TY - JOUR
T1 - Molecules with ALMA at planet-forming scales (MAPS). VI. Distribution of the small organics HCN, C2H, and H2CO
AU - Guzmán, Viviana V.
AU - Bergner, Jennifer B.
AU - Law, Charles J.
AU - Öberg, Karin I.
AU - Walsh, Catherine
AU - Cataldi, Gianni
AU - Aikawa, Yuri
AU - Bergin, Edwin A.
AU - Czekala, Ian
AU - Huang, Jane
AU - Andrews, Sean M.
AU - Loomis, Ryan A.
AU - Zhang, Ke
AU - Le Gal, Romane
AU - Alarcón, Felipe
AU - Ilee, John D.
AU - Teague, Richard
AU - Cleeves, L. Ilsedore
AU - Wilner, David J.
AU - Long, Feng
AU - Schwarz, Kamber R.
AU - Bosman, Arthur D.
AU - Pérez, Laura M.
AU - Ménard, François
AU - Liu, Yao
N1 - Funding Information:
We thank the anonymous referee for valuable comments that improved this manuscript. This paper makes use of the following ALMA data: ADS/ JAO.ALMA#2018.1.01055.L. ALMA is a partnership of ESO (representing its member states), NSF (USA) and NINS (Japan), together with NRC (Canada), MOST and ASIAA (Taiwan), and KASI (Republic of Korea), in cooperation with the Republic of Chile. The Joint ALMA Observatory is operated by ESO, AUI/NRAO and NAOJ. The National Radio Astronomy Observatory is a facility of the National Science Foundation operated under cooperative agreement by Associated Universities, Inc. V.V.G. acknowledges support from FONDECYT Iniciación 11180904 and ANID project Basal AFB-170002. J.B.B. acknowledges support from NASA through the NASA Hubble Fellowship grant No. HST-HF2-51429.001-A, awarded by the Space Telescope Science Institute, which is operated by the Association of Universities for Research in Astronomy, Inc., for NASA, under contract NAS5-26555. G.C. is supported by NAOJ ALMA Scientific Research grant code 2019-13B. C.J.L. acknowledges funding from the National Science Foundation Graduate Research Fellowship under grant DGE1745303. K.I.Ö acknowledges support from the Simons Foundation (SCOL No. 321183). K.I. Ö, E.A.B, F.A., and A.D.B. acknowledge support from NSF AAG grant No. 1907653. C.W. acknowledges financial support from the University of Leeds, STFC, and UKRI (grant Nos. ST/ R000549/1, ST/T000287/1, and MR/T040726/1). Y.A. acknowledges support by NAOJ ALMA Scientific Research grant code 2019-13B, and Grant-in-Aid for Scientific Research 18H05222 and 20H05847. S.M.A. and J.H. acknowledge funding support from the National Aeronautics and Space Administration under grant No. 17-XRP17 2-0012 issued through the Exoplanets Research Program. I.C. was supported by NASA through the NASA Hubble Fellowship grant HST-HF2-51405.001-A awarded by the Space Telescope Science Institute, which is operated by the Association of Universities for Research in Astronomy, Inc., for NASA, under contract NAS5-26555. J.H. acknowledges support for this work provided by NASA through the NASA Hubble Fellowship grant No. HST-HF2-51460.001-A awarded by the Space Telescope Science Institute, which is operated by the Association of Universities for Research in Astronomy, Inc., for NASA, under contract NAS5-26555. K.Z. acknowledges the support of the Office of the Vice Chancellor for Research and Graduate Education at the University of Wisconsin-Madison with funding from the Wisconsin Alumni Research Foundation, and the support of NASA through Hubble Fellowship grant HSTHF2- 51401.001. awarded by the Space Telescope Science Institute, which is operated by the Association of Universities for Research in Astronomy, Inc., for NASA, under contract NAS5-26555. R.L.G. acknowledges support from a CNES fellowship grant. J.D.I. acknowledges support from the Science and Technology Facilities Council of the United Kingdom (STFC) under ST/T000287/1. R.T. acknowledges support from the Smithsonian Institution as a Submillimeter Array (SMA) Fellow. L.I.C. gratefully acknowledges support from the David and Lucille Packard Foundation and Johnson & Johnson's WiSTEM2D Program. F.L. acknowledges support from the Smithsonian Institution as a Submillimeter Array (SMA) Fellow. K.R.S. acknowledges the support of NASA through the NASA Hubble Fellowship grant No. HST-HF2-51419.001 awarded by the Space Telescope Science Institute, which is operated by the Association of Universities for Research in Astronomy, Inc., for NASA, under contract NAS5-26555. L.M.P. acknowledges support from ANID project Basal AFB-170002 and from ANID FONDECYT Iniciación project No. 11181068. F.M. acknowledges support from ANR of France under contract ANR-16- CE31-0013 (Planet-Forming-Disks) and ANR-15-IDEX-02 (through CDP "Origins of Life"). Y.L. acknowledges the financial support by the Natural Science Foundation of China (grant No. 11973090).
Publisher Copyright:
© 2021. The American Astronomical Society. All rights reserved.
PY - 2021/11
Y1 - 2021/11
N2 - Small organic molecules, such as C2H, HCN, and H2CO, are tracers of the C, N, and O budget in protoplanetary disks. We present high-angular-resolution (10-50 au) observations of C2H, HCN, and H2CO lines in five protoplanetary disks from the Molecules with ALMA at Planet-forming Scales (MAPS) ALMA Large Program. We derive column density and excitation temperature profiles for HCN and C2H, and find that the HCN emission arises in a temperate (20-30 K) layer in the disk, while C2H is present in relatively warmer (20-60 K) layers. In the case of HD 163296, we find a decrease in column density for HCN and C2H inside one of the dust gaps near ~83 au, where a planet has been proposed to be located. We derive H2CO column density profiles assuming temperatures between 20 and 50 K, and find slightly higher column densities in the colder disks around T Tauri stars than around Herbig Ae stars. The H2CO column densities rise near the location of the CO snowline and/or millimeter dust edge, suggesting an efficient release of H2CO ices in the outer disk. Finally, we find that the inner 50 au of these disks are rich in organic species, with abundances relative to water that are similar to cometary values. Comets could therefore deliver water and key organics to future planets in these disks, similar to what might have happened here on Earth. This paper is part of the MAPS special issue of the Astrophysical Journal Supplement.
AB - Small organic molecules, such as C2H, HCN, and H2CO, are tracers of the C, N, and O budget in protoplanetary disks. We present high-angular-resolution (10-50 au) observations of C2H, HCN, and H2CO lines in five protoplanetary disks from the Molecules with ALMA at Planet-forming Scales (MAPS) ALMA Large Program. We derive column density and excitation temperature profiles for HCN and C2H, and find that the HCN emission arises in a temperate (20-30 K) layer in the disk, while C2H is present in relatively warmer (20-60 K) layers. In the case of HD 163296, we find a decrease in column density for HCN and C2H inside one of the dust gaps near ~83 au, where a planet has been proposed to be located. We derive H2CO column density profiles assuming temperatures between 20 and 50 K, and find slightly higher column densities in the colder disks around T Tauri stars than around Herbig Ae stars. The H2CO column densities rise near the location of the CO snowline and/or millimeter dust edge, suggesting an efficient release of H2CO ices in the outer disk. Finally, we find that the inner 50 au of these disks are rich in organic species, with abundances relative to water that are similar to cometary values. Comets could therefore deliver water and key organics to future planets in these disks, similar to what might have happened here on Earth. This paper is part of the MAPS special issue of the Astrophysical Journal Supplement.
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U2 - 10.3847/1538-4365/ac1440
DO - 10.3847/1538-4365/ac1440
M3 - Article
AN - SCOPUS:85119685233
SN - 0067-0049
VL - 257
JO - Astrophysical Journal, Supplement Series
JF - Astrophysical Journal, Supplement Series
IS - 1
M1 - 6
ER -