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A theoretical study of the mechanism of the atmospherically relevant reaction of chlorine atoms with methyl nitrate, and calculation of the reaction rate coefficients at temperatures relevant to the atmosphere

A theoretical study of the mechanism of the atmospherically relevant reaction of chlorine atoms with methyl nitrate, and calculation of the reaction rate coefficients at temperatures relevant to the atmosphere
A theoretical study of the mechanism of the atmospherically relevant reaction of chlorine atoms with methyl nitrate, and calculation of the reaction rate coefficients at temperatures relevant to the atmosphere
The reaction between atomic chlorine (Cl) and methyl nitrate (CH3ONO2) is significant in the atmosphere, as Cl is a key oxidant, especially in the marine boundary layer, and alkyl nitrates are important nitrogen-containing organic compounds, which are temporary reservoirs of the reactive nitrogen oxides NO, NO2 and NO3 (NOx). Four reaction channels HCl + CH2ONO2, CH3OCl + NO2, CH3Cl + NO3 and CH3O + ClNO2 were considered. The major channel is found to be the H abstraction channel, to give the products HCl + CH2ONO2. For all channels, geometry optimization and frequency calculations were carried out at the M06-2X/6-31+G** level, while relative electronic energies were improved to the UCCSD(T*)-F12/CBS level. The reaction barrier (Image ID:c4cp06007e-t1.gif) and reaction enthalpy (?HRX298K) of the H abstraction channel were computed to be 0.61 and ?2.30 kcal mol?1, respectively, at the UCCSD(T*)-F12/CBS//M06-2X/6-31+G** level. Reaction barriers (Image ID:c4cp06007e-t2.gif) for the other channels are more positive and these pathways do not contribute to the overall reaction rate coefficient in the temperature range considered (200–400 K). Rate coefficients were calculated for the H-abstraction channel at various levels of variational transition state theory (VTST) including tunnelling. Recommended ICVT/SCT rate coefficients in the temperature range 200–400 K are presented for the first time for this reaction. The values obtained in the 200–300 K region are particularly important as they will be valuable for atmospheric modelling calculations involving reactions with methyl nitrate. The implications of the results to atmospheric chemistry are discussed. Also, the enthalpies of formation, ?Hf,298K, of CH3ONO2 and CH2ONO2 were computed to be ?29.7 and 19.3 kcal mol?1, respectively, at the UCCSD(T*)-F12/CBS level.
1463-9076
7463-7476
Ng, Maggie
bc203fa1-3eb7-4b63-b1e9-78faca2e5c30
Mok, Daniel
89c78a4b-6c37-4f0c-8026-57246a407d35
Lee, Edmond
418ef3de-1a0c-40f4-819d-680c7568c6b9
Dyke, John
46393b45-6694-46f3-af20-d7369d26199f
Ng, Maggie
bc203fa1-3eb7-4b63-b1e9-78faca2e5c30
Mok, Daniel
89c78a4b-6c37-4f0c-8026-57246a407d35
Lee, Edmond
418ef3de-1a0c-40f4-819d-680c7568c6b9
Dyke, John
46393b45-6694-46f3-af20-d7369d26199f

Ng, Maggie, Mok, Daniel, Lee, Edmond and Dyke, John (2015) A theoretical study of the mechanism of the atmospherically relevant reaction of chlorine atoms with methyl nitrate, and calculation of the reaction rate coefficients at temperatures relevant to the atmosphere. Physical Chemistry Chemical Physics, 17 (11), 7463-7476. (doi:10.1039/c4cp06007e).

Record type: Article

Abstract

The reaction between atomic chlorine (Cl) and methyl nitrate (CH3ONO2) is significant in the atmosphere, as Cl is a key oxidant, especially in the marine boundary layer, and alkyl nitrates are important nitrogen-containing organic compounds, which are temporary reservoirs of the reactive nitrogen oxides NO, NO2 and NO3 (NOx). Four reaction channels HCl + CH2ONO2, CH3OCl + NO2, CH3Cl + NO3 and CH3O + ClNO2 were considered. The major channel is found to be the H abstraction channel, to give the products HCl + CH2ONO2. For all channels, geometry optimization and frequency calculations were carried out at the M06-2X/6-31+G** level, while relative electronic energies were improved to the UCCSD(T*)-F12/CBS level. The reaction barrier (Image ID:c4cp06007e-t1.gif) and reaction enthalpy (?HRX298K) of the H abstraction channel were computed to be 0.61 and ?2.30 kcal mol?1, respectively, at the UCCSD(T*)-F12/CBS//M06-2X/6-31+G** level. Reaction barriers (Image ID:c4cp06007e-t2.gif) for the other channels are more positive and these pathways do not contribute to the overall reaction rate coefficient in the temperature range considered (200–400 K). Rate coefficients were calculated for the H-abstraction channel at various levels of variational transition state theory (VTST) including tunnelling. Recommended ICVT/SCT rate coefficients in the temperature range 200–400 K are presented for the first time for this reaction. The values obtained in the 200–300 K region are particularly important as they will be valuable for atmospheric modelling calculations involving reactions with methyl nitrate. The implications of the results to atmospheric chemistry are discussed. Also, the enthalpies of formation, ?Hf,298K, of CH3ONO2 and CH2ONO2 were computed to be ?29.7 and 19.3 kcal mol?1, respectively, at the UCCSD(T*)-F12/CBS level.

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Accepted/In Press date: 11 February 2015
e-pub ahead of print date: 12 February 2015
Published date: 21 March 2015
Organisations: Computational Systems Chemistry

Identifiers

Local EPrints ID: 383093
URI: http://eprints.soton.ac.uk/id/eprint/383093
ISSN: 1463-9076
PURE UUID: 4d6df1f4-816e-4188-92c6-95768660a946
ORCID for John Dyke: ORCID iD orcid.org/0000-0002-9808-303X

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Date deposited: 27 Oct 2015 14:14
Last modified: 15 Mar 2024 02:35

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Contributors

Author: Maggie Ng
Author: Daniel Mok
Author: Edmond Lee
Author: John Dyke ORCID iD

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