Volatile depletion in the TW Hydrae disk atmosphere
Fujun Du, Edwin A. Bergin, and Michiel R. Hogerheijde

TL;DR
This study explains the apparent discrepancy in TW Hya's disk gas mass measurements by proposing volatile depletion in the outer disk's atmosphere, caused by solid bodies trapping carbon and oxygen, affecting gas and dust evolution models.
Contribution
It introduces a model where volatile depletion in the outer disk atmosphere accounts for the low gas mass inferred from observations, linking dust grain dynamics and planetesimal formation.
Findings
Outer disk atmosphere shows reduced carbon and oxygen abundances.
Main volatile reservoirs are locked in solid bodies near the midplane.
Inner disk may have enhanced carbon and oxygen due to inward migration.
Abstract
An abundance decrease in carbon- and oxygen-bearing species relative to dust has been frequently found in planet-forming disks, which can be attributed to an overall reduction of gas mass. However, in the case of TW Hya, the only disk with gas mass measured directly with HD rotational lines, the inferred gas mass (0.005 solar mass) is significantly below the directly measured value (0.05 solar mass). We show that this apparent conflict can be resolved if the elemental abundances of carbon and oxygen are reduced in the upper layers of the outer disk but are normal elsewhere (except for a possible enhancement of their abundances in the inner disk). The implication is that in the outer disk, the main reservoir of the volatiles (CO, water, ...) resides close to the midplane, locked up inside solid bodies that are too heavy to be transported back to the atmosphere by…
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