Binary Planetesimal Formation from Gravitationally Collapsing Pebble Clouds
David Nesvorny, Rixin Li, Jacob B. Simon, Andrew N. Youdin, Derek C., Richardson, Raphael Marschall, William M. Grundy

TL;DR
This study investigates how pebble clouds formed by streaming instability gravitationally collapse into planetesimals, producing various binary and multiple systems, with properties influenced by initial angular momentum, and compares simulation results to observed Kuiper belt binaries.
Contribution
The paper combines ATHENA and PKDGRAV simulations to analyze the collapse of pebble clouds and links initial angular momentum to the resulting planetesimal and binary properties, providing insights into Kuiper belt binaries.
Findings
Pebble clouds rapidly collapse into short-lived disk structures.
Low angular momentum clouds produce single planetesimals or tight binaries.
High angular momentum clouds form binary planetesimals resembling Kuiper belt binaries.
Abstract
Planetesimals are compact astrophysical objects roughly 1-1000 km in size, massive enough to be held together by gravity. They can grow by accreting material to become full-size planets. Planetesimals themselves are thought to form by complex physical processes from small grains in protoplanetary disks. The streaming instability (SI) model states that mm/cm-size particles (pebbles) are aerodynamically collected into self-gravitating clouds which then directly collapse into planetesimals. Here we analyze ATHENA simulations of the SI to characterize the initial properties (e.g., rotation) of pebble clouds. Their gravitational collapse is followed with the PKDGRAV N-body code, which has been modified to realistically account for pebble collisions. We find that pebble clouds rapidly collapse into short-lived disk structures from which planetesimals form. The planetesimal properties depend…
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