CO destruction in protoplanetary disk midplanes: inside versus outside the CO snow surface
Arthur D. Bosman, Ewine F. van Dishoeck, Catherine Walsh

TL;DR
This study investigates how chemical processing in protoplanetary disk midplanes affects CO abundance, revealing that CO destruction depends on temperature and ionization rates, which impacts gas mass estimates from CO observations.
Contribution
The paper demonstrates that CO chemical processing in disk midplanes can significantly reduce CO abundance, explaining discrepancies in gas mass measurements from CO and HD observations.
Findings
CO destruction is significant at temperatures below 30 K with typical ionization rates.
Warm disks around luminous stars show little CO processing, maintaining higher CO levels.
Cold disks around T Tauri stars can have CO abundances reduced by over 90%.
Abstract
CO has long been thought to be the best tracer to measure gas masses as it is readily detected at (sub)mm wavelengths in many disks. Inferred gas masses from CO in recent ALMA observations of large samples of disks seem inconsistent with their inferred dust masses. The derived gas-to-dust mass ratios from CO are 1-2 orders of magnitude lower than 100 even if photodissociation and freeze-out are included. Herschel measurements of HD line emission imply gas masses in line with gas-to-dust mass ratios of 100. This suggests that at least one additional mechanism is removing gaseous CO. Here we test the suggestion that the bulk of the CO is chemically processed and that the carbon is sequestered into less volatile species such as CO2, CH3OH and CH4 in the dense, shielded midplane regions of the disk. Using our gas-grain chemical code we perform a parameter exploration and follow the CO…
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