"From Stargazers to Starships" home page and index: on disk Sintro.htm, on the web
          http://www.phy6.org/stargaze/Sintro.htm

• Become familiar with graphs of the form r = F(φ) in polar coordinates (r, φ), in particular with the circle, ellipse and other conic sections.

• Will understand the role of the semimajor axis and eccentricity in determining the nature of an ellipse.

• Will understand that the fixed point in any planetary system is its center of gravity. (This is used in a later section in deriving the rocket principle).

Terms: Focus (of ellipse), eccentricity, semi-major axis, orbital elements, mean anomaly (qualitatively only), center of gravity.

Stories and extras: Method used in the search for other planetary systems, and the recently discovered planetary system of Upsilon Andromeda. "Alien Planets" (Skepl1stA.htm) gives further details about such searches, and how the transit of a planet in front of a star could give clues about whether the planet is a gas giant or icy or rocky.

(Suggested answers in parentheses, brackets for comments by the teacher or "optional")

   Start the lesson by reviewing polar coordinates. Then point out that in cartesian coordinates (preceding lesson) the ellipse is symmetric--around the axes and around their crossing point.

   The motion of a planet of a satellite in an elliptic orbit is not symmetric--the center of motion, the focus, is shifted towards one end, and the planet's distance from it goes up and down each orbit, like a wave.

    It suggests that cartesian coordinates are not the most suitable for handling orbits--and that, in fact, turns out to be the case. Polar coordinates, centered on the focus of the ellipse, are more suitable. As will be seen, the wave-like dependence of the distance is then clearly seen as a result of the wave-like variation of the cosine of the polar angle.

    Then present section 11b of "Stargazers," up to "Refining the First Law". Discuss the material, guided by the questions below, and conclude with "Refining the First Law" and its questions, as listed further below.

-- If a cartesian system (x,y) has the same origin as a polar system, and the reference line from which φ is measured in the polar system is the x axis--given (r,φ) of a point, what are its (x,y)?

x = r cos φ          y = r sin φ.

r² = x² + y².

[tan φ = y/x]

[Note in this section we denoted the polar angle by f, not by φ, because that is the notation used in the study of orbits. We will use capital F(f) for "a function of f" that is, "some expression involving f". ]

r = F(f) is one way.

[More generally, any expression F(r,f) involving (r,f)) can be used, for example in the form F(r,f) = a, where a is some number or zero. The important thing is that at least over some range, each f has some corresponding value of r--sometimes, more than one value.

For instance,the line

         3 r sin(f) – 2 r cos(f) = 10

What sort of line is it? Don't panic! It is just a straight line, as you easily see once you convert it to cartesian coordinates, using the relations developed earlier for the (r, φ) notation.

A constant number R, equal to the radius. Then r = R for any value of f.

[This is similar to the straight line y = 3. On that line, the value of y is the same for any x, and therefore the value of x does not have to appear.]

A number between 0 and 1, known as the eccentricity of the ellipse.

Smallest for f=0, cos f =1; biggest for f=180°, cos f = -1.

         r = a(e-1)(e+1)/(1 + e cos f)

[The class should know this identity, or else, it may be proven on the board.]
Using that form, what are the biggest and smallest value of r?

A student or the teacher derive these on the board: biggest a(1+e), smallest a(1-e).

[Optional: Draw on the board an ellipse, around its focus, and on it, show the biggest and smallest r.
    If this is the elliptic orbit of an Earth satellite, the smallest and biggest distances are know as perigee and apogee, where "gee" stands for "geo", the Earth.
   For planets orbiting the Sun, these are called the perihelion and aphelion, from "helios", the Sun.]

It is the sum of the smallest and biggest distances: a(1+e) + a(1-e) = 2a.

They are quantities used to define an orbit.

The semi-major axis a and the eccentricity e

a is the radius, e is zero.

The semi-major axis a is the precise meaning of the "mean distance" we used earlier. The square of the orbital period T is proportional to the third power (cube) of the semi-major axis.

Six elements exist: a and e define the orbital ellipse, the mean anomaly M is an angle that defines the satellite's position along that ellipse and 3 additional angles define the orientation of the orbital ellipse in 3-dimensional space.

[We can extend the equation of an ellipse to e = 1 or even e > 1, but must be careful. Suppose we draw a series of ellipses, of increasing e, all with the same minimum distance a(1-e). Then as e approaches 1, the semimajor axist grows to be larger and larger.

   With e=1, we have something infinite (a) multiplying something that is zero (1-e). We thus need to rewrite the equation in the form r = p/(1 + e cosf) With e = 1 this gives a parabola, with e>1, a hyperbola.]

Neither--each rotates around its commen center of gravity.

Planets are too dim and too close to their suns to be seen by today's telescopes. However, each such sun also moves, around the joint center of gravity of it and of its planets. For instance, with just one planet, the Sun is always on the opposite side of the center of gravity.
Therefore, if astronomers see a slight wobble in the position of a distant star, they may deduce from it the existence and motion of its planets.

Very difficult, except perhaps for planets of M-class red dwarf stars, if their orbit happens to intersect the sun-star line. We can estimate the distance to the star, and then know the energy output of the star from its brightness (also its color), and the radius of the planet's orbit from its period. So we can tell if water might be liquid there, and also estimate the mass of the star.

    If the planet "transits" in front of the star, the dimming is proportional to the cross-sectional area of the planet, telling about the radius of the planet. From the wobble of the star's position we have the planet's mass, so these two give an estimate of the planet's density, allowing gaseous planets and solid ones to be told apart.