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Formation of Regular Satellites from Ancient Massive Rings in the Solar System
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Formation of Regular Satellites from Ancient Massive Rings in the Solar System
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When a planetary tidal disk -like Saturn's rings- spreads beyond the Roche radius (inside which planetary tides prevent aggregation), satellites form and migrate away. Here, we show that most regular satellites in the solar system probably formed in this way. According to our analytical model, when the spreading is slow, a retinue of satellites appear with masses increasing with distance to the Roche radius, in excellent agreement with Saturn's, Uranus', and Neptune's satellite systems. This suggests that Uranus and Neptune used to have massive rings that disappeared to give birth to most of their regular satellites. When the spreading is fast, only one large satellite forms, as was the case for Pluto and Earth. This conceptually bridges the gap between terrestrial and giant planet systems.
Forward citations
Cited by 2 Pith papers
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Tidal evolution of packed moon systems around an Earth-mass planet
Including tidal migration cuts the maximum stable moon count around an Earth-mass planet to about two Moon-sized, three Pluto-sized, or five Ceres-sized moons, confined to narrow orbital-spacing windows.
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Ring formation around giant planets by tidal disruption of a single passing large Kuiper belt object II: The dynamical fate of tidal fragments
N-body simulations show tidal fragments form narrow circular equatorial rings around Saturn for low-to-moderate inclinations with radius set by vertical angular momentum conservation, while high inclinations cause mos...
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