Collisional Evolution of the Primordial Trans-Neptunian Disk: Implications for Planetary Migration and the Current Size Distribution of TNOs

Astronomy and Astrophysics – Astronomy

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A recent model of the evolution of the outer solar system [1,2] predicts that the outer planets were initially in a much more compact configuration and began to slowly migrate due to interactions with a massive trans-Neptunian disk of planetesimals. After ˜700 Myr of slow migration, Jupiter and Saturn cross their mutual 2:1 mean-motion resonance, destabilizing the system, triggering the late heavy bombardment (LHB), and causing a rapid migration of the outer planets to their current orbital configuration. This model requires that the dynamical excitation and resulting collisional activity in the trans-Neptunian disk was low enough that ˜35 Earth masses of material could remain after 700 Myr.
We will present the results of simulations of the dynamical excitation of the primordial trans-Neptunian disk and of the resulting collisional evolution of the disk. Our preliminary work suggests that there is a reasonable range of parameters over which the primordial trans-Neptunian disk is able to remain massive (>30 Earth masses) for 700 Myr. In addition, the final size distribution of trans-Neptunian bodies in our simulations is consistent with the survey results of Bernstein et al. [3] for the total trans-Neptunian object (TNO) population. The 700 Myr of collisional evolution in the massive, primordial trans-Neptunian disk would dwarf any subsequent collisional evolution in the current, much less massive TNO population. Hence, the current population of TNOs is likely a fossil remnant of the early primordial phase.
References: [1] Gomes et al., Nature 435, 2005. [2] Tsiganis et al., Nature 435, 2005. [3] Bernstein et al., AJ 128, 2004.

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