Probing the Temperature Structure of the Inner Region of a Protoplanetary Disk
arXiv:2305.12598 · doi:10.1051/0004-6361/202346253
Abstract
Midplane heating induced by disk accretion plays a key role in determining the disk temperature particularly at the inner disk midplane where planets form. However, the efficiency of accretion heating has been not well constrained by observations. We construct two-dimensional models of the Class II disk around CW Tau, taking into account the midplane heating. The models are compared with the ALMA dust continuum observations at Bands 4, 6, 7 and 8, with an angular resolution of 0.1 arcsec. The observed brightness temperatures are almost wavelength-indenpendent at 10 au. We find that if the maximum dust size is , the brightness temperatures predicted by the model exceed the observed values, regardless of the efficiency of accretion heating. The low observed brightness temperatures can be explained if millimeter scattering reduces the intensity. If the disk is passive, needs to be either or few . The accretion heating significantly increases the brightness temperature particularly when , and hence needs to be either or few . The midplane temperature is expected to be 1.5-3 times higher than the observed brightness temperatures, depending on the models. The dust settling effectively increases the temperature of the dust responsible for the millimeter emission in the active disk, which makes the model with -sized dust overpredicts the brightness temperatures when strong turbulence is absent. Porous dust (porosity of 0.9) makes the accretion heating more efficient so that some sort of reduction in accretion heating is required. Future longer wavelength and higher angular resolution observations will help us constrain the heating mechanisms of the inner protoplanetary disks.
19 pages, 25 figures, accepted for publication in A&A
References in corpus (30)
- Gas- and dust evolution in protoplanetary disks
- Particle Stirring in Turbulent Gas Disks: Including Orbital Oscillations
- An Optical Spectroscopic Study of T Tauri Stars. I. Photospheric Properties
- Towards Chemical Constraints on Hot Jupiter Migration
- Planetesimal formation starts at the snow line
- Dust size distributions in coagulation/fragmentation equilibrium: Numerical solutions and analytical fits
- One Solution to the Mass Budget Problem for Planet Formation: Optically Thick Disks with Dust Scattering
- The Radial Distribution of Dust Particles in the HL Tau Disk from ALMA and VLA Observations
- How drifting and evaporating pebbles shape giant planets I: Heavy element content and atmospheric C/O
- 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
- Characterizing the dust content of disk substructures in TW Hya
- Temperature Structure in the Inner Regions of Protoplanetary Disks: Inefficient Accretion Heating Controlled by Nonideal Magnetohydrodynamics
- Distribution of solids in the rings of the HD 163296 disk: a multiwavelength study
- Relation between the luminosity of young stellar objects and their circumstellar environment
- GIARPS High-resolution Observations of T Tauri stars (GHOsT). IV. Accretion properties of the Taurus-Auriga young association
- Effects of scattering, temperature gradients, and settling on the derived dust properties of observed protoplanetary disks
- Carbon depletion observed inside T Tauri inner rims: Formation of icy, kilometer size planetesimals by 1 Myr
- Scattering-induced intensity reduction: large mass content with small grains in the inner region of the TW Hya disk
- Intrinsic polarisation of elongated porous dust grains
- Mapping Protoplanetary Disk Vertical Structure with CO Isotopologue Line Emission
- Jupiter's "Cold" Formation in the Protosolar Disk Shadow: An Explanation for the Planet's Uniformly Enriched Atmosphere
- Impact of Differential Dust Settling on the SED and Polarization: Application to the Inner Region of the HL Tau Disk
- Massive compact dust disk with a gap around CW Tau revealed by ALMA multi-band observations
- A global two-layer radiative transfer model for axisymmetric, shadowed protoplanetary disks
- Electric heating and angular momentum transport in laminar models of protoplanetary disks
- (Sub)millimeter Dust Polarization of Protoplanetary Disks from Scattering by Large Millimeter-Sized Irregular Grains
- The Roles of Dust Growth in the Temperature Evolution and Snow Line Migration in Magnetically Accreting Protoplanetary Disks
- The Molecular Composition of Shadowed Protosolar Disk Midplanes beyond the Water Snowline
- The growth of super-Earths: the importance of a self-consistent treatment of disc structures and pebble accretion
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