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Our planet's radial equation of motion, (303), can be combined with
Eq. (322) to give
 |
(325) |
Suppose that
. It follows that
 |
(326) |
Likewise,
 |
(327) |
Hence, Eq. (325) can be written
 |
(328) |
The general solution to the above equation takes the form
![\begin{displaymath}
u(\theta) = \frac{G\,M}{h^2}\left[1 - e\,\cos(\theta-\theta_0)\right],
\end{displaymath}](img995.png) |
(329) |
where
and
are arbitrary constants. Without loss of generality, we can
set
by rotating our coordinate system about the
-axis. Thus,
we obtain
 |
(330) |
where
 |
(331) |
We immediately recognize Eq. (330) as the equation of a conic
section which is confocal with the origin (i.e., with the Sun).
Specifically, for
, Eq. (330) is the equation of an ellipse
which is confocal with the Sun. Thus, the orbit of our planet
around the Sun in a confocal ellipse--this is Kepler's first law
of planetary motion. Of course, a planet cannot have a parabolic
or a hyperbolic orbit, since such orbits are only appropriate to objects which are ultimately able to escape from the Sun's gravitational field.
Next: Kepler's Third Law
Up: Planetary Motion
Previous: Kepler's Second Law
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Richard Fitzpatrick
2008-01-13