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comment by user-inactivated
user-inactivated  ·  1735 days ago  ·  link  ·    ·  parent  ·  post: Space fans of Hubski - Why don't moons ever have moons of their own?

    the lunar gravity field is 'lumpy' and not smooth; satellites in orbit at low altitude will become unstable quickly.

Interesting. Is this true for all moons, or just ours? Is it shape dependent, for example are the gravity fields of Mars' potato moons even lumpier?

    Knowing whether that is true or not may have to wait for discoveries of moons orbiting distant exoplanets. Moons themselves are much harder to detect and only one promising candidate has been found so far – a possible exomoon orbiting the Jupiter-sized exoplanet Kepler-1625b. That possible moon – about the size of Neptune – is large enough and far enough from its planet that submoons should be possible as well. Astronomers will need to verify that primary moon first – if it does exist – before looking for any submoons.

Dala was telling me about binary planets again last night, where the center of gravity is between two planets and not in a planet, like Pluto and its moon. That exo planet and its possible moon are so massive, I wonder if they might actually be binary planets too . . .





user-inactivated  ·  1734 days ago  ·  link  ·  
This comment has been deleted.
user-inactivated  ·  1733 days ago  ·  link  ·  

Gravity is space turbulence. :)

Devac  ·  1735 days ago  ·  link  ·  

    Interesting. Is this true for all moons, or just ours? Is it shape dependent, for example are the gravity fields of Mars' potato moons even lumpier?

It's true for anything that's not a perfect sphere or having a homogenous (the same in all directions) distribution of mass. Forgetting about things like mountain ranges and other topographical features, the simple fact that the Earth rotates makes the equatorial radius larger than the pole radius, so it's already not a perfect sphere. Then you have to account for things like continental plates being lighter than oceanic plates, which (probably) isn't as significant as the convective movement of magma below the crust (which complicates things even further).