SO
Sulphur monoxide
Flags: Detected, RATE12
Empirical: OS
Mass: 48 amu
Dipole moment: 1.550 D
Heat of formation: 5.0 kJ mol-1
Added to system: 2003-04-28 18:00:49
Reactions: Formation | Destruction
58 SO formation reactions
Reaction | α | β | γ | Tl - Tu (K) | |
---|---|---|---|---|---|
1 | O + S- → SO + e- | 1.00e-10 | 0.00 | 0.00 | 10 - 41000 |
2 | Mg + SO+ → SO + Mg+ | 1.00e-10 | 0.00 | 0.00 | 10 - 41000 |
3 | NH3 + SO+ → SO + NH3+ | 1.30e-9 | -0.50 | 0.00 | 10 - 41000 |
4 | Na + SO+ → SO + Na+ | 2.30e-9 | 0.00 | 0.00 | 10 - 41000 |
5 | SO+ + CH2CCH2 → C3H4+ + SO | 6.84e-10 | 0.00 | 0.00 | 10 - 41000 |
6 | SO+ + CH3CHCH2 → C3H6+ + SO | 1.82e-10 | 0.00 | 0.00 | 10 - 41000 |
7 | SO+ + CH3COCH3 → CH3COCH3+ + SO | 1.26e-9 | 0.00 | 0.00 | 10 - 41000 |
8 | SO+ + CH3OCH3 → CH3OCH3+ + SO | 1.80e-10 | -0.50 | 0.00 | 10 - 41000 |
9 | SO+ + Fe → Fe+ + SO | 1.60e-9 | 0.00 | 0.00 | 10 - 41000 |
10 | SO2 + CRPHOT → SO + O | 1.30e-17 | 0.00 | 922.00 | 10 - 41000 |
11 | HSO+ + e- → SO + H | 2.00e-7 | -0.50 | 0.00 | 10 - 300 |
12 | HSO2+ + e- → SO + O + H | 1.00e-7 | -0.50 | 0.00 | 10 - 300 |
13 | HSO2+ + e- → SO + OH | 1.00e-7 | -0.50 | 0.00 | 10 - 300 |
14 | OCS+ + e- → C + SO | 1.05e-8 | -0.62 | 0.00 | 10 - 300 |
15 | SO2+ + e- → SO + O | 2.81e-7 | -0.52 | 0.00 | 10 - 300 |
16 | O2 + SiS+ → SiO+ + SO | 2.67e-11 | 0.00 | 0.00 | 10 - 41000 |
17 | S + SiO+ → SO + Si+ | 1.00e-9 | 0.00 | 0.00 | 10 - 41000 |
18 | C- + SO+ → C + SO | 7.51e-8 | -0.50 | 0.00 | 10 - 41000 |
19 | C10- + SO+ → C10 + SO | 7.51e-8 | -0.50 | 0.00 | 10 - 41000 |
20 | C10H- + SO+ → C10H + SO | 7.51e-8 | -0.50 | 0.00 | 10 - 41000 |
21 | C2- + SO+ → C2 + SO | 7.51e-8 | -0.50 | 0.00 | 10 - 41000 |
22 | C2H- + SO+ → C2H + SO | 7.51e-8 | -0.50 | 0.00 | 10 - 41000 |
23 | C3- + SO+ → C3 + SO | 7.51e-8 | -0.50 | 0.00 | 10 - 41000 |
24 | C3H- + SO+ → C3H + SO | 7.51e-8 | -0.50 | 0.00 | 10 - 41000 |
25 | C3N- + SO+ → C3N + SO | 7.51e-8 | -0.50 | 0.00 | 10 - 41000 |
26 | C4- + SO+ → C4 + SO | 7.51e-8 | -0.50 | 0.00 | 10 - 41000 |
27 | C4H- + SO+ → C4H + SO | 7.51e-8 | -0.50 | 0.00 | 10 - 41000 |
28 | C5- + SO+ → C5 + SO | 7.51e-8 | -0.50 | 0.00 | 10 - 41000 |
29 | C5H- + SO+ → C5H + SO | 7.51e-8 | -0.50 | 0.00 | 10 - 41000 |
30 | C5N- + SO+ → C5N + SO | 7.51e-8 | -0.50 | 0.00 | 10 - 41000 |
31 | C6- + SO+ → C6 + SO | 7.51e-8 | -0.50 | 0.00 | 10 - 41000 |
32 | C6H- + SO+ → C6H + SO | 7.51e-8 | -0.50 | 0.00 | 10 - 41000 |
33 | C7- + SO+ → C7 + SO | 7.51e-8 | -0.50 | 0.00 | 10 - 41000 |
34 | C7H- + SO+ → C7H + SO | 7.51e-8 | -0.50 | 0.00 | 10 - 41000 |
35 | C8- + SO+ → C8 + SO | 7.51e-8 | -0.50 | 0.00 | 10 - 41000 |
36 | C8H- + SO+ → C8H + SO | 7.51e-8 | -0.50 | 0.00 | 10 - 41000 |
37 | C9- + SO+ → C9 + SO | 7.51e-8 | -0.50 | 0.00 | 10 - 41000 |
38 | C9H- + SO+ → C9H + SO | 7.51e-8 | -0.50 | 0.00 | 10 - 41000 |
39 | CH- + SO+ → CH + SO | 7.51e-8 | -0.50 | 0.00 | 10 - 41000 |
40 | CN- + SO+ → CN + SO | 7.51e-8 | -0.50 | 0.00 | 10 - 41000 |
41 | H- + SO+ → H + SO | 7.51e-8 | -0.50 | 0.00 | 10 - 41000 |
42 | O- + SO+ → O + SO | 7.51e-8 | -0.50 | 0.00 | 10 - 41000 |
43 | O2- + SO+ → O2 + SO | 7.51e-8 | -0.50 | 0.00 | 10 - 41000 |
44 | OH- + SO+ → OH + SO | 7.51e-8 | -0.50 | 0.00 | 10 - 41000 |
45 | S- + SO+ → S + SO | 7.51e-8 | -0.50 | 0.00 | 10 - 41000 |
46 | C + SO2 → CO + SO | 7.00e-11 | 0.00 | 0.00 | 10 - 300 |
47 | NO + S → SO + N | 1.75e-10 | 0.00 | 20200.00 | 2420 - 3870 |
48 | O2 + S → SO + O | 1.76e-12 | 0.81 | -30.80 | 200 - 3460 |
49 | O + CS → SO + C | 4.68e-11 | 0.50 | 28940.00 | 964 - 41000 |
50 | O + HS → SO + H | 1.74e-10 | -0.20 | 5.70 | 298 - 2000 |
51 | O + NS → SO + N | 1.00e-11 | 0.00 | 0.00 | 133 - 300 |
52 | O + OCS → SO + CO | 1.60e-11 | 0.00 | 2150.00 | 200 - 2500 |
53 | O + S2 → SO + S | 1.70e-11 | 0.00 | 0.00 | 298 - 2500 |
54 | O + SO2 → SO + O2 | 9.01e-12 | 0.00 | 9837.00 | 440 - 3760 |
55 | OH + S → SO + H | 6.60e-11 | 0.00 | 0.00 | 298 - 298 |
56 | S + SO2 → SO + SO | 9.76e-12 | 0.00 | 4545.00 | 1250 - 1600 |
57 | S + SO2 → SO + SO | 9.76e-12 | 0.00 | 4545.00 | 1250 - 1600 |
58 | SO2 + PHOTON → SO + O | 1.90e-9 | 0.00 | 2.40 | 10 - 41000 |
Variation of log fractional abundance (relative to H2) with log time (years) in a dark cloud model. Ref. RATE12 paper.