Indications of Rapid Dust Formation in the Inner Region of a Protoplanetary Disk
Thanawuth Thanathibodee, Catherine Espaillat, Nuria Calvet, Zhaohuan Zhu, Julalak Nammanee, Caeley Pittman, Maire Volz
TL;DR
The study targets rapid inner-disk dust evolution in CVSO 1942 by comparing a 2024 JWST/MIRI spectrum with archival Spitzer/IRS data and NEOWISE photometry, revealing a mid-infrared flux increase by a factor of ~2 at $λ \,\leq\, 10\,\mu$m over a timescale of $\lesssim$2 weeks. The excess is well modeled by warm (≈1400 K), optically thick dust near the sublimation radius, with an emitting area of about $A \approx 1.93\times10^{23}$ cm$^2$ and a minimum dust mass $M_d \gtrsim 9.7\times10^{20}$ g (≈$4.9\times10^{-13}$ M$_{\odot}$), while the 10 μm silicate feature remains unchanged. The authors argue for rapid in situ dust formation, possibly from planetesimal collisions, as the most plausible mechanism, with alternative explanations such as accretion bursts or drifting dust clumps disfavored by the data. This provides evidence for active dust production at the inner disk edge and hints at the late stages of disk evolution toward a debris-disk-like state, underscoring the need for multi-timescale monitoring. Absent longer-term data, the exact triggering process remains uncertain but is consistent with in situ events in a low-accretion, transitional disk system.
Abstract
We report a significant increase in mid-infrared emission $\leq10$ $μ$m in a transitional disk. The 2024 JWST/MIRI observation of the disk around CVSO 1942 reveals flux increase by a factor of two at $λ\leq10$ $μ$m, compared to the near photospheric flux level observed with Spitzer/IRS in 2005. No significant change in flux at $\gtrsim15$ $μ$m is detected in the spectra. Comparing the MIRI/MRS spectrum and NEOWISE photometry, we found that this $\leq10$ $μ$m flux increase occurs on a timescale of 2 weeks and is consistent with the presence of warm (1,400 K), optically thick, large ($\gtrsim1$ $μ$m) dust grains near the dust sublimation radius. We propose that this rapid dust appearance may indicate in situ dust formation, possibly from planetesimal collisions in the inner disk.
