4.7 Article

An ALMA Survey of DCN/H13CN and DCO+/H13CO+ in Protoplanetary Disks

Journal

ASTROPHYSICAL JOURNAL
Volume 835, Issue 2, Pages -

Publisher

IOP PUBLISHING LTD
DOI: 10.3847/1538-4357/835/2/231

Keywords

astrochemistry; ISM: molecules; protoplanetary disks; radio lines: ISM

Funding

  1. Gaia Multilateral Agreement
  2. National Science Foundation Graduate Research Fellowship [DGE-1144152]
  3. Simons Collaboration on the Origins of Life (SCOL)
  4. David and Lucile Packard Foundation
  5. EU A-ERC grant [291141 CHEMPLAN]
  6. Grants-in-Aid for Scientific Research [16H00931] Funding Source: KAKEN

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The deuterium enrichment of molecules is sensitive to their formation environment. Constraining patterns of deuterium chemistry in protoplanetary disks is therefore useful for probing how material is inherited or reprocessed throughout the stages of star and planet formation. We present ALMA observations at similar to 0.6 resolution of DCO+, (HCO+)-C-13, DCN, and (HCN)-C-13 in the full disks around T Tauri stars AS 209 and IM Lup, in the transition disks around T Tauri stars V4046 Sgr and LkCa 15, and in the full disks around Herbig Ae stars MWC 480 and HD 163296. We also present ALMA observations of HCN in the IM Lup disk. DCN, DCO+, and (HCO+)-C-13 are detected in all disks, and (HCN)-C-13 in all but the IM Lup disk. We find efficient deuterium fractionation for the sample, with estimates of disk-averaged DCO+/HCO+ and DCN/HCN abundance ratios ranging from similar to 0.02-0.06 and similar to 0.005-0.08, respectively, which is comparable to values reported for other interstellar environments. The relative distributions of DCN and DCO+ vary between disks, suggesting that multiple formation pathways may be needed to explain the diverse emission morphologies. In addition, gaps and rings observed in both (HCO+)-C-13 and DCO+ emission provide new evidence that DCO+ bears a complex relationship with the location of the midplane CO snowline.

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