HS+
Sulphur hydride ion
Flags: Detected, RATE12
Empirical: HS+
Mass: 33 amu
Heat of formation: 1137.0 kJ mol-1
Added to system: 2003-05-06 06:43:21
Reactions: Formation | Destruction
27 HS+ formation reactions
Reaction | α | β | γ | Tl - Tu (K) | |
---|---|---|---|---|---|
1 | H+ + HS → HS+ + H | 1.60e-9 | 0.00 | 0.00 | 10 - 41000 |
2 | CH+ + S → HS+ + C | 4.70e-10 | 0.00 | 0.00 | 10 - 41000 |
3 | CH5+ + S → HS+ + CH4 | 1.30e-9 | 0.00 | 0.00 | 10 - 41000 |
4 | H+ + H2S → HS+ + H2 | 9.90e-10 | -0.50 | 0.00 | 10 - 41000 |
5 | H+ + OCS → HS+ + CO | 2.10e-9 | 0.00 | 0.00 | 10 - 41000 |
6 | H2+ + H2S → HS+ + H2 + H | 8.60e-10 | -0.50 | 0.00 | 10 - 41000 |
7 | H2 + S+ → HS+ + H | 1.10e-10 | 0.00 | 9860.00 | 328 - 41000 |
8 | H2CO+ + S → HS+ + HCO | 5.50e-10 | 0.00 | 0.00 | 10 - 41000 |
9 | H2O+ + S → HS+ + OH | 4.30e-10 | 0.00 | 0.00 | 10 - 41000 |
10 | H3+ + S → HS+ + H2 | 2.60e-9 | 0.00 | 0.00 | 10 - 41000 |
11 | H + H2S+ → HS+ + H2 | 2.00e-10 | 0.00 | 0.00 | 10 - 41000 |
12 | HCN+ + S → HS+ + CN | 5.70e-10 | 0.00 | 0.00 | 10 - 41000 |
13 | HCO+ + S → HS+ + CO | 3.30e-10 | 0.00 | 0.00 | 10 - 41000 |
14 | HCO + S+ → HS+ + CO | 3.60e-10 | -0.50 | 0.00 | 10 - 41000 |
15 | HNO+ + S → HS+ + NO | 1.10e-9 | 0.00 | 0.00 | 10 - 41000 |
16 | He+ + H2S2 → HS+ + HS + He | 2.00e-9 | -0.50 | 0.00 | 10 - 41000 |
17 | He+ + H2S → HS+ + He + H | 4.84e-10 | -0.50 | 0.00 | 10 - 41000 |
18 | N+ + H2S → HS+ + NH | 5.51e-10 | -0.50 | 0.00 | 10 - 41000 |
19 | N2+ + H2S → HS+ + N2 + H | 1.13e-9 | -0.50 | 0.00 | 10 - 41000 |
20 | HN2+ + S → HS+ + N2 | 1.10e-9 | 0.00 | 0.00 | 10 - 41000 |
21 | NH+ + S → HS+ + N | 6.90e-10 | 0.00 | 0.00 | 10 - 41000 |
22 | NH2+ + H2S → HS+ + NH3 | 1.80e-10 | -0.50 | 0.00 | 10 - 41000 |
23 | NH2+ + S → HS+ + NH | 4.40e-10 | 0.00 | 0.00 | 10 - 41000 |
24 | O+ + H2S → HS+ + OH | 4.20e-10 | -0.50 | 0.00 | 10 - 41000 |
25 | O + H2S+ → HS+ + OH | 3.10e-10 | 0.00 | 0.00 | 10 - 41000 |
26 | OH+ + S → HS+ + O | 4.30e-10 | 0.00 | 0.00 | 10 - 41000 |
27 | S + O2H+ → HS+ + O2 | 1.10e-9 | 0.00 | 0.00 | 10 - 41000 |
Variation of log fractional abundance (relative to H2) with log time (years) in a dark cloud model. Ref. RATE12 paper.