Disk Dispersal: Theoretical Understanding and Observational Constraints
Journal article, 2016

Protoplanetary disks dissipate rapidly after the central star forms, on time-scales comparable to those inferred for planet formation. In order to allow the formation of planets, disks must survive the dispersive effects of UV and X-ray photoevaporation for at least a few Myr. Viscous accretion depletes significant amounts of the mass in gas and solids, while photoevaporative flows driven by internal and external irradiation remove most of the gas. A reasonably large fraction of the mass in solids and some gas get incorporated into planets. Here, we review our current understanding of disk evolution and dispersal, and discuss how these might affect planet formation. We also discuss existing observational constraints on dispersal mechanisms and future directions.

Accretion

Winds

Protoplanetary disks

Planet formation

Author

U. Gorti

NASA Ames Research Center

René Liseau

Chalmers, Earth and Space Sciences, Radio Astronomy and Astrophysics

Z. Sándor

Hungarian Academy of Sciences

C. Clarke

University of Cambridge

Space Science Reviews

0038-6308 (ISSN) 1572-9672 (eISSN)

Vol. 205 1-4 125-152

Subject Categories

Astronomy, Astrophysics and Cosmology

Infrastructure

Onsala Space Observatory

DOI

10.1007/s11214-015-0228-x

More information

Latest update

2/20/2019