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The Unexpectedly Bright Comet C-2012 F6 (Lemmon) Unveiled at Near-Infrared WavelengthsWe acquired near-infrared spectra of the Oort cloud comet C/2012 F6 (Lemmon) at three different heliocentric distances (R h) during the comet's 2013 perihelion passage, providing a comprehensive measure of the outgassing behavior of parent volatiles and cosmogonic indicators. Our observations were performed pre-perihelion at R h = 1.2 AU with CRIRES (on 2013 February 2 and 4), and post-perihelion at R h = 0.75 AU with CSHELL (on March 31 and April 1) and R h = 1.74 AU with NIRSPEC (on June 20). We detected 10 volatile species (H2O, OH* prompt emission, C2H6, CH3OH, H2CO, HCN, CO, CH4, NH3, and NH2), and obtained upper limits for two others (C2H2 and HDO). One-dimensional spatial profiles displayed different distributions for some volatiles, confirming either the existence of polar and apolar ices, or of chemically distinct active vents in the nucleus. The ortho-para ratio for water was 3.31 +/- 0.33 (weighted mean of CRIRES and NIRSPEC results), implying a spin temperature >37 K at the 95% confidence limit. Our (3σ) upper limit for HDO corresponds to D/H < 2.45 × 10-3 (i.e., <16 Vienna Standard Mean Ocean Water, VSMOW). At R h = 1.2 AU (CRIRES), the production rate for water was Q(H2O) = 1.9 +/- 0.1 × 1029 s-1 and its rotational temperature was T rot ~ 69 K. At R h = 0.75 AU (CSHELL), we measured Q(H2O) = 4.6 +/- 0.6 × 1029 s-1 and T rot = 80 K on March 31, and 6.6 +/- 0.9 × 1029 s-1 and T rot = 100 K on April 1. At R h = 1.74 AU (NIRSPEC), we obtained Q(H2O) = 1.1 +/- 0.1 × 1029 s-1 and T rot ~ 50 K. The measured volatile abundance ratios classify comet C/2012 F6 as rather depleted in C2H6 and CH3OH, while HCN, CH4, and CO displayed abundances close to their median values found among comets. H2CO was the only volatile showing a relative enhancement. The relative paucity of C2H6 and CH3OH (with respect to H2O) suggests formation within warm regions of the nebula. However, the normal abundance of HCN and hypervolatiles CH4 and CO, and the enhancement of H2CO, may indicate a possible heterogeneous nucleus of comet C/2012 F6 (Lemmon), possibly as a result of radial mixing within the protoplanetary disk
Document ID
20150006821
Acquisition Source
Goddard Space Flight Center
Document Type
Reprint (Version printed in journal)
Authors
Paganini, Lucas
(Catholic Univ. of America Washington, DC, United States)
Disanti, Michael A.
(NASA Goddard Space Flight Center Greenbelt, MD United States)
Mumma, Michael J.
(NASA Goddard Space Flight Center Greenbelt, MD United States)
Villanueva, Geronimo L.
(Catholic Univ. of America Washington, DC, United States)
Bonev, Boncho P.
(Catholic Univ. of America Washington, DC, United States)
Keane, Jacqueline V.
(Hawaii Univ. Honolulu, HI, United States)
Gibb, Erika L.
(Missouri Univ. Saint Louis, MO, United States)
Boehnhardt, Hermann
(Max-Planck-Inst. fuer Sonnensystemforschung Lindau, Germany)
Meech, Karen J.
(Hawaii Univ. Honolulu, HI, United States)
Date Acquired
April 27, 2015
Publication Date
December 6, 2013
Publication Information
Publication: The Astronomical Journal
Publisher: American Astronomical Society
Volume: 147
Issue: 1
Subject Category
Astronomy
Report/Patent Number
GSFC-E-DAA-TN21971
Funding Number(s)
CONTRACT_GRANT: NCC5-538
CONTRACT_GRANT: NNA09DA77A
CONTRACT_GRANT: NNX13AD84A
CONTRACT_GRANT: NNX14AC98A
Distribution Limits
Public
Copyright
Public Use Permitted.
Keywords
C/2012 F6
comets
Oort Cloud
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