Table 5
Rel. abundance of sulfur-bearing species with respect to water in [%].
| Comet | H2S | OCS | SO | SO2 | CS | CS2 | S2 |
|
|
|||||||
| 1P/Halley | 0.4[1] | 0.2[2] | |||||
| C/1995 O1 (Hale-Bopp) | 1.5[3] | 0.4[3] | 0.3[3,4] | 0.2[3] | 0.1[6] | 0.17[3] | 0.02[5] |
| C/1996 B2 (Hyakutake) | 0.8[7] | 0.1[8] | 0.1[6] | 0.1[7] | 0.01[9] | ||
| C/2001 A2 (LINEAR) | 1.15[10] | 0.07[10] | |||||
| 73P/SW3/B | 0.2–0.4[11] | 0.12–0.19[11] | |||||
| 73P/ SW3/C | 0.16–0.3[11] | 0.08–0.14[11] | |||||
| 9P/Tempel 1 before impact | 0.5[12] | <0.13[12] | |||||
| 67P summer hemisphere | 0.67[13] | 0.017[13] | 0.004[13] | 0.011[13] | a) | 0.003[13] | 0.0004[13] |
| 67P winter hemisphere | 1.75[13] | 0.098[13] | 0.0014[13] | 0.041[13] | a) | 0.024[13] | 0.0013[13] |
Notes. This table is based on Table 1 in Bockelée-Morvan et al. (2004), on Table 4 in Mumma & Charnley (2011) and on Table 3 in Radeva et al. (2013). References. [1] Eberhardt et al. (1994); [2] Feldman et al. (1987); [3] Bockelée-Morvan et al. (2000); [4] Lis et al. (1997b); [5] Despois et al. (2005); [6] Charnley & Rodgers (2008); [7] Biver et al. (1999); [8] Woodney et al. (1997); [9] Weaver et al. (1996); [10] Biver et al. (2006) (values at 1.1 AU); [11] Biver et al. (2008); [12] Biver et al. (2007); [13] this work; comments: a) CS cannot be resolved from CO2 by ROSINA.
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