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Table 2

CRIRES+ total production rates (Q) and mixing ratios with respect to water in C/2021 A1.

Date (dd.mm.yy) Molecule Q [1026 molecules s−1] [%]
29.12.2021 H2O 1213 ± 107 100
CH3OH 6.52 ± 1.46 0.54 ± 0.12
NH3 <7.3 <0.6
H2CO 3.46 ± 0.75 0.29 ± 0.06
C2H 1.98 ± 0.79 0.16 ± 0.07
CH4 3.24 ± 0.34 0.27 ± 0.03
6.75 ± 0.77 0.56 ± 0.06

01.01.2022 H2O 12 590 ± 409 100
CH3OH 47.2 ± 4.2 0.38 ± 0.03
NH3 <93.1 <0.74
H2CO 30 ± 3 0.24 ± 0.02
C2H6 23.6 ± 1.5 0.19 ± 0.01
CH4 28 ± 9 0.222 ± 0.007
HCl 3.93 ± 0.37 0.031 ± 0.003
47.0 ± 0.6 0.37 ± 0.01

03.01.22 H2O 7204 ± 341 100
CH3OH 30 ± 5 0.42 ± 0.07
NH3 <42 <0.6
H2CO 17.8 ± 2.2 0.25 ± 0.03
C2H6 15 ± 3 0.21 ± 0.03
CH4 19 ± 1 0.26 ± 0.01
HCl 1.75 ± 0.57 0.024 ± 0.008
44.6 ± 0.9 0.62 ± 0.01

Notes. Production rates are calculated for a rotational temperature of (87 ± 11) K, (102 ± 2) K, and (109 ± 2) K, and a growth factor of (1.83 ± 0.15), (1.87 ± 0.05), and (2.43 ± 0.10), for the first, second, and third observing nights, respectively. Upper limits are given at 3σ level (i.e., 99% confidence level).(†) A secondary species; production rates for NH2 were verified with the Planetary Spectrum Generator (PSG, Villanueva et al. 2018), which incorporate a daughter photo-dissociation model together with the NH2 g-factors (assuming NH3 as the parent species).

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