The most common set of orbital elements used to parameterize Keplerian orbits consists of the major radius, ; the mean longitude at epoch,
; the eccentricity, ;
the inclination (relative to some reference plane), ; the longitude of the perihelion,
; and the longitude of the ascending node,
. (See Section 4.12.) The mean orbital angular velocity is
[see Equation (4.117)].
Consider how a particular Lagrange bracket transforms under
a rotation of the coordinate system , , about the -axis (if we look along the axis).
We can write
|
(G.41) |
where
|
(G.42) |
Let the new coordinate system be
. A rotation about the
-axis though an angle
brings the ascending node to the -axis. See Figure 4.6.
The relation between the old and new coordinates is (see Section A.6)
The partial derivatives with respect to can be written
|
|
(G.46) |
|
|
(G.47) |
|
|
(G.48) |
|
|
(G.49) |
where
|
|
(G.50) |
|
|
(G.51) |
|
|
(G.52) |
|
|
(G.53) |
Let , , , and be the equivalent quantities
obtained by replacing by in the preceding equations.
It thus follows that
Hence,
|
(G.56) |
Now,
Similarly,
Let
|
(G.59) |
Because and
, it follows that
However,
|
(G.61) |
because the left-hand side is the component of the angular momentum per unit mass parallel to
the -axis. Of course, this axis is inclined at an angle
to the -axis, which is parallel to the angular momentum vector.
Thus, we obtain
|
(G.62) |
Consider a rotation of the coordinate system about the -axis. Let the
new coordinate system be , , . A rotation through an
angle brings the orbit into the - plane. See Figure 4.6.
Let
|
(G.63) |
By analogy
with the previous analysis,
|
(G.64) |
However, and are both zero, because the orbit lies
in the - plane. Hence,
|
(G.65) |
Consider, finally, a rotation of the coordinate system about the -axis. Let the
final coordinate system be , , . A rotation through an angle
brings the perihelion to the -axis. See Figure 4.6.
Let
|
(G.66) |
By analogy with the previous analysis,
|
(G.67) |
However,
|
(G.68) |
so, from Equations (G.62) and (G.65),
|
(G.69) |
It thus remains to calculate
.
The coordinates
and
—where represents radial distance from the Sun, and
is the true anomaly—are functions of the major radius, ,
the eccentricity, , and the mean anomaly,
.
Because the Lagrange brackets
are independent of time, it is sufficient to evaluate them at
; that is, at the perihelion point. It is easily
demonstrated from Equations (4.86) and (4.87) that
|
|
(G.70) |
|
|
(G.71) |
|
|
(G.72) |
|
|
(G.73) |
at small . Hence, at
,
|
|
(G.74) |
|
|
(G.75) |
|
|
(G.76) |
|
|
(G.77) |
|
|
(G.78) |
|
|
(G.79) |
because
. All other partial derivatives are zero.
Because the orbit in the , , coordinate system only
depends on the elements , , and
, we
can write
Substitution of the values of the derivatives evaluated at
into this expression yields
and
|
(G.84) |
where
.
Hence, from Equation (G.69), we obtain
|
(G.85) |