Modeling dust growth in protoplanetary disks: The breakthrough case
arXiv:1406.0870 · doi:10.1051/0004-6361/201423708
Abstract
Simple toy models are often not sufficient to cover the complexity of the dust coagulation process, and a number of numerical approaches are therefore used, among which integration of the Smoluchowski equation and various versions of Monte Carlo algorithm are the most popular. In this paper, we directly compare the Smoluchowski and Monte Carlo approaches and we find a general agreement for most of the coagulation problems. However, for the sweep-up growth driven by the "lucky" breakthrough mechanism, the methods exhibit very different resolution dependencies. With too few mass bins, the Smoluchowski algorithm tends to overestimate the growth rate and the probability of breakthrough. The Monte Carlo method is less resolution dependent in the growth timescale aspect but it tends to underestimate the breakthrough chance due to its limited dynamic mass range. We discuss the features and drawbacks of both the approaches, which may limit their astrophysical applications.
arXiv comment7 pages, 4 figures; accepted for publication in Astronomy & Astrophysics
References in corpus (30)
- Coagulation, fragmentation and radial motion of solid particles in protoplanetary disks
- Dust coagulation in protoplanetary disks: a rapid depletion of small grains
- Gas- and dust evolution in protoplanetary 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
- Closed-form expressions for particle relative velocities induced by turbulence
- The Minimum-Mass Extrasolar Nebula: In-Situ Formation of Close-In Super-Earths
- Dust coagulation in protoplanetary disks: porosity matters
- Planetesimal formation by sweep-up: How the bouncing barrier can be beneficial to growth
- Dust Growth and Settling in Protoplanetary Disks and Disk Spectral Energy Distributions. I. Laminar Disks
- Adding particle collisions to the formation of asteroids and Kuiper belt objects via streaming instabilities
- Numerical Modeling of the Coagulation and Porosity Evolution of Dust Aggregates
- Breaking through: The effects of a velocity distribution on barriers to dust growth
- From dust to planetesimals: an improved model for collisional growth in protoplanetary disks
- High Velocity Dust Collisions: Forming Planetesimals in a Fragmentation Cascade with Final Accretion
- Low-velocity collisions of centimeter-sized dust aggregates
- A representative particle approach to coagulation and fragmentation of dust aggregates and fluid droplets
- The outcome of protoplanetary dust growth: pebbles, boulders, or planetesimals? III. Sedimentation driven coagulation inside the snow-line
- Free Collisions in a Microgravity Many-Particle Experiment III: The Collision Behavior of sub-Millimeter-Sized Dust Aggregates
- Monte Carlo simulation of particle interactions at high dynamic range: Advancing beyond the Googol
- Accretion among preplanetary bodies: the many faces of runaway growth
- Planetesimal formation via sweep-up growth at the inner edge of dead zones
- Bouncing Behavior of Microscopic Dust Aggregates
- The Physics of Protoplanetesimal Dust Agglomerates. V. Multiple Impacts of Dusty Agglomerates at Velocities Above the Fragmentation Threshold
- Preplanetary scavengers: Growing tall in dust collisions
- The physics of protoplanetesimal dust agglomerates. VII The low-velocity collision behavior of large dust agglomerates
- Dust Size Growth and Settling in a Protoplanetary Disk
- Growth and fragmentation of centimetre-sized dust aggregates: the dependence on aggregate size and porosity
- A method for coupling dynamical and collisional evolution of dust in circumstellar disks: the effect of a dead zone
- Growth of grains in Brown Dwarf disks
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- DustPy: A Python Package for Dust Evolution in Protoplanetary Disks
- Streaming Instability in Turbulent Protoplanetary Disks
- Global Modeling of Nebulae with Particle Growth, Drift and Evaporation Fronts. I: Methodology and Typical Results
- Collision velocity of dust grains in self-gravitating protoplanetary discs
- Dust properties across the CO snowline in the HD 163296 disk from ALMA and VLA observations
- Jumping the Gap: The Formation Conditions and Mass Function of Pebble-Pile Planetesimals
- Eulerian and modified Lagrangian approaches to multi-dimensional condensation and collection
- Analysis of Numerical Algorithms for Computing Rapid Momentum Transfers between the Gas and Dust in Simulations of Circumstellar Disks
- Evolution of porous dust grains in protoplanetary discs -- I. Growing grains
- The external photoevaporation of structured protoplanetary disks
- Changes in the metallicity of gas giant planets due to pebble accretion
- Dust growth, fragmentation and self-induced dust traps in PHANTOM
- The role of the drag force in the gravitational stability of dusty planet forming disc -- I. Analytical theory
- Dust Coagulation Reconciles Protoplanetary Disk Observations with the Vertical Shear Instability. I. Dust Coagulation and the VSI Dead Zone
- Tracking Dust Grains During Transport and Growth in Protoplanetary Disks
- Compaction during fragmentation and bouncing produces realistic dust grain porosities in protoplanetary discs
- Dust Accumulation near the Magnetospheric Truncation of Protoplanetary Discs around T Tauri Stars
- Breakthrough revisited: investigating the requirements for growth of dust beyond the bouncing barrier
- Dust Growth and Dynamics in Protoplanetary Nebulae: Implications for Opacity, Thermal Profile and Gravitational Instability
- The impact of dust evolution on the dead zone outer edge in magnetized protoplanetary disks
- Chemical evolution in planet-forming regions with growing grains
- Selective Aggregation Experiments on Planetesimal Formation and Mercury-Like Planets
- Dust grain shattering in protoplanetary discs: collisional fragmentation or rotational disruption?
- The motion of chondrules and other particles in a protoplanetary disc with temperature fluctuations
- On the Courant-Friedrichs-Lewy condition for numerical solvers of the coagulation equation
- Aeolian erosion in protoplanetary discs: How impactful it is on dust evolution?
- Effects of Stellar X-ray Photoevaporation on Planetesimal Formation via the Streaming Instability
- A fast tree algorithm for multi-component coagulation equation
- Origin of nucleosynthetic isotope variability in the NC reservoir: Evidence from Ti, Cr, and Mo isotopes