Table C.1.
Summary of the reactions involving HONO.
Reaction | ΔE | α | β | γ | F0 | g | Reference | ||
---|---|---|---|---|---|---|---|---|---|
kJ mol−1 | |||||||||
1. | H+ + HONO | → HONO+ + H | −235 | 0 | Ionpol1, capture rate theory. We avoid introducing HONO+. | ||||
– | → H2O + NO+ | −693 | 1.0 | 2.0 × 10−9 | 5.27 | 3 | 0 | ||
2. | He+ + HONO | → HONO+ + He | 0 | Ionpol1, capture rate theory. We avoid introducing HONO+. | |||||
→ HO + NO+ + He | 1.0 | 1.0 × 10−9 | 5.27 | 3 | 0 | ||||
3. | C + HONO | → CO + NO + H | −459 | 3.0 × 10−10 | 0 | 0 | 2 | 0 | Capture rate theory, approximate branching ratio. |
4. | C+ + HONO | → CO + NO+ + H | −635 | 2.0 × 10−9 | −0.4 | 0 | 3 | 0 | Capture rate theory, approximate branching ratio. (HCO+ + NO is likely a non-negligible exit channel). |
→ HCO+ + NO | −817 | 0 | −0.4 | 0 | 3 | 0 | |||
5. | OH + HONO | → NO2 + H2O | −21 | 7.0 × 10−12 | −0.6 | 0 | 1.6 | 10 | This reaction has been studied between 278 and 373 K. The results from Jenkin & Cox (1987) show large uncertainty due to complicated secondary reactions. The results from Burkholder et al. (1992) show no barrier and a negative temperature dependency. We use an expression compatible with experimental data and leading to reasonable rate constant at 10 K. |
6. | HONO + H![]() |
→ H2ONO++ H2 | −358 | 1.0 | 2.38 × 10−9 | 5.27 | 2 | 0 | Ionpol1. The others isomers are also likely to be produced but we avoid introducing too many species without a notably different chemical behaviour. |
→ HONOH+ + H2 | −232 | 0 | |||||||
→ HONHO+ + H2 | −196 | 0 | |||||||
7. | HONO + HCO+ | → H2ONO+ + CO | −210 | 1.0 | 9.45 × 10−10 | 5.27 | 2 | 0 | Ionpol1. |
8. | H2ONO+ + e− | → HONO + H | −524 | 2.0 × 10−7 | −0.5 | 0 | 3 | 0 | Rate by comparison with similar DR (Fournier et al. 2013; Florescu-Mitchell & Mitchell 2006; Geppert et al. 2004) and branching ratios deduced roughly from similar reactions using Plessis et al. (2012). The important fact is that HONO is likely a non-negligible product. |
→ H2O + NO | −825 | 1.0 × 10−7 | −0.5 | 0 | 3 | 0 | |||
→ H + OH + NO | −339 | 2.0 × 10−7 | −0.5 | 0 | 3 | 0 | |||
→ H2O + N + O | −207 | 1.0 × 10−7 | −0.5 | 0 | 3 | 0 | |||
9. | s-H + s-NO2 | → s-HONO | −317 | 0.7 | 0 | Radical-radical reaction, well known in gas phase (Michael et al. 1979; Nguyen et al. 1998; Su et al. 2002). Both approach towards N and O atoms are attractive. | |||
→ HNO2 | −281 | 0.3 | 0 | ||||||
→ s-NO + s-OH | −132 | 0 | |||||||
10. | s-H + s-HONO | → s-H2NO2 | −163 | 1 | 2600 | We use the theoretical work from Hsu et al. (1997). H2NO2 = (HN(O)OH). Some NO + H2O are likely to be produced but this exit channel involves a transition state close to the H + HONO entrance level. | |||
→ s-H2 + s-NO2 | −109 | 0 | |||||||
→ s-NO + s-H2O | −301 | 0 | |||||||
→ s-HON + s-OH | +164 | 0 | |||||||
11. | s-H + s-H2NO2 | → s-H3NO2 | −302 | 1 | 0 | M06-2X/AVTZ calculations (this work). H3NO2 = HO–NH–OH. Some HNO may be produced. | |||
→ s-HON + s-H2O | −159 | 0 | |||||||
→ s-HNO + s-H2O | −327 | 0 | |||||||
12. | s-OH + s-NO | → s-HONO | −185 | 1 | 0 | The OH + NO reaction is a radical-radical barrierless reaction (Forster et al. 1995). |
Notes. Exothermicities of the reactions (ΔE in kJ mol−1) are calculated at M06-2X/AVTZ level using Gaussian 2009 software. Definitions of α, β, γ, F0, g, Ionpol1 and Ionpol2 can been found in Wakelam et al. (2010, 2012): k = α × (T/300)β × exp(−γ/T) cm3 mol−1 s−1, T range is 10–300 K except in some cases (noted). Ionpol1: k = αβ(0.62 + 0.4767γ (300/T)0.5) cm3 mol−1 s−1, Ionpol2: k = αβ(1 + 0.0967γ(300/T)0.5 + (γ2/10.526) (300/T)) cm3 mol−1 s−1, F0 = exp(Δk/k0) (≈1 + (Δk/k0) and F(T) = F0exp(g ∣ 1/T − 1/T0∣).
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