Particle transport in evolving protoplanetary disks: Implications for results from Stardust
arXiv:1007.1989 · doi:10.1088/0004-637X/719/2/1633
Abstract
Samples returned from comet 81P/Wild 2 by Stardust confirm that substantial quantities of crystalline silicates were incorporated into the comet at formation. We investigate the constraints that this observation places upon protoplanetary disk physics, assuming that outward transport of particles processed at high temperatures occurs via advection and turbulent diffusion in an evolving disk. We also look for constraints on particle formation locations. Our results are based upon 1D disk models that evolve with time under the action of viscosity and photoevaporation, and track solid transport using an ensemble of individual particle trajectories. We find that two classes of disk model are consistent with the Stardust findings. One class features a high particle diffusivity (a Schmidt number Sc < 1), which suffices to diffuse particles up to 20 microns in size outward against the mean gas flow. For Sc > 1, such models are unlikely to be viable, and significant outward transport requires that the particles of interest settle into a midplane layer that experiences an outward gas flow. In either class of models, the mass of inner disk material that reaches the outer disk is a strong function of the disk's initial compactness. Hence, models of grain transport within steady-state disks underestimate the efficiency of outward transport. Neither model results in sustained outward transport of very large particles exceeding a mm in size. We show that the transport efficiency generally falls off rapidly with time. Hence, high-temperature material must be rapidly incorporated into icy bodies to avoid fallback, and significant radial transport may only occur during the initial phase of rapid disk evolution. It may also vary substantially between disks depending upon their initial mass distributions. We discuss implications for Spitzer observations of crystalline silicates in T Tauri disks.
ApJ, in press
References in corpus (10)
- Particle Stirring in Turbulent Gas Disks: Including Orbital Oscillations
- Accretion disc viscosity: how big is alpha?
- Dust dynamics during protoplanetary disc clearing
- Crystalline silicates and dust processing in the protoplanetary disks of the Taurus young cluster
- Two-Dimensional Transport of Solids in Viscous Protoplanetary Disks
- Accretion in protoplanetary disks: the imprint of core properties
- Growth and migration of solids in evolving protostellar disks I: Methods and Analytical tests
- Mixing in the Solar Nebula: Implications for Isotopic Heterogeneity and Large-Scale Transport of Refractory Grains
- Crystalline silicates as a probe of disk formation history
- Dust crystallinity in protoplanetary disks: the effect of diffusion/viscosity ratio
Cited by in corpus (40)
- A simple model for the evolution of the dust population in protoplanetary disks
- Wind-driven Accretion in Protoplanetary Disks. I: Suppression of the Magnetorotational Instability and Launching of the Magnetocentrifugal Wind
- Global Simulations of the Inner Regions of Protoplanetary Disks with Comprehensive Disk Microphysics
- Global Evolution of an Accretion Disk with Net Vertical Field: Coronal Accretion, Flux Transport, and Disk Winds
- C/O and Snowline Locations in Protoplanetary Disks: The Effect of Radial Drift and Viscous Gas Accretion
- Carbon-rich planet formation in a solar composition disk
- Dust Transport in MRI Turbulent Disks: Ideal and Non-ideal MHD with Ambipolar Diffusion
- Global Modeling of Nebulae with Particle Growth, Drift and Evaporation Fronts. I: Methodology and Typical Results
- Utilitarian Opacity Model for Aggregate Particles in Protoplanetary Nebulae and Exoplanet Atmospheres
- Gas and multi-species dust dynamics in viscous protoplanetary discs: the importance of the dust back-reaction
- Probing the Protosolar Disk Using Dust Filtering at Gaps in the Early Solar System
- On the aerodynamic redistribution of chondrite components in protoplanetary disks
- Meridional circulation in turbulent protoplanetary disks
- The imprint of photoevaporation on edge-on discs
- 3D Lagrangian turbulent diffusion of dust grains in a protoplanetary disk: method and first applications
- The measured compositions of Uranus and Neptune from their formation on the CO iceline
- Formulas for Radial Transport in Protoplanetary Disks
- The Tidal Downsizing hypothesis for planet formation and the composition of Solar System comets
- Radial transport of refractory inclusions and their preservation in the dead zone
- Evolution of the Solar Nebula. IX. Gradients in the Spatial Heterogeneity of the Short-Lived Radioisotopes Fe and Al and the Stable Oxygen Isotopes
- Snow-lines as probes of turbulent diffusion in protoplanetary discs
- Global variation of the dust-to-gas ratio in evolving protoplanetary discs
- Transport of solids in protoplanetary disks: Comparing meteorites and astrophysical models
- On vertical variations of gas flow in protoplanetary disks and their impact on the transport of solids
- Gravitoviscous protoplanetary disks with a dust component. V. The dynamic model for freeze-out and sublimation of volatiles
- Time evolution of a viscous protoplanetary disk with a free geometry: toward a more self-consistent picture
- The Future of Stardust Science
- The circulation of dust in protoplanetary discs and the initial conditions of planet formation
- Photophoretic transport of hot minerals in the solar nebula
- Outward Motion of Porous Dust Aggregates by Stellar Radiation Pressure in Protoplanetary Disks
- Radial Transport and Meridional Circulation in Accretion Disks
- Absorption Efficiencies of Forsterite. I: DDA Explorations in Grain Shape and Size
- Dust Transport in Protoplanetary Disks with Wind-driven Accretion
- SOFIA Infrared Spectrophotometry of Comet C/2012 K1 (Pan-STARRS)
- Inner dusty regions of protoplanetary discs - I. High resolution temperature structure
- Refractory Metal Nuggets -- Formation of the First Condensates in the Solar Nebula
- Asteroids and Comets
- Dust processing in protoplanetary envelopes as the origin of hot minerals in comets
- Comets in context: Comparing comet compositions with protosolar nebula models
- On the crystallinity of silicate dust in evolving protoplanetary disks due to magnetically driven disk winds