Streaming instability of multiple particle species II -- Numerical convergence with increasing particle number
arXiv:2106.15302 · doi:10.1051/0004-6361/202140690
Abstract
The streaming instability provides an efficient way of overcoming the growth barriers in the initial stages of the planet formation process. Considering the realistic case of a particle size distribution, the dynamics of the system is altered compared to the outcome of single size models. In order to understand the outcome of the multi-species streaming instability in detail, we perform a large parameter study in terms of particle number, particle size distribution, particle size range, initial metallicity and initial particle scale height. We study vertically stratified systems and determine the metallicity threshold for filament formation. We compare these with a system where the initial particle distribution is unstratified and find that its evolution follows that of its stratified counterpart. We find that change in particle number does not result in significant variation in the efficiency and timing of filament formation. We also see that there is no clear trend for how varying the size distribution in combination with particle size range changes the outcome of the multi-species streaming instability. Finally, we find that an initial metallicity of and both result in similar critical metallicity values for the start of filament formation. Our results show that the inclusion of a particle size distribution into streaming instability simulations, while changing the dynamics as compared to mono-disperse systems, does not result in overall unfavorable conditions for solid growth. We attribute the sub-dominant role of multiple species to the high-density conditions in the midplane, conditions under which also linear stability analysis predict little difference between single and multiple species.
arXiv comment13 pages, 13 figures, 2 tables, accepted to A\&A
References in corpus (27)
- Streaming Instabilities in Protoplanetary Disks
- First Results from High Angular Resolution ALMA Observations Toward the HL Tau Region
- 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
- Dynamics of Solids in the Midplane of Protoplanetary Disks: Implications for Planetesimal Formation
- Evidence of fast pebble growth near condensation fronts in the HL Tau protoplanetary disk
- 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
- Concentrating small particles in protoplanetary disks through the streaming instability
- How to form planetesimals from mm-sized chondrules and chondrule aggregates
- Dust size distributions in coagulation/fragmentation equilibrium: Numerical solutions and analytical fits
- Initial mass function of planetesimals formed by the streaming instability
- Particle-Gas Dynamics with Athena: Method and Convergence
- On the Outer Edges of Protoplanetary Dust Disks
- On the structure of the transition disk around TW Hya
- Dust Evolution Can Produce Scattered Light Gaps in Protoplanetary Disks
- Streaming Instability for Particle-Size Distributions
- Streaming Instability with Multiple Dust Species: I. Favourable Conditions for the Linear Growth
- Testing the Jeans, Toomre and Bonnor-Ebert concepts for planetesimal formation: 3D streaming instability simulations of diffusion regulated formation of planetesimals
- Polydisperse Streaming Instability I. Tightly coupled particles and the terminal velocity approximation
- Streaming Instability of Multiple Particle Species in Protoplanetary Disks
- Polydisperse Streaming Instability III. Dust evolution encourages fast instability
- Stratified and vertically-shearing streaming instabilities in protoplanetary disks
- Polydisperse Streaming Instability II. Methods for solving the linear stability problem
- Dense Particle Clouds in Laboratory Experiments in Context of Drafting and Streaming Instability
- Observation of aerodynamic instability in the flow of a particle stream in a dilute gas
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- Dust growth and evolution in protoplanetary disks
- Nucleation and growth of iron pebbles explains the formation of iron-rich planets akin to Mercury
- Streaming Instability with Multiple Dust Species: II. Turbulence and Dust-Gas Dynamics at Nonlinear Saturation
- Dust Settling and Clumping in MRI Turbulent Outer Protoplanetary Disks
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- The coexistence of the streaming instability and the vertical shear instability in protoplanetary disks: Planetesimal formation thresholds explored in two-dimensional global models
- Planetesimal Initial Mass Functions following Diffusion Regulated Gravitational Collapse
- Impact of Local Pressure Enhancements on Dust Concentration inTurbulent Protoplanetary Discs
- Resilience of Planetesimal Formation in Weakly-Reinforced Pressure Bumps
- Exciting spiral arms in protoplanetary discs from flybys
- Compaction during fragmentation and bouncing produces realistic dust grain porosities in protoplanetary discs
- Streaming instabilities in accreting and magnetized laminar protoplanetary disks
- Planetesimal formation via the streaming instability with multiple grain sizes
- Polydisperse Formation of Planetesimals: The dust size distribution in clumps
- Planetesimal formation via the streaming instability in simulations of infall dominated young disks
- On Secular Gravitational Instability in Vertically Stratified Disks
- Resonant drag instabilities for polydisperse dust. II. The streaming and settling instabilities
- Evading the dust fragmentation barrier with the streaming instability in protoplanetary disks
- Dust Dynamics in Hall-effected Protoplanetary Disks. I. Background Drift Hall Instability
- Planetesimal gravitational collapse in a gaseous environment: Thermal and dynamic evolution