta\dot{\psi}_i$ $\textstyle =$ $\displaystyle \frac{75}{T_i({\rm yr})}\left\{\sum_{j<i}\left(\frac{M_j}{M_0}\ri...
...}\right)^2 + \frac{175}{64}\left(\frac{R_j}{R_i}
\right)^4+\cdots\right]\right.$  
    $\displaystyle \left.+ \sum_{j>i}\left(\frac{M_j}{M_0}\right)
\left(\frac{R_i}{R...
...right)^2 + \frac{175}{64}\left(\frac{R_i}{R_j}
\right)^4+\cdots\right]\right\}.$  
      (1055)


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 $M/M_0$ $T({\rm yr})$ R( au)
Mercury $1.66\times 10^{-7}$ $0.241$ $0.387$
Venus $2.45\times 10^{-6}$ $0.615$ $0.723$
Earth $3.04\times 10^{-6}$ $1.000$ $1.00$
Mars $3.23\times 10^{-7}$ $1.881$ $1.52$
Jupiter $9.55\times 10^{-4}$ $11.86$ $5.20$
Saturn $2.86\times 10^{-4}$ $29.46$ $9.54$
Uranus $4.36\times 10^{-5}$ $84.01$ $19.19$
Neptune $5.18\times 10^{-5}$ $164.8$ $30.07$



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 $(\delta\dot{\Psi})_{obs}$ $(\delta\dot{\Psi})_{th}$
Mercury $5.75$ $5.50$
Venus $2.04$ $10.75$
Earth $11.45$ $11.87$
Mars $16.28$ $17.60$
Jupiter $6.55$ $7.42$
Saturn $19.50$ $18.36$
Uranus $3.34$ $2.72$
Neptune $0.36$ $0.65$


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.
\begin{figure}
\epsfysize =3.5in
\centerline{\epsffile{prec.eps}}
\end{figure}

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 ($e=0.0068$), which renders its perihelion point extremely sensitive to small perturbations.


next up previous contents
Next: Perihelion Precession of Mercury Up: Gravitational Potential Theory Previous: Potential Due to a   Contents
Richard Fitzpatrick 2008-01-13