Solving grain size inconsistency between ALMA polarization and VLA continuum in the Ophiuchus IRS 48 protoplanetary disk
arXiv:2007.15014 · doi:10.3847/1538-4357/abaab4
Abstract
The protoplanetary disk around Ophiuchus IRS 48 shows an azimuthally asymmetric dust distribution in (sub-)millimeter observations, which is interpreted as a vortex, where millimeter/centimeter-sized particles are trapped at the location of the continuum peak. In this paper, we present 860 m ALMA observations of polarized dust emission of this disk. The polarized emission was detected toward a part of the disk. The polarization vectors are parallel to the disk minor axis, and the polarization fraction was derived to be \%. These characteristics are consistent with models of self-scattering of submillimeter-wave emission, which indicate a maximum grain size of m. However, this is inconsistent with the previous interpretation of millimeter/centimeter dust particles being trapped by a vortex. To explain both, ALMA polarization and previous ALMA and VLA observations, we suggest that the thermal emission at 860 m wavelength is optically thick () at the dust trap with the maximum observable grain size of m rather than an optically thin case with cm dust grains. We note that we cannot rule out that larger dust grains are accumulated near the midplane if the 860 m thermal emission is optically thick.
22 pages, 17 figures, accepted for publication in ApJ
References in corpus (22)
- Particle Stirring in Turbulent Gas Disks: Including Orbital Oscillations
- Gaps, Rings, and Non-Axisymmetric Structures in Protoplanetary Disks - From Simulations to ALMA Observations
- One Solution to the Mass Budget Problem for Planet Formation: Optically Thick Disks with Dust Scattering
- Lupus disks with faint CO isotopologues: low gas/dust or large carbon depletion?
- The Radial Distribution of Dust Particles in the HL Tau Disk from ALMA and VLA Observations
- Protoplanetary disk rings and gaps across ages and luminosities
- The evidence of radio polarization induced by the radiative grain alignment and self-scattering of dust grains in a protoplanetary disk
- The anomalously low (sub)millimeter spectral indices of some protoplanetary disks may be explained by dust self-scattering
- Dust Trapping by Vortices in Transitional Disks: Evidence for Non-ideal MHD Effects in Protoplanetary Disks
- Spatially Resolved Magnetic Field Structure in the Disk of a T Tauri Star
- ALMA Reveals Transition of Polarization Pattern with Wavelength in HL Tau's Disk
- Effects of dust feedback on vortices in protoplanetary disks
- Submillimeter polarization observation of the protoplanetary disk around HD 142527
- A cavity and further radial substructures in the disk around HD~97048
- Dust-trapping vortices and a potentially planet-triggered spiral wake in the pre-transitional disk of V1247 Orionis
- Spatial separation of small and large grains in the transitional disk around the young star IRS 48
- Nonsticky Ice at the Origin of the Uniformly Polarized Submillimeter Emission from the HL Tau Disk
- HD 169142 in the eyes of ZIMPOL/SPHERE
- Radial variations in grain sizes and dust scale heights in the protoplanetary disk around HD 163296 revealed by ALMA polarization observation
- Investigating dust trapping in transition disks with millimeter-wave polarization
- ALMA observations of Elias 2-24: a protoplanetary disk with multiple gaps in the Ophiuchus Molecular Cloud
- Dust concentration and emission in protoplanetary disks vortices
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