Table D.1
Spectra and band strengths used to construct the augmented dataset of linear combinations of pure ice spectra.
| Molecule | Experiment | Reference | Integrated band (cm−1) | Band strength (cm molecule−1) | Reference |
|---|---|---|---|---|---|
| H2O | OCdb #74–77 (10–100 K) | Hudgins et al. (1993) | 3330 ± 400 | 2.2 · 10−16 | Gerakines et al. (1995) |
| CO | LIDA #75 (15–25 K) Univap #G1 (10 K) | van Broekhuizen et al. (2006) Rocha & Pilling (2014) | 2139 ± 5 | 1.4 · 10−17 | Gerakines et al. (1995) |
| CO2 | OCdb #45–48 (10–70 K) | Hudgins et al. (1993) | 2343 ± 15 | 1.1 · 10−16 | Gerakines et al. (1995) |
| CH3OH | OCdb #37–40 (10–100 K) | Hudgins et al. (1993) | 1027 ± 50 | 1.8 · 10−17 | Hudgins et al. (1993) |
| NH3 | LIDA #116 (10–70 K) | Taban et al. (2003) | 1070 ± 60 | 2.1 · 10−17 | Sandford & Allamandola (1993) |
| CH4 | OCdb #42–44 (10–30 K) | Hudgins et al. (1993) | 1303 ± 10 | 8.4 · 10−18 | Boogert et al. (1997) |
Notes. The position of the integrated band is given as the centre plus/minus an approximate width. Band strengths were derived from the bibliographic work by Bouilloud et al. (2015), taking the corrected values corresponding to the closest temperature to the experimental spectrum for each case. Note: for CO we joined the spectrum #G1 from Univap with the spectra #75 from LIDA, to increase the effective temperature range.
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