Formation and Dynamical Evolution of the Neptune Trojans - the Influence of the Initial Solar System Architecture
arXiv:1002.3673 · doi:10.1111/j.1365-2966.2010.16381.x
Abstract
In this work, we investigate the dynamical stability of pre-formed Neptune Trojans under the gravitational influence of the four giant planets in compact planetary architectures, over 10 Myr. In our modelling, the initial orbital locations of Uranus and Neptune (aN) were varied to produce systems in which those planets moved on non-resonant orbits, or in which they lay in their mutual 1:2, 2:3 and 3:4 mean-motion resonances (MMRs). In total, 420 simulations were carried out, examining 42 different architectures, with a total of 840000 particles across all runs. In the non-resonant cases, the Trojans suffered only moderate levels of dynamical erosion, with the most compact systems (those with aN less than or equal 18 AU) losing around 50% of their Trojans by the end of the integrations. In the 2:3 and 3:4 MMR scenarios, however, dynamical erosion was much higher with depletion rates typically greater than 66% and total depletion in the most compact systems. The 1:2 resonant scenarios featured disruption on levels intermediate between the non-resonant cases and other resonant scenarios, with depletion rates of the order of tens of percent. Overall, the great majority of plausible pre-migration planetary architectures resulted in severe levels of depletion of the Neptunian Trojan clouds. In particular, if Uranus and Neptune formed near their mutual 2:3 or 3:4 MMR and at heliocentric distances within 18 AU (as favoured by recent studies), we found that the great majority of pre-formed Trojans would have been lost prior to Neptune's migration. This strengthens the case for the great bulk of the current Neptunian Trojan population having been captured during that migration.
arXiv comment17 pages, 2 figures, MNRAS (in press). Abstract slightly reduced in size, but in original form in the PDF file
References in corpus (19)
- Towards a Deterministic Model of Planetary Formation I: a Desert in the Mass and Semi Major Axis Distributions of Extra Solar Planets
- Models of Giant Planet formation with migration and disc evolution
- Orbital Evolution of Planets Embedded in a Planetesimal Disk
- Dynamics of the giant planets of the solar system in the gaseous proto-planetary disk and relationship to the current orbital architecture
- Final Stages of Planet Formation
- Neptune's Migration into a Stirred-Up Kuiper Belt: A Detailed Comparison of Simulations to Observations
- Simulations of the Population of Centaurs I: The Bulk Statistics
- A record of planet migration in the Main Asteroid Belt
- Resonance Occupation in the Kuiper Belt: Case Examples of the 5:2 and Trojan Resonances
- An Outer Planet Beyond Pluto and Origin of the Trans-Neptunian Belt Architecture
- On the migration-induced resonances in a system of two planets with masses in the Earth mass range
- Neptune Trojans as a Testbed for Planet Formation
- A safety net for fast migrators: Interactions between gap-opening and sub-gap-opening bodies in a protoplanetary disk
- Resonance sticking in the scattered disk
- The Capture of Centaurs as Trojans
- Origin and Dynamical Evolution of Neptune Trojans - I: Formation and Planetary Migration
- From mean-motion resonances to scattered planets: Producing the Solar System, eccentric exoplanets and Late Heavy Bombardments
- Survival of Trojan-Type Companions of Neptune During Primordial Planet Migration
- The Dynamics of Neptune Trojan: I. the Inclined Orbits
Cited by in corpus (5)
- Evolution of the reservoirs of volatiles in the protosolar nebula
- Modelling the Inner Debris Disc of HR 8799
- Absolute colours and phase coefficients of trans-Neptunian objects: Correlations and Populations
- A thermophysical and dynamical study of the Hildas (1162) Larissa and (1911) Schubart
- A sub-Neptune transiting the young field star HD 18599 at 40 pc