The depletion of water during dispersal of planet-forming disk regions
A. Banzatti, K. M. Pontoppidan, C. Salyk, G. Herczeg, E. F. van, Dishoeck, G. A. Blake

TL;DR
This study uses high-resolution spectra to analyze water vapor emission in protoplanetary disks, revealing inside-out water depletion linked to molecular gaps and providing benchmarks for disk chemical evolution models.
Contribution
It presents the most comprehensive spectral dataset of water vapor in disks, establishing a new correlation between water emission and CO gas emission radius, and highlights water depletion as a key process inside the snow line.
Findings
Water emission decreases with increasing CO gas radius.
Disks around stars >1.5 M_sun have inner gaps with depleted molecular gas.
Infrared water spectra trace inside-out water depletion.
Abstract
We present a new velocity-resolved survey of 2.9 m spectra of hot HO and OH gas emission from protoplanetary disks, obtained with CRIRES at the VLT ( 3 km s). With the addition of archival Spitzer-IRS spectra, this is the most comprehensive spectral dataset of water vapor emission from disks ever assembled. We provide line fluxes at 2.9-33 m that probe from disk radii of au out to the region across the water snow line. With a combined dataset for 55 disks, we find a new correlation between HO line fluxes and the radius of CO gas emission as measured in velocity-resolved 4.7 m spectra (R), which probes molecular gaps in inner disks. We find that HO emission disappears from 2.9 m (hotter water) to 33 m (colder water) as R increases and expands out to the snow line radius. These results suggest that…
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