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Table 3

Ice column densities and abundances with respect to H2O ice towards Ced 110 IRS4A and IRS4B compared with literature values.

Species Nice (1017 cm−2) XH2O(%)${X_{{{\rm{H}}_{\rm{2}}}{\rm{O}}}}\left( \% \right)$ Literature (% H2O)

IRS4A(a) IRS4B IRS4A IRS4B LYSOs (b) NIR38 (e) J110621 (f) Comet 67P/C-G (f)
H2O 45.2±2.3 63.548.169.3$63.5_{48.1}^{69.3}$ 100 100 100 100 100 100
12CO2 11.19.715.0$11.1_{9.7}^{15.0}$ 7.16.87.9$7.1_{6.8}^{7.9}$ 24.5 11.2 282337$28_{23}^{37}$ 20.17.338.7$20.1_{7.3}^{38.7}$ 13.06.119.0$13.0_{6.1}^{19.0}$ 4.7±1.4
13CO2 0.1±0.01 0.2 0.3 0.3
12CO 6.65.97.2$6.6_{5.9}^{7.2}$ 10.4 211235$21_{12}^{35}$ 43.120.065.4$43.1_{20.0}^{65.4}$ 27.513.047.2$27.5_{13.0}^{47.2}$ 3.1±0.9
CH4 0.780.521.0(0.800.551.12)$0.78_{0.52}^{1.0}\left( {0.80_{0.55}^{1.12}} \right)$ 1.7 (1.8) 4.536$4.5_3^6$ 2.61.44.8$2.6_{1.4}^{4.8}$ 1.90.92.4$1.9_{0.9}^{2.4}$ 0.340±0.07
SO2 0.110.060.17(0.090.070.15)$0.11_{0.06}^{0.17}\left( {0.09_{0.07}^{0.15}} \right)$ 0.2 (0.2) 0.2c 0.05 0.04 0.127±0.100
NH3 2.881.903.86(0.0)$2.88_{1.90}^{3.86}(0.0)$ 5.72.16.3$5.7_{2.1}^{6.3}$ 6.4 (0.0) 8.9 648$6_4^8$ 4.42.110.6$4.4_{2.1}^{10.6}$ 5.02.58.6$5.0_{2.5}^{8.6}$ 0.67±0.20
HCOOH 0.920.561.28(0.410.220.61)$0.92_{0.56}^{1.28}\left( {0.41_{0.22}^{0.61}} \right)$ 2.0 (0.9) <0.5–4(d), 1.0(c) 0.013±0.008
CH3OH 0.940.701.3(0.890.671.05)$0.94_{0.70}^{1.3}\left( {0.89_{0.67}^{1.05}} \right)$ 3.852.75.2$3.85_{2.7}^{5.2}$ 2.1 (2.0) 6.1 6512$6_5^{12}$ 8.92.617.7$8.9_{2.6}^{17.7}$ 3.92.58.2$3.9_{2.5}^{8.2}$ 0.21±0.06
OCN 0.920.461.4(0.630.350.82)$0.92_{0.46}^{1.4}\left( {0.63_{0.35}^{0.82}} \right)$ 2.0 (1.4) 0.60.40.8,1.2$0.6_{0.4}^{0.8},1.2$(c) 0.3 0.3
N2O 0.810.531.10(0.850.551.21)$0.81_{0.53}^{1.10}\left( {0.85_{0.55}^{1.21}} \right)$ 1.8 (1.9)

Upper limits

NH4+${\rm{NH}}_4^ + $ <6.5 <14.3 11715$11_7^15$ <6 <8
H2CO <3.4 <7.5 ∼6 0.32±0.1

Notes. This table shows literature values for LYSOs, the two field stars probing lines of sight towards Chamaleon I (NIR38 and J110621), and the comet 67P/G-C. (a)Values inside parentheses are calculated based on the data after polynomial silicate subtraction. (b)When not indicated otherwise, the values correspond to the median and lower and upper quartile values from summarised by Boogert et al. (2015), (c)Rocha et al. (2024b): IRAS 2A, (d)Öberg et al. (2011), (e)McClure et al. (2023), (f)Rubin et al. (2019).

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