Influences of protoplanet-induced three-dimensional gas flow on pebble accretion . Headwind regime
arXiv:2009.07636 · doi:10.1051/0004-6361/202039153
Abstract
Pebble accretion is one of the major theories in planet formation. Aerodynamically small particles, called pebbles, are highly affected by the gas flow. A growing planet embedded in a protoplanetary disk induces three-dimensional (3D) gas flow. In our previous study, Paper I, we focused on the shear regime of pebble accretion, and investigated the influence of planet-induced gas flow on pebble accretion. In Paper I, we found that pebble accretion is inefficient in the planet-induced gas flow compared to that in the unperturbed flow, in particular when , where St is the Stokes number. Following Paper I, we investigate the influence of planet-induced gas flow on pebble accretion. We consider the headwind of the gas, which is not included in Paper I. We extend our study to the headwind regime of pebble accretion in this study. Assuming a nonisothermal, inviscid sub-Keplerian gas disk, we perform 3D hydrodynamical simulations on the spherical polar grid which has a planet with the dimensionless mass, , located at its center, where and are the Bondi radius and the disk scale height. We then numerically integrate the equation of motion of pebbles in 3D using hydrodynamical simulation data. Combining our results with the spacial variety of turbulence strength and pebble size in a disk, we conclude that the planet-induced gas flow still allows for pebble accretion in the early stage of planet formation. Suppression of pebble accretion due to the planet-induced gas flow occurs only in the late stage of planet formation, in particular in the inner region of the disk. This may be helpful to explain the distribution of exoplanets and the architecture of the Solar System, both of which have small inner and large outer planets.
arXiv comment24 pages, 23 figures, Accepted for publication in Astronomy and Astrophysics (A&A). arXiv admin note: text overlap with arXiv:1911.12999
References in corpus (56)
- First Results from High Angular Resolution ALMA Observations Toward the HL Tau Region
- The false positive rate of Kepler and the occurrence of planets
- The Disk Substructures at High Angular Resolution Project (DSHARP): I. Motivation, Sample, Calibration, and Overview
- Rapid growth of gas-giant cores by pebble accretion
- Giant Planet Occurrence in the Stellar Mass-Metallicity Plane
- Particle Stirring in Turbulent Gas Disks: Including Orbital Oscillations
- The effect of gas drag on the growth of protoplanets -- Analytical expressions for the accretion of small bodies in laminar disks
- The Mass-Radius Relation for 65 Exoplanets Smaller than 4 Earth Radii
- The Athena++ Adaptive Mesh Refinement Framework: Design and Magnetohydrodynamic Solvers
- Ringed Substructure and a Gap at 1 AU in the Nearest Protoplanetary Disk
- Gaps and Rings in an ALMA Survey of Disks in the Taurus Star-forming Region
- Separating gas-giant and ice-giant planets by halting pebble accretion
- Dust and Gas in the disc of HL Tauri: Surface density, dust settling, and dust-to-gas ratio
- The Disk Substructures at High Angular Resolution Project (DSHARP) VI: Dust trapping in thin-ringed protoplanetary disks
- Gaps, Rings, and Non-Axisymmetric Structures in Protoplanetary Disks - From Simulations to ALMA Observations
- Evidence of fast pebble growth near condensation fronts in the HL Tau protoplanetary disk
- Pebble isolation mass --- scaling law and implications for the formation of super-Earths and gas giants
- Sintering-induced Dust Ring Formation in Protoplanetary Disks: Application to the HL Tau Disk
- Observational Signatures of Planets in Protoplanetary Disks I: Gaps Opened by Single and Multiple Young Planets in Disks
- On planet formation in HL Tau
- Hints for a Turnover at the Snow Line in the Giant Planet Occurrence Rate
- Formation of planetary systems by pebble accretion and migration: How the radial pebble flux determines a terrestrial-planet or super-Earth growth mode
- An Extension of the Athena++ Code Framework for GRMHD Based on Advanced Riemann Solvers and Staggered-Mesh Constrained Transport
- Mass Estimates of a Giant Planet in a Protoplanetary Disk from the Gap Structures
- Hydrodynamics of Embedded Planets' First Atmospheres. II. A Rapid Recycling of Atmospheric Gas
- On the water delivery to terrestrial embryos by ice pebble accretion
- Two-Component Secular Gravitational Instability in a Protoplanetary Disk: A Possible Mechanism for Creating Ring-Like Structures
- ALMA continuum observations of the protoplanetary disk AS 209. Evidence of multiple gaps opened by a single planet
- The radial dependence of pebble accretion rates: A source of diversity in planetary systems I. Analytical formulation
- Protoplanetary disk rings and gaps across ages and luminosities
- Mass constraint for a planet in a protoplanetary disk from the gap width
- Reduced gas accretion on super-Earths and ice giants
- Hydrodynamics of embedded planets' first atmospheres - III. The role of radiation transport for super-Earth planets
- The 3D Flow Field Around an Embedded Planet
- Catching drifting pebbles I. Enhanced pebble accretion efficiencies for eccentric planets
- An Origin of Multiple Ring Structure and Hidden Planets in HL Tau: A Unified Picture by Secular Gravitational Instability
- The initial conditions for planet formation: Turbulence driven by hydrodynamical instabilities in disks around young stars
- Suppression of atmospheric recycling of planets embedded in a protoplanetary disc by buoyancy barrier
- Circumplanetary Disk Dynamics in the Isothermal and Adiabatic Limits
- Nonsticky Ice at the Origin of the Uniformly Polarized Submillimeter Emission from the HL Tau Disk
- Efficiency of thermal relaxation by radiative processes in protoplanetary discs: constraints on hydrodynamic turbulence
- Revised description of dust diffusion and a new instability creating multiple rings in protoplanetary disks
- Pebble dynamics and accretion onto rocky planets. I. Adiabatic and convective models
- On the filtering and processing of dust by planetesimals 1. Derivation of collision probabilities for non-drifting planetesimals
- The steady-state flow pattern past gravitating bodies
- Horseshoe drag in three-dimensional globally isothermal disks
- ALMA observations of Elias 2-24: a protoplanetary disk with multiple gaps in the Ophiuchus Molecular Cloud
- Envelopes of embedded super-Earths II. Three-dimensional isothermal simulations
- Non-linear Development of Secular Gravitational Instability in Protoplanetary Disks
- Dual-Wavelength ALMA Observations of Dust Rings in Protoplanetary Disks
- Gas flow around a planet embedded in a protoplanetary disc: the dependence on the planetary mass
- Inner Super-Earths, Outer Gas Giants: How Pebble Isolation and Migration Feedback Keep Jupiters Cold
- Catching drifting pebbles II. A stochastic equation of motions for pebbles
- Influences of three-dimensional gas flow induced by protoplanets on pebble accretion --. shear regime
- Pebble dynamics and accretion onto rocky planets. II. Radiative models
- Gas-Assisted Growth of Protoplanets in a Turbulent Medium
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- Recycling of the first atmospheres of embedded planets: Dependence on core mass and optical depth
- An Analytical Theory for the Growth from Planetesimals to Planets by Polydisperse Pebble Accretion
- The Growth of Protoplanets via the Accretion of Small Bodies in Disks Perturbed by the Planetary Gravity
- Mars' atmospheric neon suggests volatile-rich primitive mantle
- Spin of protoplanets generated by pebble accretion: Influences of protoplanet-induced gas flow
- Dust ring and gap formation by gas flow induced by low-mass planets embedded in protoplanetary disks . Steady-state model
- On the origin of transition disk cavities: Pebble-accreting protoplanets vs Super-Jupiters
- Interior dynamics of envelopes around disk-embedded planets
- A multi-fluid approach for polydisperse pebble accretion: From particles to fluids, establishing the multifluid framework