Tidal Barrier and the Asymptotic Mass of Proto Gas-Giant Planets
arXiv:astro-ph/0701269 · doi:10.1086/512537
Abstract
Extrasolar planets found with radial velocity surveys have masses ranging from several Earth to several Jupiter masses. While mass accretion onto protoplanetary cores in weak-line T-Tauri disks may eventually be quenched by a global depletion of gas, such a mechanism is unlikely to have stalled the growth of some known planetary systems which contain relatively low-mass and close-in planets along with more massive and longer period companions. Here, we suggest a potential solution for this conundrum. In general, supersonic infall of surrounding gas onto a protoplanet is only possible interior to both of its Bondi and Roche radii. At a critical mass, a protoplanet's Bondi and Roche radii are equal to the disk thickness. Above this mass, the protoplanets' tidal perturbation induces the formation of a gap. Although the disk gas may continue to diffuse into the gap, the azimuthal flux across the protoplanets' Roche lobe is quenched. Using two different schemes, we present the results of numerical simulations and analysis to show that the accretion rate increases rapidly with the ratio of the protoplanet's Roche to Bondi radii or equivalently to the disk thickness. In regions with low geometric aspect ratios, gas accretion is quenched with relatively low protoplanetary masses. This effect is important for determining the gas-giant planets' mass function, the distribution of their masses within multiple planet systems around solar type stars, and for suppressing the emergence of gas-giants around low mass stars.
References in corpus (2)
Cited by in corpus (27)
- Toward a Deterministic Model of Planetary Formation V. Accumulation Near the Ice Line
- The Population of Viscosity- and Gravitational Wave-Driven Supermassive Black Hole Binaries Among Luminous AGN
- Growing the gas-giant planets by the gradual accumulation of pebbles
- Toward a Deterministic Model of Planetary Formation VII: Eccentricity Distribution of Gas Giants
- Origin of the Different Architectures of the Jovian and Saturnian Satellite Systems
- Evolution of Migrating Planets Undergoing Gas Accretion
- Final Masses of Giant Planets II: Jupiter Formation in a Gas-Depleted Disk
- Assembling the Building Blocks of Giant Planets around Intermediate Mass Stars
- Microlensing Results Challenge the Core Accretion Runaway Growth Scenario for Gas Giants
- Planetesimal Accretion onto Growing Proto-Gas-Giant Planets
- Hydrodynamics of Embedded Planets' First Atmospheres. I. A Centrifugal Growth Barrier for 2D Flows
- Do Giant Planets Survive Type II Migration?
- Gas Accretion onto a Protoplanet and Formation of a Gas Giant Planet
- Accretion onto Stars in the Disks of Active Galactic Nuclei
- Interaction of Close-in Planets with the Magnetosphere of their Host Stars. II. Super-Earths as Unipolar Inductors and their Orbital Evolution
- N-body simulations of planet formation via pebble accretion I: First Results
- The Preservation of Super Earths and the Emergence of Gas Giants after Their Progenitor Cores have Entered the Pebble Isolation Phase
- Spin Evolution of Stellar-mass Black Holes Embedded in AGN disks: Orbital Eccentricity Produces Retrograde Circumstellar Flows
- Accretion of Gas Giants Constrained by the Tidal Barrier
- Planetesimal clearing and size-dependent asteroid retention by secular resonance sweeping during the depletion of the solar nebula
- Retention of Long-Period Gas Giant Planets: Type II Migration Revisited
- No Sub-Saturn Mass Planet Desert in the CORALIE/HARPS Radial Velocity Sample
- Embryo impacts and gas giant mergers I: Dichotomy of Jupiter and Saturn's core mass
- A Substellar Companion in a 1.3 yr Nearly-circular Orbit of HD 16760
- The Influence of Disk Composition on the Evolution of Stars in the Disks of Active Galactic Nuclei
- Chondrule Formation by the Jovian Sweeping Secular Resonance
- Effects of Thermodynamics on the Concurrent Accretion and Migration of Gas Giants in Protoplanetary Disks