Kuiper Belt Formation via Grainy Planetary Migration
Patryk Sofia Lykawka, Jonathan Horner, Pedro Bernardinelli

TL;DR
This study uses N-body simulations to explore Kuiper Belt formation, revealing the roles of grainy planetary migration, primordial Plutos, and initial disk edge, but also highlighting the need for additional processes to explain all observed TNO populations.
Contribution
It introduces detailed N-body models incorporating grainy migration and primordial Plutos, advancing understanding of Kuiper Belt structure and its formation mechanisms.
Findings
Reproduces main TNO populations within 50 au
Resonant captures favor close Neptunian MMRs
Models fail to produce detached and high-inclination TNOs
Abstract
We used N-body simulations to model the 4.5 Gyr orbital evolution of the early Kuiper Belt, incorporating a massive protoplanetary disk, the four giant planets, and 1500 primordial Pluto-class bodies ("Plutos") that drove Neptune's grainy migration. The analysis of 67 simulated systems revealed key insights: (1) All systems featured the primary trans-Neptunian object (TNO) populations: cold/hot classical, resonant, scattered, and detached; (2) Captures into stable resonant orbits favored close Neptunian mean motion resonances (MMRs; e.g., 3:2, 2:1), while distant ones beyond 50 au (e.g., 5:2 MMR) were underpopulated; (3) Optimal matches to observed resonant fractions and the classical region (including the kernel) arose from models considering a jumping Neptune, self-gravitating Plutos, and an initial disk edge at 45-47 au; (4) Models including primordial scattered disks boosted distant…
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Taxonomy
TopicsAstro and Planetary Science · Paleontology and Stratigraphy of Fossils · Geological and Geochemical Analysis
