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We need to remember that Kepler had no dynamic theory of what was going on here. This was an empirical kinematic exercise on the special case of planets orbiting the Sun.
I don't know whether or not he did a similar exercise on Jupiter's moons. Such an exercise would yield a similar equation relating the orbital period and radius, but with a different proportionality constant. The general case would be of the form P2 = KR3, with Jupiter's K being about 1,000 times that of the Sun. As a result of Newton's work we now know that K = 1/M, where M is the mass of the primary object. |
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Somewhat more pedantically, the value of the constant in Kepler's third law scales with the inverse of (Msun + Mplanet) for each planet, which is always within a range of 0.1%. An additional small effect comes from the fact that the masses of planets interior to the one considered also ad to the net force on its orbit in a time-averaged sense. This is a huge effect for distributed systems such as galaxies, but again doesn't matter at the 0.1% level in the Solar System.
Kepler did find that the Galilean satellites of Jupiter followed the same pattern with a different constant, using data Galileo set him. (I suspect Galileo was frustrated by the same thing that frustrates some of my students when I set them this exercise - they have similar brightnesses, and we usually see their orbits from nearly their common plane, so its a real chore to keep track of which one is which unless you have frequent position measurements). |
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Because no one had calculated them prior to that time.
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Although it may not be exactly analogous. If a planet is always closer to the sun than you are, then it must always be pulling you at least a little in the direction of the sun. But if a planet is farther away, sometimes it will be pulling you towards the sun (when it is on the other side), and sometimes it will be pulling you away (when it is on the same side and behind you).
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When Jupiter is at quadrature, the gravitational acceleration vectors of Earth and Sun are of equal magnitude, but are angled inward. This would give the illusion of strengthening the Earth-Sun gravitational attraction. I think the average effect over a complete revolution is a subtraction, but I am not absolutely sure. |
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Arg, I hate it when that happens
![]() Yes, I was considering the sun to be so massive that its movement would be unaffected by the other planets, but that's not appropriate if we are considering the affect of one planet on another ![]()
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A spherical shell outside an orbit has no effect whatsoever on an orbit. This is because of Gauss theorem. Or else, an area and therefore the mass of a spherical shell is proportional to the square of distance, and since gravitational attraction is proportional to inverse square, the opposite portions of a spherical shell cancel exactly.
But an uniform ring does have a gravitational effect inside. The length and mass are proportional to distance, so a nearer part of the ring will exert stronger attraction. Does the effect of a ring differ from that of a planet orbiting the same path? |
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If you gave more details of your ring, compared to a planet, maybe that'll answer both my questions and Arnold Layne's |
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1) a ring with mass uniformly distributed along its circumference 2) a point planet with the same total mass as 1), orbiting on the same path as the ring did 3) a point planet with the exact same mass and orbit as in 2), but orbiting in the opposite direction. How different are the effects? |
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Yes. Tycho's data was accurate and respected enough in Kepler's view to discover the ellipitical orbit as the solution. This also ended the idea of uniform motion around the orbit. This probably got him going on finding the relationship between period and distance, which he did discover.
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