Forbidden atomic carbon, nitrogen, and oxygen emission lines in the water-poor comet C/2016 R2 (Pan-STARRS)

被引:18
作者
Raghuram, S. [1 ]
Hutsemekers, D. [2 ]
Opitom, C. [3 ]
Jehin, E. [2 ]
Bhardwaj, A. [1 ]
Manfroid, J. [2 ]
机构
[1] Phys Res Lab, Ahmadabad 380009, Gujarat, India
[2] Univ Liege, STAR Inst, Allee 6 Aout 19c, B-4000 Liege, Belgium
[3] ESO, Alonso de Cordova 3107, Santiago, Chile
关键词
comets: individual: C; 2016 R2 (Pan-STARRS); techniques: spectroscopic; molecular processes; atomic processes; VACUUM-ULTRAVIOLET PHOTODISSOCIATION; TRANSITION-PROBABILITIES; C(D-1) ATOMS; UV-SPECTRUM; CHEMISTRY; ORIGIN; O(1D); H2O; CO2; PHOTOCHEMISTRY;
D O I
10.1051/0004-6361/201936713
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Context. The N-2 and CO-rich and water-depleted comet C/2016 R2 (Pan-STARRS) - hereafter "C/2016 R2" - is a unique comet for detailed spectroscopic analysis.Aims. We aim to explore the associated photochemistry of parent species, which produces different metastable states and forbidden emissions, in this cometary coma of peculiar composition.Methods. We reanalyzed the high-resolution spectra of comet C/2016 R2 obtained in February 2018 using the UVES spectrograph of the European Southern Observatory Very Large Telescope. Various forbidden atomic emission lines of [CI], [NI], and [OI] were observed in the optical spectrum of this comet when it was at 2.8 au from the Sun. The observed forbidden emission intensity ratios are studied in the framework of a couple-chemistry emission model.Results. The model calculations show that CO2 is the major source of both atomic oxygen green and red doublet emissions in the coma of C/2016 R2 (while for most comets it is generally H2O), whereas, CO and N-2 govern the atomic carbon and nitrogen emissions, respectively. Our modeled oxygen green-to-red-doublet and carbon-to-nitrogen emission ratios are higher by a factor of three than what is found from observations. These discrepancies could be due to uncertainties associated with photon cross sections or unknown production and/or loss sources. Our modeled oxygen green-to-red-doublet emission ratio is close to what is seen in observations when we consider an O-2 abundance with a production rate of 30% relative to the CO production rate. We constrained the mean photodissociation yield of CO, producing C(S-1) at about 1%, a quantity which has not been measured in the laboratory. The collisional quenching is not a significant loss process for N(D-2) though its radiative lifetime is significant (10 h). Hence, the observed [NI] doublet-emission ratio ([NI] 5198/5200) of 1.22, which is smaller than the terrestrial measurement by a factor 1.4, is mainly due to the characteristic radiative decay of N(D-2).
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页数:15
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