Accretion Processes
Alessandro Morbidelli

TL;DR
This paper reviews the multiple accretion processes in planetary formation, from dust sticking to planetesimal formation and planetary growth, emphasizing historical developments and recent discoveries.
Contribution
It provides a comprehensive overview of the various accretion mechanisms involved in planet formation, highlighting recent advances and the complexity of the process.
Findings
Multiple accretion processes operate at different scales.
Recent discoveries have unveiled new mechanisms in planetesimal formation.
Accretion must be both efficient and rapid to explain planetary system development.
Abstract
In planetary science, accretion is the process in which solids agglomerate to form larger and larger objects and eventually planets are produced. The initial conditions are a disc of gas and microscopic solid particles, with a total mass of about 1% of the gas mass. Accretion has to be effective and fast. Effective, because the original total mass in solids in the solar protoplanetary disk was probably of the order of ~ 300 Earth masses, and the mass incorporated into the planets is ~100 Earth masses. Fast, because the cores of the giant planets had to grow to tens of Earth masses in order to capture massive doses of hydrogen and helium from the disc before the dispersal of the latter, i.e. in a few millions of years. There is probably not one accretion process but several, depending on the scale at which accretion operates. A first process is the sticking of microscopic dust into…
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Taxonomy
TopicsAstro and Planetary Science · Astrophysics and Star Formation Studies · Spacecraft and Cryogenic Technologies
