Table 4
Comparison of the band strengths of this work with literature results.
| ν1,ν3 H2O (3292 cm−1) | ν3 12CO2 (2345 cm−1) | ν 12CO (2139 cm−1) | ||||||
|---|---|---|---|---|---|---|---|---|
| A′ (10−16 cm/molec) | ρ (g/cm3) | T (K) | A′ (10−17 cm/molec) | ρ (g/cm3) | T (K) | A′ (10−17 cm/molec) | ρ (g/cm3) | T (K) |
| 2.0 (a) | 0.63 | 10 | 9.45 (a) | 1.06 | 10 | 0.91 (a) | 0.91 | 10 |
| 2.0 (b) | 0.94 | 10 | 7.6 (f) | (1.64) * | 14 | 1.1 (h) | 1.029 | 30 |
| 1.7 (c) | 1 | 10 | 14 (c) | 1 | 10 | 1.12 (e) | 0.80 | 25 |
| 1.9 (d) | 1.1 | 15 | 7.6 (e) | 1.11 | 25 | 0.87 (i) | 0.876 | 20 |
| 1.5 (e) | 0.87 | 25 | 11.8 (g) | 1.28 | 10 | 1.1-0.88 (j) | 1.029 | 10 |
Notes. Literature results for the stretching modes of H2O, CO2, and CO in single-species ices. The ice densities used in each case are also shown.
(a)This work. (b)Hagen et al. (1981). (c)Hudgins et al. (1993). (d)Mastrapa et al. (2009). (e) Bouilloud et al. (2015). (f)Gerakines et al. (1995). (g) Gerakines & Hudson (2015). (h)Jiang et al. (1975). (i)Gonzalez Diaz et al. (2022). (j)Gerakines et al. (2023) (A′ dependent on spectral resolution. See the text). *Gerakines et al. (1995) scaled their results to the band strengths of Yamada & Person (1964) who performed measurements for ice deposited at 60-80 K and assumed ρ = 1.64g cm−3(see the text).
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