Rapid Evolution of Volatile CO from the Protostellar Disk Stage to the Protoplanetary Disk Stage

preprint2020arXivOpen access

Abstract

Recent observations show that the CO gas abundance, relative to H2_2, in many 1-10 Myr old protoplanetary disks may be heavily depleted, by a factor of 10-100 compared to the canonical interstellar medium value of 10−4^{-4}. When and how this depletion happens can significantly affect compositions of planetesimals and atmospheres of giant planets. It is therefore important to constrain if the depletion occurs already at the earliest protostellar disk stage. Here we present spatially resolved observations of C18^{18}O, C17^{17}O, and 13^{13}C18^{18}O JJ=2-1 lines in three protostellar disks. We show that the C18^{18}O line emits from both the disk and the inner envelope, while C17^{17}O and 13^{13}C18^{18}O lines are consistent with a disk origin. The line ratios indicate that both C18^{18}O and C17^{17}O lines are optically thick in the disk region, and only 13^{13}C18^{18}O line is optically thin. The line profiles of the 13^{13}C18^{18}O emissions are best reproduced by Keplerian gaseous disks at similar sizes as their mm-continuum emissions, suggesting small radial separations between the gas and mm-sized grains in these disks, in contrast to the large separation commonly seen in protoplanetary disks. Assuming a gas-to-dust ratio of 100, we find that the CO gas abundances in these protostellar disks are consistent with the ISM abundance within a factor of 2, nearly one order of magnitude higher than the average value of 1-10 Myr old disks. These results suggest that there is a fast, ∼\sim1 Myr, evolution of the abundance of CO gas from the protostellar disk stage to the protoplanetary disk stage.

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