Direct Formation of Planetary Embryos in Self-Gravitating Disks
arXiv:2204.13310 · doi:10.3847/1538-4357/ac7228
Abstract
Giant planets have been discovered at large separations from the central star. Moreover, a striking number of young circumstellar disks have gas and/or dust gaps at large orbital separations, potentially driven by embedded planetary objects. To form massive planets at large orbital separations through core accretion within disk lifetime, however, an early solid body to seed pebble and gas accretion is desirable. Young protoplanetary disks are likely self-gravitating, and these gravitoturbulent disks may efficiently concentrate solid material at the midplane driven by spiral waves. We run 3D local hydrodynamical simulations of gravitoturbulent disks with Lagrangian dust particles to determine whether particle and gas self-gravity can lead to the formation of dense solid bodies, seeding later planet formation. When self-gravity between dust particles is included, solids of size to concentrate within the gravitoturbulent spiral features and collapse under their own self-gravity into dense clumps up to several in mass at wide orbits. Simulations with dust that drift most efficiently, , form the most massive clouds of particles, while simulations with smaller dust particles, , have clumps with masses an order of magnitude lower. When the effect of dust backreaction onto the gas is included, dust clumps become smaller by a factor of a few but more numerous. The existence of large solid bodies at an early stage of the disk can accelerate the planet formation process, particularly at wide orbital separations, and potentially explain planets distant from the central stars and young protoplanetary disks with substructures.
20 pages, 12 figures, ApJ submitted - first referee report received, online video at https://youtu.be/hqtwMIe1dwk
References in corpus (36)
- The NumPy array: a structure for efficient numerical computation
- Particle Stirring in Turbulent Gas Disks: Including Orbital Oscillations
- Characterising the Gravitational Instability in Cooling Accretion Discs
- One Solution to the Mass Budget Problem for Planet Formation: Optically Thick Disks with Dust Scattering
- Initial mass function of planetesimals formed by the streaming instability
- Formation of planetary systems by pebble accretion and migration: Growth of gas giants
- The newborn planet population emerging from ring-like structures in discs
- Numerical requirements for simulations of self gravitating and non-self gravitating disks
- A giant exoplanet orbiting a very low-mass star challenges planet formation models
- Turbulence sets the length scale for planetesimal formation: Local 2D simulations of streaming instability and planetesimal formation
- Embryos grown in the dead zone: Assembling the first protoplanetary cores in low mass self-gravitating circumstellar disks of gas and solids
- Episodic accretion: the interplay of infall and disc instabilities
- Anisotropic Infall and Substructure formation in Embedded Disks
- Global magnetohydrodynamical models of turbulence in protoplanetary disks I. A cylindrical potential on a Cartesian grid and transport of solids
- Convergence of the critical cooling rate for protoplanetary disk fragmentation achieved; the key role of numerical dissipation of angular momentum
- Dust Transport in MRI Turbulent Disks: Ideal and Non-ideal MHD with Ambipolar Diffusion
- A case of simultaneous star and planet formation
- Testing the Jeans, Toomre and Bonnor-Ebert concepts for planetesimal formation: 3D streaming instability simulations of diffusion regulated formation of planetesimals
- A wide-orbit giant planet in the high-mass b Centauri binary system
- The fragmentation criteria in local vertically stratified self-gravitating disk simulations
- Gravito-Turbulent Disks in 3D: Turbulent Velocities vs. Depth
- Streaming Instability with Multiple Dust Species: II. Turbulence and Dust-Gas Dynamics at Nonlinear Saturation
- Formation and evolution of protostellar accretion discs. I. Angular-momentum budget, gravitational self-regulation, and numerical convergence
- Salt, Hot Water, and Silicon Compounds Tracing Massive Twin Disks
- Characterizing gravito-turbulence in 3D: turbulent properties and stability against fragmentation
- Planetesimal formation in self-gravitating discs: the effects of particle self-gravity and back-reaction
- Radially resolved simulations of collapsing pebble clouds in protoplanetary discs
- A two-step gravitational cascade for the fragmentation of self-gravitating discs
- Particle Dynamics in 3D Self-gravitating Disks II: Strong Gas Accretion and Thin Dust Disks
- Particle Dynamics in 3D Self-gravitating Disks I: Spirals
- Orbital advection with magnetohydrodynamics and vector potential
- The radial structure of planetary bodies formed by the streaming instability
- The observational impact of dust trapping in self-gravitating discs
- Planetary core formation via multi-species pebble accretion
- Architecture of planetary systems predicted from protoplanetary disks observed with ALMA I: mass of the possible planets embedded in the dust gap
- Pebble accretion in self-gravitating protostellar discs
Cited by in corpus (9)
- Testing a New Model of Embedded Protostellar Disks Against Observation: The Majority of Orion Class 0/I Disks Are Likely Warm, Massive, and Gravitationally Unstable
- Planetesimal Initial Mass Functions following Diffusion Regulated Gravitational Collapse
- Spirals and clumps in V960 Mon: signs of planet formation via gravitational instability around an FU Ori star?
- Revisiting collisional dust growth in Class 0/I protostellar disks: Sweep-up can convert a few of dust into kg pebbles in 0.1 Myr
- Filling in the Gaps: Can Gravitationally Unstable Discs Form the Seeds of Gas Giant Planets?
- Disk Evolution Study Through Imaging of Nearby Young Stars (DESTINYS): Diverse outcomes of binary-disk interactions
- Planetesimal Growth in Evolving Protoplanetary Disks: Constraints from the Pebble Supply
- Winding Motion of Spirals in a Gravitationally Unstable Protoplanetary Disk
- Gravitational instability in planet-forming discs