Grain growth signatures in the protoplanetary discs of Chamaeleon and Lupus

TL;DR

This study uses multi-wavelength observations of T Tauri stars in Chamaeleon and Lupus to identify signs of grain growth in protoplanetary discs, revealing widespread growth to centimeter sizes and complex emission mechanisms.

Contribution

It provides new observational evidence of grain growth up to cm sizes in protoplanetary discs and explores emission mechanisms through temporal monitoring.

Findings

90% detection rate at 3 and 7 mm

7 out of 11 sources show grain growth to mm sizes

Presence of excess emission from ionised wind and/or chromospheric activity

Abstract

We present ATCA results of a 3 and 7 mm continuum survey of 20 T Tauri stars in the Chamaeleon and Lupus star forming regions. This survey aims to identify protoplanetary discs with signs of grain growth. We detected 90% of the sources at 3 and 7 mm, and determined the spectral slopes, dust opacity indices and dust disc masses. We also present temporal monitoring results of a small sub-set of sources at 7, 15 mm and 3+6 cm to investigate grain growth to cm sizes and constrain emission mechanisms in these sources. Additionally, we investigated the potential correlation between grain growth signatures in the infrared (10 \mu m silicate feature) and millimetre (1-3 mm spectral slope, {\alpha}). Eleven sources at 3 and 7 mm have dominant thermal dust emission up to 7 mm, with 7 of these having a 1-3 mm dust opacity index less than unity, suggesting grain growth up to at least mm sizes. The Chamaeleon sources observed at 15 mm and beyond show the presence of excess emission from an ionised wind and/or chromo- spheric emission. Long-timescale monitoring at 7 mm indicated that cm-sized pebbles are present in at least four sources. Short-timescale monitoring at 15 mm suggests the excess emission is from thermal free-free emission. Finally, a weak correlation was found between the strength of the 10 \mum feature and {\alpha}, suggesting simultaneous dust evolution of the inner and outer parts of the disc. This survey shows that grain growth up to cm-sized pebbles and the presence of excess emission at 15 mm and beyond are common in these systems, and that temporal monitoring is required to disentangle these emission mechanisms.