An alternative origin for debris rings of planetesimals
Sergei Nayakshin, Seung-Hoon Cha

TL;DR
This paper proposes that debris rings and Kuiper belt-like structures can form from planetesimals generated within gas clumps in the Tidal Downsizing planet formation scenario, offering an alternative origin to core accretion models.
Contribution
It introduces a novel mechanism for debris ring formation via planetesimals originating inside migrating gas clumps in the Tidal Downsizing hypothesis.
Findings
Planetesimals on distant orbits become unbound and form wide rings.
Close orbit planetesimals may become satellites of giant planets.
The model explains the sharp edge and mass deficit of the Kuiper belt.
Abstract
Core Accretion, the most widely accepted scenario for planet formation, postulates existence of km-sized solid bodies, called planetesimals, arranged in a razor-thin disc in the earliest phases of planet formation. In the Tidal Downsizing hypothesis, an alternative scenario for formation of planets, grain growth, sedimentation and formation of planetary cores occur inside dense and massive gas clumps formed in the outer cold disc by gravitational instability. As a clump migrates inward, tidal forces of the star remove all or most of the gas from the clump, downsizing it to a planetary mass body. Here we argue that such a clump may form not only the planetary core but also numerous smaller bodies. As an example, we consider the simplest case of bodies on circular orbits around the planetary core in the centre of the gas clump. Bodies smaller than 1 km suffer a strong enough aerodynamic…
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