Conditions for Gravitational Instability in Protoplanetary Disks
arXiv:1205.3013 · doi:10.1093/pasj/64.5.116
Abstract
Gravitational instability is one of considerable mechanisms to explain the formation of giant planets. We study the gravitational stability for the protoplanetary disks around a protostar. The temperature and Toomre's Q-value are calculated by assuming local equilibrium between viscous heating and radiative cooling (local thermal equilibrium). We assume constant viscosity and use a cooling function with realistic opacity. Then, we derive the critical surface density that is necessary for a disk to become gravitationally unstable as a function of . This critical surface density is strongly affected by the temperature dependence of the opacity. At the radius AU, where ices form, the value of changes discontinuously by one order of magnitude. This is determined only by local thermal process and criterion of gravitational instability. By comparing a given surface density profile to , one can discuss the gravitational instability of protoplanetary disks. As an example, we discuss the gravitational instability of two semi-analytic models for protoplanetary disks. One is the steady state accretion disk, which is realized after the viscous evolution. The other is the disk that has the same angular momentum distribution with its parent cloud core, which corresponds to the disk that has just formed. As a result, it is found that the disks tend to become gravitationally unstable for because ices enable the disks to become low temperature. In the region closer to the protostar than , it is difficult for a typical protoplanetary disk to fragment because of the high temperature and the large Coriolis force. From this result, we conclude that the fragmentation near the central star is possible but difficult.
accepted for publication in PASJ. Draft version with 26 pages, 8 figures, 1 table
References in corpus (5)
- Direct Imaging of Multiple Planets Orbiting the Star HR 8799
- Optical Images of an Exosolar Planet 25 Light Years from Earth
- Global Models for the Evolution of Embedded, Accreting Protostellar Disks
- The Thermal Regulation of Gravitational Instabilities in Protoplanetary Disks III. Simulations with Radiative Cooling and Realistic Opacities
- The response of self-graviting protostellar discs to slow reduction in cooling timescale: the fragmentation boundary revisited
Cited by in corpus (16)
- A revised condition for self-gravitational fragmentation of protoplanetary disks
- Dispersal of protoplanetary disks by the combination of magnetically driven and photoevaporative winds
- From Birth to Death of Protoplanetary Disks: Modeling Their Formation, Evolution, and Dispersal
- Gravitational instability in protostellar disks at low metallicities
- Mass constraints for 15 protoplanetary disks from HD 1-0
- Apparent disk-mass reduction and planetesimal formation in gravitationally unstable disks in Class 0/I YSOs
- Jupiter's formation in the vicinity of the amorphous ice snowline
- Formation, orbital and thermal evolution, and survival of planetary-mass clumps in the early phase of circumstellar disk evolution
- On the gravitational stability of gravito-turbulent accretion disks
- The influence of infall on the properties of protoplanetary discs
- One-armed spirals in locally isothermal, radially structured self-gravitating discs
- Orbital Evolution of Moons in Weakly Accreting Circumplanetary Disks
- The Origin of the Rotation Profiles in Star Forming Clouds
- Kinematic evidence for an embedded planet in the IM Lupi disc
- Constraints on planet formation via gravitational instability across cosmic time
- Dynamics of Dusty Vortices II: Stability of 2D dust laden vortices