From Planetesimals to Dust: Low Gravity Experiments on Recycling Solids at the Inner Edge of Protoplanetary Disks
Caroline de Beule, Thorben Kelling, Gerhard Wurm, Jens Teiser, Tim, Jankowski

TL;DR
This study demonstrates that light-induced erosion of dusty bodies in protoplanetary disks is gravity-dependent and acts as an efficient recycling mechanism, influencing dust transport and planetesimal formation.
Contribution
The paper provides experimental evidence and a model showing how light-induced erosion affects dust dynamics at the inner edges of protoplanetary disks.
Findings
Light-induced erosion is strongly gravity dependent.
Erosion can prevent large bodies from migrating inward.
Produced dust can be transported outward and participate in planetesimal growth.
Abstract
Transporting solids of different sizes is an essential process in the evolution of protoplanetary disks and planet formation. Large solids are supposed to drift inward; high-temperature minerals found in comets are assumed to have been transported outward. From low-gravity experiments on parabolic flights we studied the light-induced erosion of dusty bodies caused by a solid-state greenhouse effect and photophoresis within a dust bed's upper layers. The gravity levels studied were 0.16g, 0.38g, 1g, and 1.7g. The light flux during the experiments was 12 +/- 2 kW/m^2 and the ambient pressure was 6 +/- 0.9 mbar. Light-induced erosion is strongly gravity dependent, which is in agreement with a developed model. In particular for small dusty bodies ((sub)-planetesimals), efficient erosion is possible at the optically thin inner edges of protoplanetary disks. Light-induced erosion prevents…
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