Theory of Turbulent Accretion Disks

ArXiv astro-ph/0107408 (2001)

Abstract:

In low-mass disks, turbulent torques are probably the most important way of redistributing angular momentum. Here we present the theory of turbulent accretion disks. We show the molecular viscosity is far too small to account for the evolutionary timescale of disks, and we describe how turbulence may result in enhanced transport of (angular) momentum. We then turn to the magnetorotational instability, which thus far is the only mechanism that has been shown to initiate and sustain turbulence in disks. Finally, we present both the basis and the structure of alpha disk models.

Linear analysis of the Hall effect in protostellar disks

ASTROPHYSICAL JOURNAL 552:1 (2001) 235-247

Authors:

SA Balbus, C Terquem

Tidally-induced angular momentum transport in disks

ArXiv astro-ph/0008514 (2000)

Abstract:

We discuss the transport of angular momentum induced by tidal effects in a disk surrounding a star in a pre-main sequence binary system. We consider the effect of both density and bending waves. Although tidal effects are important for truncating protostellar disks and for determining their size, it is unlikely that tidally-induced angular momentum transport plays a dominant role in the evolution of protostellar disks. Where the disk is magnetized, transport of angular momentum is probably governed by MHD turbulence. In a non self-gravitating laminar disk, the amount of transport provided by tidal waves is probably too small to account for the lifetime of protostellar disks. In addition, tidal effects tend to be localized in the disk outer regions.

Disks, extrasolar planets and migration

Space Science Reviews 92:1-2 (2000) 323-340

Authors:

C Terquem, JCB Papaloizou, RP Nelson

Abstract:

We review results about protoplanetary disk models, protoplanet migration and formation of giant planets with migrating cores. We first model the protoplanetary nebula as an α-accretion disk and present steady state calculations for different values of α and gas accretion rate through the disk. We then review the current theories of protoplanet migration in the context of these models, focusing on the gaseous disk-protoplanet tidal interaction. According to these theories, the migration timescale may be shorter than the planetary formation timescale. Therefore we investigate planet formation in the context of a migrating core, considering both the growth of the core and the build-up of the envelope in the course of the migration.

Disk evolution towards planet formation

DISKS, PLANETESIMALS, AND PLANETS, PROCEEDINGS 219 (2000) 19-30

Authors:

C Terquem, JCB Papaloizou, RP Nelson