Initial mass function of planetesimals formed by the streaming instability
arXiv:1611.02285 · doi:10.1051/0004-6361/201629561
Abstract
The streaming instability is a mechanism to concentrate solid particles into overdense filaments that undergo gravitational collapse and form planetesimals. However, it remains unclear how the initial mass function of these planetesimals depends on the box dimensions of numerical simulations. To resolve this, we perform simulations of planetesimal formation with the largest box dimensions to date, allowing planetesimals to form simultaneously in multiple filaments that can only emerge within such large simulation boxes. In our simulations, planetesimals with sizes between 80 km and several hundred kilometers form. We find that a power law with a rather shallow exponential cutoff at the high-mass end represents the cumulative birth mass function better than an integrated power law. The steepness of the exponential cutoff is largely independent of box dimensions and resolution, while the exponent of the power law is not constrained at the resolutions we employ. Moreover, we find that the characteristic mass scale of the exponential cutoff correlates with the mass budget in each filament. Together with previous studies of high-resolution simulations with small box domains, our results therefore imply that the cumulative birth mass function of planetesimals is consistent with an exponentially tapered power law with a power-law exponent of approximately -1.6 and a steepness of the exponential cutoff in the range of 0.3-0.4.
11 pages, 5 figures, 3 tables; accepted for publication in Astronomy & Astrophysics; language editing completed
References in corpus (25)
- Galactic Stellar and Substellar Initial Mass Function
- Toward Understanding Massive Star Formation
- 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
- The effect of gas drag on the growth of protoplanets -- Analytical expressions for the accretion of small bodies in laminar disks
- The outcome of protoplanetary dust growth: pebbles, boulders, or planetesimals? II. Introducing the bouncing barrier
- The outcome of protoplanetary dust growth: pebbles, boulders, or planetesimals? I. Mapping the zoo of laboratory collision experiments
- Protoplanetary Disk Turbulence Driven by the Streaming Instability: Non-Linear Saturation and Particle Concentration
- Particle Clumping and Planetesimal Formation Depend Strongly on Metallicity
- Zonal Flows and Long-Lived Axisymmetric Pressure Bumps in Magnetorotational Turbulence
- Dynamics of Solids in the Midplane of Protoplanetary Disks: Implications for Planetesimal Formation
- The Mass and Size Distribution of Planetesimals Formed by the Streaming Instability. I. The Role of Self-Gravity
- Protoplanetary Disk Turbulence Driven by the Streaming Instability: Linear Evolution and Numerical Methods
- The structure of protoplanetary discs around evolving young stars
- How to form planetesimals from mm-sized chondrules and chondrule aggregates
- Dust size distributions in coagulation/fragmentation equilibrium: Numerical solutions and analytical fits
- Planetesimal formation by sweep-up: How the bouncing barrier can be beneficial to growth
- Adding particle collisions to the formation of asteroids and Kuiper belt objects via streaming instabilities
- The Effect of the Radial Pressure Gradient in Protoplanetary Disks on Planetesimal Formation
- Particle-Gas Dynamics with Athena: Method and Convergence
- Survival of the mm-cm size grain population observed in protoplanetary disks
- High-resolution simulations of planetesimal formation in turbulent protoplanetary discs
- On the Feeding Zone of Planetesimal Formation by the Streaming Instability
Cited by in corpus (120)
- The Disk Substructures at High Angular Resolution Project (DSHARP) VI: Dust trapping in thin-ringed protoplanetary disks
- Concentrating small particles in protoplanetary disks through the streaming instability
- Formation of TRAPPIST-1 and other compact systems
- Thresholds for Particle Clumping by the Streaming Instability
- Resonant Drag Instabilities in protoplanetary disks: the streaming instability and new, faster-growing instabilities
- Dust evolution in protoplanetary discs and the formation of planetesimals. What have we learned from laboratory experiments?
- A highly settled disk around Oph 163131
- Evidence for universality in the initial planetesimal mass function
- The Natural History of 'Oumuamua
- Turbulence sets the length scale for planetesimal formation: Local 2D simulations of streaming instability and planetesimal formation
- The Mass and Size Distribution of Planetesimals Formed by the Streaming Instability. II. The Effect of the Radial Gas Pressure Gradient
- Demographics of Planetesimals Formed by the Streaming Instability
- Connecting planet formation and astrochemistry: A main sequence for C/O in hot-exoplanetary atmospheres
- Protoplanetary Disk Rings as Sites for Planetesimal Formation
- Streaming Instability in Turbulent Protoplanetary Disks
- Pebble-driven Planet Formation around Very Low-mass Stars and Brown Dwarfs
- Pebble-driven planet formation for TRAPPIST-1 and other compact systems
- Solution to the debris disc mass problem: planetesimals are born small?
- How efficient is the streaming instability in viscous protoplanetary disks?
- Implications of the interstellar object 1I/'Oumuamua for planetary dynamics and planetesimal formation
- How dust fragmentation may be beneficial to planetary growth by pebble accretion
- A Tale of Planet Formation: From Dust to Planets
- Turbulence Regulates the Rate of Planetesimal Formation via Gravitational Collapse
- Growth after the streaming instability: from planetesimal accretion to pebble accretion
- Efficient planet formation by pebble accretion in ALMA rings
- On the Numerical Robustness of the Streaming Instability: Particle Concentration and Gas Dynamics in Protoplanetary Disks
- Connecting planet formation and astrochemistry: Refractory carbon depletion leading to super-stellar C/O in giant planetary atmospheres
- Requirements for gravitational collapse in planetesimal formation --- the impact of scales set by Kelvin-Helmholtz and nonlinear streaming instability
- On the coexistence of the streaming instability and the vertical shear instability in protoplanetary disks
- Composition of Early Planetary Atmospheres II: Coupled Dust and Chemical Evolution in Protoplanetary Disks
- Rapid Formation of Massive Planetary Cores in a Pressure Bump
- Effect of nucleation on icy pebble growth in protoplanetary discs
- Testing the Jeans, Toomre and Bonnor-Ebert concepts for planetesimal formation: 3D streaming instability simulations of diffusion regulated formation of planetesimals
- Linear growth of streaming instability in pressure bumps
- Formation of solar system analogs I: looking for initial conditions through a population synthesis analysis
- Self-Stirring of Debris Discs by Planetesimals Formed by Pebble Concentration
- The impact of pebble flux regulated planetesimal formation on giant planet formation
- Interstellar object 'Oumuamua as an extinct fragment of an ejected cometary planetesimal
- Exploring the conditions for forming cold gas giants through planetesimal accretion
- Debris Disc Constraints on Planetesimal Formation
- Streaming Instability with Multiple Dust Species: II. Turbulence and Dust-Gas Dynamics at Nonlinear Saturation
- Planet Formation: An Optimized Population-Synthesis Approach
- Dust Settling and Clumping in MRI Turbulent Outer Protoplanetary Disks
- From Pebbles and Planetesimals to Planets and Dust: the Protoplanetary Disk--Debris Disk Connection
- 1I/2017 'Oumuamua-like Interstellar Asteroids as Possible Messengers from the Dead Stars
- Mineralogy, structure and habitability of carbon-enriched rocky exoplanets: A laboratory approach
- Rapid Formation of Jupiter and Wide-Orbit Exoplanets in Disks with Pressure Bumps
- Formation of Comets
- Streaming instability of multiple particle species II -- Numerical convergence with increasing particle number
- Stratified and vertically-shearing streaming instabilities in protoplanetary disks
- The coexistence of the streaming instability and the vertical shear instability in protoplanetary disks: Planetesimal formation thresholds explored in two-dimensional global models
- The hot main Kuiper belt size distribution from OSSOS
- Planetesimal Initial Mass Functions following Diffusion Regulated Gravitational Collapse
- From Dust to Planets I: Planetesimal and Embryo Formation
- Linking planetary embryo formation to planetesimal formation II: The impact of pebble accretion in the terrestrial planet zone
- Planet formation in stellar binaries: Global simulations of planetesimal growth
- Dust Settling Instability in Protoplanetary Discs
- Dust growth, fragmentation and self-induced dust traps in PHANTOM
- Formation of Terrestrial Planets
- Direct Formation of Planetary Embryos in Self-Gravitating Disks
- Origin and dynamical evolution of the asteroid belt
- An inflationary disk phase to explain extended protoplanetary dust disks
- On the inclinations of the Jupiter Trojans
- Are there any pristine comets? Constraints from pebble structure
- Channels for streaming instability in dusty discs
- On the multiple generations of planetary embryos
- The interplay between pebble and planetesimal accretion in population synthesis models and its role in giant planet formation
- Vertical settling of pebbles in turbulent circumbinary discs and the in situ formation of circumbinary planets
- Morphological signatures induced by dust back reaction in discs with an embedded planet
- Global N-body simulations of circumbinary planet formation around Kepler-16 and -34 analogues I: Exploring the pebble accretion scenario
- Compaction during fragmentation and bouncing produces realistic dust grain porosities in protoplanetary discs
- Promoted Mass Growth of Multiple, Distant Giant Planets through Pebble Accretion and Planet-Planet Collision
- Streaming instabilities in accreting and magnetized laminar protoplanetary disks
- Dust-vortex instability in the regime of well-coupled grains
- The radial structure of planetary bodies formed by the streaming instability
- Growing the seeds of pebble accretion through planetesimal accretion
- Solving for the 2D Water Snowline with Hydrodynamic Simulations. Emergence of gas outflow, water cycle and temperature plateau
- Effects of pebble accretion on the growth and composition of planetesimals in the inner Solar System
- Instabilities and Flow Structures in Protoplanetary Disks: Setting the Stage for Planetesimal Formation
- Streaming instability on different scales. I. Planetesimal mass distribution variability
- High Resolution Study of Planetesimal Formation by Gravitational Collapse of Pebble Clouds
- On the suppression of giant planet formation around low-mass stars in clustered environments
- Planetesimal formation via the streaming instability with multiple grain sizes
- Growth after the streaming instability: The radial distance dependence of the planetary growth
- The big sibling of AU Mic: a cold dust-rich debris disk around CP-72 2713 in the Pic moving group
- Dust-Gas Coupling in Turbulence- and MHD Wind-Driven Protoplanetary Disks: Implications for Rocky Planet Formation
- Extreme Pebble Accretion in Ringed Protoplanetary Discs
- Can the giant planets of the Solar System form via pebble accretion in a smooth protoplanetary disc?
- Dust-gas dynamics driven by the streaming instability with various pressure gradients
- Resolving the outer ring of HD 38206 using ALMA and constraining limits on planets in the system
- A brief overview of planet formation
- MRI-active inner regions of protoplanetary discs. II. Dependence on dust, disc and stellar parameters
- Turbulent Disk Viscosity and the Bifurcation of Planet Formation Histories
- Connecting Planetary Composition with Formation
- Nonlinear evolution of streaming instabilities in accreting protoplanetary disks
- Observation of aerodynamic instability in the flow of a particle stream in a dilute gas
- Planetesimal formation via the streaming instability in simulations of infall dominated young disks
- Composition constraints of the TRAPPIST-1 planets from their formation
- Super-Earth formation in systems with cold giants
- Formation of Multiple Dynamical Classes in the Kuiper Belt via Disk Dissipation
- Dust grain shattering in protoplanetary discs: collisional fragmentation or rotational disruption?
- The influence of planetesimal fragmentation on planet formation
- Prograde spin-up during gravitational collapse
- Particle clustering in turbulence: Prediction of spatial and statistical properties with deep learning
- From Planetesimals to Dwarf Planets by Pebble Accretion
- Giant planet formation via pebble accretion across different stellar masses
- Planetesimal Growth in Evolving Protoplanetary Disks: Constraints from the Pebble Supply
- Aeolian erosion in protoplanetary discs: How impactful it is on dust evolution?
- Planet Mass Function around M stars at 1-10 au: A Plethora of sub-Earth mass objects
- Filament formation due to diffusive instabilities in dusty protoplanetary disks
- Long-term evolution of the temperature structure in magnetized protoplanetary disks and its implication for the dichotomy of planetary composition
- Exploring the conditions for forming planetesimals by the streaming instability and planetary systems by pebble accretion
- Effects of Stellar X-ray Photoevaporation on Planetesimal Formation via the Streaming Instability
- The Luminosity Function of Ultra-Faint Trans-Neptunian Objects Detected by JWST
- Evading the dust fragmentation barrier with the streaming instability in protoplanetary disks
- Dust Growth in ALMA Rings: II. Dusty Rossby Wave Instability
- Streaming instabilities in accreting protoplanetary disks: A parameter study
- Dust Dynamics in Hall-effected Protoplanetary Disks. I. Background Drift Hall Instability
- A close-encounter method for simulating the dynamics of planetesimals
- OSSOS finds an Exponential Cutoff in the Size Distribution of the Cold Classical Kuiper belt