Did Saturn's rings form during the Late Heavy Bombardment ?
arXiv:0809.5073 · doi:10.1016/j.icarus.2008.10.019
Abstract
The origin of Saturn\' s massive ring system is still unknown. Two popular scenarios - the tidal splitting of passing comets and the collisional destruction of a satellite - rely on a high cometary flux in the past. In the present paper we attempt to quantify the cometary flux during the Late Heavy Bombardment (LHB) to assess the likelihood of both scenarios. Our analysis relies on the so-called Nice model of the origin of the LHB (Tsiganis et al., 2005; Morbidelli et al., 2005; Gomes et al., 2005) and on the size distribution of the primordial trans-Neptunian planetesimals constrained in Charnoz & Morbidelli (2007). We find that the cometary flux on Saturn during the LHB was so high that both scenarios for the formation of Saturn rings are viable in principle. However, a more detailed study shows that the comet tidal disruption scenario implies that all four giant planets should have comparable ring systems whereas the destroyed satellite scenario would work only for Saturn, and perhaps Jupiter. This is because in Saturnś system, the synchronous orbit is interior to the Roche Limit, which is a necessary condition for maintaining a satellite in the Roche zone up to the time of the LHB. We also discuss the apparent elimination of silicates from the ring parent body implied by the purity of the ice in Saturn \' s rings. The LHB has also strong implications for the survival of the Saturnian satellites: all satellites smaller than Mimas would have been destroyed during the LHB, whereas Enceladus would have had from 40% to 70% chance of survival depending on the disruption model. In conclusion, these results suggest that the LHB is the sweet moment for the formation of a massive ring system around Saturn.
39 pages, 9 figures, 3 tables. Accepted for publication in ICARUS. New version with figures included in the text
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Cited by in corpus (20)
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- Impact bombardment chronology of the terrestrial planets from 4.5 Ga to 3.5 Ga
- Ring Formation around Giant Planets by Tidal Disruption of a Single Passing Large Kuiper Belt Object
- Solar System Physics for Exoplanet Research
- Compositions and origins of outer planet systems: Insights from the Roche critical density
- Accretion of Saturn's Inner Mid-sized Moons from a Massive Primordial Ice Ring
- Formation of Multiple-Satellite Systems From Low-Mass Circumplanetary Particle Disks
- Formation of Exomoons: A Solar System Perspective
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- Cronomoons: origin, dynamics, and light-curve features of ringed exomoons
- A Pluto--Charon Sonata: Dynamical Limits on the Masses of the Small Satellites
- Constraints on planetesimal disk mass from the cratering record and equatorial ridge on Iapetus
- Seasonal variation of radial brightness contrast of Saturn's rings viewed in mid-infrared by Subaru/COMICS
- The Dynamical Viability of an Extended Jupiter Ring System
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- Survival of exomoons around exoplanets
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