Multi-frequency analysis of the ALMA and VLA high resolution continuum observations of the substructured disc around CI Tau. Preference for sub-mm-sized low-porosity amorphous carbon grains
Francesco Zagaria, Stefano Facchini, Pietro Curone, Jonathan P. Williams, Cathie J. Clarke, Álvaro Ribas, Marco Tazzari, Enrique Macías, Richard A. Booth, Giovanni P. Rosotti, Leonardo Testi
TL;DR
This work uses high-resolution ALMA and VLA continuum data across 0.9 mm to 9.1 mm to jointly constrain dust temperature, density, and grain size in the CI Tau disc, explicitly testing how dust composition and porosity affect interpretive models. A two-step Bayesian radiative-transfer analysis that accounts for absorption and scattering shows that amorphous carbon grains with compact microphysics (Ricci, compact) best reproduce the observed surface-brightness and spectral-index profiles, yielding a near-constant maximum grain size of $a_{ m max}\approx (7.1\pm0.8)\times10^{-2}$ cm and marginal optical depths ($\tau_\nu \lesssim 1$) from 0.9 to 9.1 mm; porosity up to ~50% remains compatible, while graphite-rich mixtures are disfavored. The inferred dust density enhancements align with rings at ≈27, 60, and 152 au, and the grain-size distribution slope $q$ increases with radius, suggesting fragmentation- or bouncing-limited growth with ring confinement. The analysis also finds a substantial centimetre-wavelength non-dust contribution, likely including optically thick gyrosynchrotron emission, and estimates a modest pebble mass of ~31 $M_\oplus$ for the fiducial composition (with porosity allowing higher upper bounds up to ≈134 $M_\oplus$), implying that giant planet cores could be assembled in CI Tau under plausible efficiencies. These results demonstrate the power of combining multi-frequency, high-resolution data with physically constrained dust opacities to disentangle disc structure, dust evolution, and planet-formation potential, while highlighting the need for deeper cm-wavelength data and polarimetric observations to further tighten composition and porosity constraints.
Abstract
(Abridged) We present high angular resolution and sensitivity ALMA 3.1 mm and VLA 9.1 mm observations of the disc around CI Tau. These new data were combined with similar-resolution archival ALMA 0.9 and 1.3 mm observations and new and archival VLA 7.1 mm, 2.0, 3.0, and 6.0 cm photometry to study the properties of dust in this system. At wavelengths <3.1 mm, CI Tau's continuum emission is very extended and highly substructured (with three gaps, four rings, and two additional gap-ring pairs identified by non-parametric visibility modelling). Instead, the VLA 9.1 mm data are dominated by a bright central component, only partially (< 50%) due to dust emission, surrounded by a marginally detected, faint, and smooth halo. We fitted the ALMA and VLA 9.1 mm data together, adopting a physical model that accounts for the effects of dust absorption and scattering. For our fiducial dust composition ("Ricci" opacities), we retrieved a flat maximum grain size distribution across the disc radius of $(7.1\pm0.8)\times10^{-2}$ cm, that we tentatively attributed to fragmentation of fragile dust or bouncing. We tested, for the first time, the dependence of our results on the adopted dust composition model to assess which mixture can best reproduce the observations. We found that the "Ricci" opacities work better than the traditionally adopted "DSHARP" ones, while graphite-rich mixtures perform significantly worse. We also show that, for our fiducial composition, the data prefer low-porosity (< 70%) grains, in contrast with claims of highly porous aggregates in younger sources, which we tentatively justified by time-dependent compaction. Our results are in line with constraints from disc population synthesis models and naturally arise from CI Tau's peculiar spectral behaviour, making this disc an ideal target for deeper cm-wavelength and dust polarisation follow-ups.
