Dynamics of Porous Dust Aggregates and Gravitational Instability of Their Disk
arXiv:1705.04520 · doi:10.3847/1538-4357/aa7388
Abstract
We consider the dynamics of porous icy dust aggregates in a turbulent gas disk and investigate the stability of the disk. We evaluate the random velocity of porous dust aggregates by considering their self-gravity, collisions, aerodynamic drag, turbulent stirring and scattering due to gas. We extend our previous work by introducing the anisotropic velocity dispersion and the relaxation time of the random velocity. We find the minimum mass solar nebular model to be gravitationally unstable if the turbulent viscosity parameter is less than about . The upper limit of for the onset of gravitational instability is derived as a function of the disk parameters. We discuss the implications of the gravitational instability for planetesimal formation.
arXiv comment38 pages, 14 figures, accepted for publication in ApJ
References in corpus (45)
- Rapid planetesimal formation in turbulent circumstellar discs
- Streaming Instabilities in Protoplanetary Disks
- Nonlinear Outcome of Gravitational Instability in Cooling, Gaseous Disks
- Rapid growth of gas-giant cores by pebble accretion
- Particle Stirring in Turbulent Gas Disks: Including Orbital Oscillations
- Wind-driven Accretion in Protoplanetary Disks. I: Suppression of the Magnetorotational Instability and Launching of the Magnetocentrifugal Wind
- Planetesimal Formation by Gravitational Instability
- Forming the cores of giant planets from the radial pebble flux in protoplanetary discs
- Rapid Coagulation of Porous Dust Aggregates Outside the Snow Line: A Pathway to Successful Icy Planetesimal Formation
- Forming Planetesimals in Solar and Extrasolar Nebulae
- Magnetorotational Instability in Protoplanetary Disks. II. Ionization State and Unstable Regions
- Particle Clumping and Planetesimal Formation Depend Strongly on Metallicity
- Towards planetesimals: dense chondrule clumps in the protoplanetary nebula
- Dynamics of Solids in the Midplane of Protoplanetary Disks: Implications for Planetesimal Formation
- Size-selective concentration of chondrules and other small particles in protoplanetary nebula turbulence
- Fluffy dust forms icy planetesimals by static compression
- Disk Winds Driven by Magnetorotational Instability and Dispersal of Proto-Planetary Disks
- How to form planetesimals from mm-sized chondrules and chondrule aggregates
- On the Formation of Planetesimals via Secular Gravitational Instabilities with Turbulent Stirring
- Two-Component Secular Gravitational Instability in a Protoplanetary Disk: A Possible Mechanism for Creating Ring-Like Structures
- The Effect of the Radial Pressure Gradient in Protoplanetary Disks on Planetesimal Formation
- Numerical Modeling of the Coagulation and Porosity Evolution of Dust Aggregates
- Modeling Magnetorotational Turbulence in Protoplanetary Disks with Dead Zones
- Static compression of porous dust aggregates
- Geometrical Cross Sections of Dust Aggregates and a Compression Model for Aggregate Collisions
- Dead zones as safe-havens for planetesimals: influence of disc mass and external magnetic field
- Dust and gas density evolution at a radial pressure bump in protoplanetary disks
- Density waves in the shearing sheet I. Swing amplification
- From Planetesimals to Planets in Turbulent Protoplanetary Disks I. Onset of Runaway Growth
- The Fate of Planetesimals in Turbulent Disks with Dead Zones. I. The Turbulent Stirring Recipe
- Planetesimal and Protoplanet Dynamics in a Turbulent Protoplanetary Disk: Ideal Stratified Disks
- -body Simulation of Planetesimal Formation Through Gravitational Instability of a Dust Layer
- The effects of the Tidal Force on Shear Instabilities in the Dust Layer of the Solar Nebula
- Pitch Angle of Galactic Spiral Arms
- Rocky Planetesimal Formation via Fluffy Aggregates of Nanograins
- Secular Gravitational Instability of a Dust Layer in Shear Turbulence
- Density waves in the shearing sheet V. Feedback cycle for swing amplification by non-linear effects
- Galactic Spiral Arms by Swing Amplification
- On dust-gas gravitational instabilities in protoplanetary discs
- N-Body Simulation of Planetesimal Formation through Gravitational Instability of a Dust Layer in Laminar Gas Disk
- Planetesimal Formation at the Boundary Between Steady Super/Sub-Keplerian Flow Created by Inhomogeneous Growth of Magnetorotational Instability
- Swing Amplification of Galactic Spiral Arms: Phase Synchronization of Stellar Epicycle Motion
- N-Body Simulation of Planetesimal Formation through Gravitational Instability and Coagulation. II. Accretion Model
- Planetesimal Formation by Gravitational Instability of a Porous-Dust Disk
- Two evolutional paths of an axisymmetric gravitational instability in the dust layer of a protoplanetary disk
Cited by in corpus (5)
- Planet Formation around Super Massive Black Holes in the Active Galactic Nuclei
- Formation of "Blanets" from Dust Grains around the Supermassive Black Holes in Galaxies
- Ejection of Chondrules from Fluffy Matrices
- Nonlinear Outcome of Coagulation Instability in Protoplanetary Disks II: Dust Ring Formation Mediated by Backreaction and Fragmentation
- Gravitational instability of a dust layer composed of porous silicate dust aggregates in a protoplanetary disk