arXiv Analytics

Sign in

arXiv:1604.02952 [astro-ph.SR]AbstractReferencesReviewsResources

Dust Evolution and the Formation of Planetesimals

T. Birnstiel, M. Fang, A. Johansen

Published 2016-04-11Version 1

The solid content of circumstellar disks is inherited from the interstellar medium: dust particles of at most a micrometer in size. Protoplanetary disks are the environment where these dust grains need to grow at least 13 orders of magnitude in size. Our understanding of this growth process is far from complete, with different physics seemingly posing obstacles to this growth at various stages. Yet, the ubiquity of planets in our galaxy suggests that planet formation is a robust mechanism. This chapter focuses on the earliest stages of planet formation, the growth of small dust grains towards the gravitationally bound "planetesimals", the building blocks of planets. We will introduce some of the key physics involved in the growth processes and discuss how they are expected to shape the global behavior of the solid content of disks. We will consider possible pathways towards the formation of larger bodies and conclude by reviewing some of the recent observational advances in the field.

Comments: 43 pages, 6 figures, accepted. Chapter in International Space Science Institute (ISSI) Book on "The Disk in Relation to the Formation of Planets and their Proto-atmospheres", to be published in Space Science Reviews by Springer
Categories: astro-ph.SR, astro-ph.EP
Related articles: Most relevant | Search more
arXiv:2407.03520 [astro-ph.SR] (Published 2024-07-03)
Planet Formation and Disk Chemistry: Dust and Gas Evolution during Planet Formation
arXiv:2411.05203 [astro-ph.SR] (Published 2024-11-07)
Sites of Planet Formation in Binary Systems. II. Double the Disks in DF Tau
Taylor Kutra et al.
arXiv:2008.00751 [astro-ph.SR] (Published 2020-08-03)
AB Aur, a Rosetta stone for studies of planet formation (I): chemical study of a planet-forming disk