Self-Stirring of Debris Discs by Planetesimals Formed by Pebble Concentration
Alexander V. Krivov, Mark Booth

TL;DR
This paper demonstrates that small planetesimals formed by pebble concentration can self-stir debris discs faster than previously thought, often explaining observed disc excitation without requiring planets, except in some large cases.
Contribution
It introduces an analytic model showing rapid self-stirring by small planetesimals, challenging the assumption that only Pluto-sized bodies can stir debris discs.
Findings
Most observed debris discs are consistent with self-stirring by small planetesimals.
Some large discs around young stars still require planetary stirrers.
The excitation timescale depends on disc mass, radius, and stellar mass.
Abstract
When a protoplanetary disc loses gas, it leaves behind planets and one or more planetesimal belts. The belts get dynamically excited, either by planets ('planet stirring') or by embedded big planetesimals ('self-stirring'). Collisions between planetesimals become destructive and start to produce dust, creating an observable debris disc. Following Kenyon & Bromley (2008), it is often assumed that self-stirring starts to operate as soon as the first ~1000 km-sized embedded 'Plutos' have formed. However, state-of-the-art pebble concentration models robustly predict planetesimals between a few km and ~200 km in size to form in protoplanetary discs rapidly, before then slowly growing into Pluto-sized bodies. We show that the timescale, on which these planetesimals excite the disc sufficiently for fragmentation, is shorter than the formation timescale of Plutos. Using an analytic model based…
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