Dust properties across the CO snowline in the HD 163296 disk from ALMA and VLA observations

TL;DR

This study investigates grain growth and dust property variations across the CO snowline in the HD 163296 protoplanetary disk using ALMA and VLA data, revealing larger grains inside the snowline and possible dust processing at this boundary.

Contribution

It provides new observational evidence of grain size distribution changes across the CO snowline, indicating dust processing and transport mechanisms in the disk.

Findings

Large grains ($ extgreater$1 cm) inside 50 AU

Smaller grains beyond 150 AU

Enhanced large grain production at the CO snowline

Abstract

To characterize the mechanisms of planet formation it is crucial to investigate the properties and evolution of protoplanetary disks around young stars, where the initial conditions for the growth of planets are set. Our goal is to study grain growth in the disk of the young, intermediate mass star HD163296 where dust processing has already been observed, and to look for evidence of growth by ice condensation across the CO snowline, already identified in this disk with ALMA. Under the hypothesis of optically thin emission we compare images at different wavelengths from ALMA and VLA to measure the opacity spectral index across the disk and thus the maximum grain size. We also use a Bayesian tool based on a two-layer disk model to fit the observations and constrain the dust surface density. The measurements of the opacity spectral index indicate the presence of large grains and pebbles ($\geq$1 cm) in the inner regions of the disk (inside $\sim$50 AU) and smaller grains, consistent with ISM sizes, in the outer disk (beyond 150 AU). Re-analysing ALMA Band 7 Science Verification data we find (radially) unresolved excess continuum emission centered near the location of the CO snowline at $\sim$90 AU. Our analysis suggests a grain size distribution consistent with an enhanced production of large grains at the CO snowline and consequent transport to the inner regions. Our results combined with the excess in infrared scattered light found by Garufi et al. (2014) suggests the presence of a structure at 90~AU involving the whole vertical extent of the disk. This could be evidence for small scale processing of dust at the CO snowline.