Self-consistent ring model in protoplanetary disks: temperature dips and substructure formation
arXiv:2110.00858 · doi:10.3847/1538-4357/ac2c82
Abstract
Rings and gaps are ubiquitous in protoplanetary disks. Larger dust grains will concentrate in gaseous rings more compactly due to stronger aerodynamic drag. However, the effects of dust concentration on the ring's thermal structure have not been explored. Using MCRT simulations, we self-consistently construct ring models by iterating the ring's thermal structure, hydrostatic equilibrium, and dust concentration. We set up rings with two dust populations having different settling and radial concentration due to their different sizes. We find two mechanisms that can lead to temperature dips around the ring. When the disk is optically thick, the temperature drops outside the ring, which is the shadowing effect found in previous works adopting a single-dust population in the disk. When the disk is optically thin, a second mechanism due to excess cooling of big grains is found. Big grains cool more efficiently, which leads to a moderate temperature dip within the ring where big dust resides. This dip is close to the center of the ring. Such temperature dip within the ring can lead to particle pile-up outside the ring and feedback to the dust distribution and thermal structure. We couple the MCRT calculations with a 1D dust evolution model and show that the ring evolves to a different shape and may even separate to several rings. Overall, dust concentration within rings has moderate effects on the disk's thermal structure, and self-consistent model is crucial not only for protoplanetary disk observations but also for planetesimal and planet formation studies.
17 pages, 11 figures, accepted by ApJ
References in corpus (22)
- The NumPy array: a structure for efficient numerical computation
- Particle Stirring in Turbulent Gas Disks: Including Orbital Oscillations
- Gaps, Rings, and Non-Axisymmetric Structures in Protoplanetary Disks - From Simulations to ALMA Observations
- Evidence of fast pebble growth near condensation fronts in the HL Tau protoplanetary disk
- Molecules with ALMA at Planet-forming Scales (MAPS) I: Program Overview and Highlights
- A Circumplanetary Disk Around PDS70c
- Direct mapping of the temperature and velocity gradients in discs. Imaging the vertical CO snow line around IM Lupi
- One Solution to the Mass Budget Problem for Planet Formation: Optically Thick Disks with Dust Scattering
- The Disk Substructures at High Angular Resolution Project (DSHARP): III. Spiral Structures in the Millimeter Continuum of the Elias 27, IM Lup, and WaOph 6 Disks
- The Radial Distribution of Dust Particles in the HL Tau Disk from ALMA and VLA Observations
- Highly structured disk around the planet host PDS 70 revealed by high-angular resolution observations with ALMA
- Molecules with ALMA at Planet-forming Scales (MAPS) IV: Emission Surfaces and Vertical Distribution of Molecules
- The anomalously low (sub)millimeter spectral indices of some protoplanetary disks may be explained by dust self-scattering
- Planet formation by pebble accretion in ringed disks
- Dust-driven viscous ring-instability in protoplanetary disks
- Annular substructures in the transition disks around LkCa 15 and J1610
- Giant planet formation at the pressure maxima of protoplanetary disks II. A hybrid accretion scenario
- Observational Signatures of Tightly Wound Spirals Driven by Buoyancy Resonances in Protoplanetary Disks
- Dual-Wavelength ALMA Observations of Dust Rings in Protoplanetary Disks
- Rapid Formation of Jupiter and Wide-Orbit Exoplanets in Disks with Pressure Bumps
- Survival of ALMA Rings in the Absence of Pressure Maxima
- High resolution observations of molecular emission lines toward the CI Tau proto-planetary disc: planet-carved gaps or shadowing?
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- Porous Dust Particles in Protoplanetary Disks: Application to the HL Tau Disk
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- No Significant Correlation between Line-emission and Continuum Substructures in the Molecules with ALMA at Planet-forming Scales Program
- Distributions of gas and small and large grains in the LkH disk trace a young planetary system
- Evidence for a Sharp CO Snowline Transition in a Protoplanetary Disk and Implications for Millimeter-wave Observations of CO Isotopologues
- On the origin of transition disk cavities: Pebble-accreting protoplanets vs Super-Jupiters