On the Formation of Super-Earths with Implications for the Solar System
Rebecca G. Martin, Mario Livio

TL;DR
This paper investigates how turbulence levels in protoplanetary disks influence super-Earth formation locations, proposing that both in situ formation in dead zones and migration from outer regions contribute to observed super-Earth diversity.
Contribution
It introduces the role of dead zones in disks for super-Earth formation and suggests multiple formation pathways, explaining the diversity in super-Earth properties and the uniqueness of the Solar System.
Findings
Dead zones can enable in situ super-Earth formation due to increased inner disk material.
Fully turbulent disks favor formation farther out with inward migration.
The Solar System's lack of super-Earths may be due to specific disk conditions.
Abstract
We first consider how the level of turbulence in a protoplanetary disk affects the formation locations for the observed close-in super-Earths in exosolar systems. We find that a protoplanetary disk that includes a dead zone (a region of low turbulence) has substantially more material in the inner parts of the disk, possibly allowing for in situ formation. For the dead zone to last the entire lifetime of the disk requires the active layer surface density to be sufficiently small, <100 g/cm^2. Migration through a dead zone may be very slow and thus super-Earth formation followed by migration towards the star through the dead zone is less likely. For fully turbulent disks, there is not enough material for in situ formation. However, in this case, super-Earths can form farther out in the disk and migrate inwards on a reasonable timescale. We suggest that both of these formation mechanisms…
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