Howes, NUM orcid.org/0000-0002-4335-8593, Mir, ZS, Blitz, MA orcid.org/0000-0001-6710-4021 et al. (4 more authors) (2018) Kinetic studies of C₁ and C₂ Criegee intermediates with SO₂ using laser flash photolysis coupled with photoionization mass spectrometry and time resolved UV absorption spectroscopy. Physical Chemistry Chemical Physics, 20 (34). pp. 22218-22227. ISSN 1463-9076
Abstract
Recent, direct studies have shown that several reactions of stabilized Criegee intermediates (SCI) are significantly faster than indicated by earlier indirect measurements. The reaction of SCI with SO₂ may contribute to atmospheric sulfate production, but there are uncertainties in the mechanism of the reaction of the C1 Criegee intermediate, CH₂OO, with SO₂. The reactions of C1, CH₂OO, and C₂, CH₃CHOO, Criegee intermediates with SO₂ have been studied by generating stabilized Criegee intermediates by laser flash photolysis (LFP) of RI₂/O₂ (R = CH₂ or CH₃CH) mixtures with the reactions being followed by photoionization mass spectrometry (PIMS). PIMS has been used to determine the rate coefficient for the reaction of CH₃CHI with O₂, k = (8.6 ± 2.2) × 10⁻¹² cm³ molecule⁻¹ s⁻¹ at 295 K and 2 Torr (He). The yield of the C₂ Criegee intermediate under these conditions is 0.86 ± 0.11. All errors in the abstract are a combination of statistical at the 1σ level and an estimated systematic contribution. For the CH₂OO + SO₂ reaction, additional LFP experiments were performed monitoring CH₂OO by time-resolved broadband UV absorption spectroscopy (TRUVAS). The following rate coefficients have been determined at room temperature ((295 ± 2) K):CH₂OO + SO₂: k = (3.74 ± 0.43) × 10⁻¹¹ cm³ molecule⁻¹ s⁻¹ (LFP/PIMS),k = (3.87 ± 0.45) × 10⁻¹¹ cm³ molecule⁻¹ s⁻¹ (LFP/TRUVAS)CH₃CHOO + SO₂: k = (1.7 ± 0.3) × 10⁻¹¹ cm³ molecule⁻¹ s⁻¹ (LFP/PIMS)LFP/PIMS also allows for the direction observation of CH₃CHO production from the reaction of CH₃CHOO with SO₂, suggesting that SO₃ is the co-product. For the reaction of CH₂OO with SO₂ there is no evidence of any variation in reaction mechanism with [SO₂] as had been suggested in an earlier publication (Chhantyal-Pun et al., Phys. Chem. Chem. Phys., 2015, 17, 3617). A mean value of k = (3.76 ± 0.14) × 10⁻¹¹ cm³ molecule⁻¹ s⁻¹ for the CH₂OO + SO₂ reaction is recommended from this and previous studies. The atmospheric implications of the results are briefly discussed.
Metadata
Item Type: | Article |
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Authors/Creators: |
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Copyright, Publisher and Additional Information: | © 2018, the Owner Societies. This is an author produced version of a paper published in Physical Chemistry Chemical Physics. Uploaded in accordance with the publisher's self-archiving policy. |
Dates: |
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Institution: | The University of Leeds |
Academic Units: | The University of Leeds > Faculty of Engineering & Physical Sciences (Leeds) > School of Chemistry (Leeds) > Physical Chemistry (Leeds) |
Funding Information: | Funder Grant number NERC NE/L010798/1 |
Depositing User: | Symplectic Publications |
Date Deposited: | 22 Aug 2018 13:53 |
Last Modified: | 06 Aug 2019 00:39 |
Status: | Published |
Publisher: | Royal Society of Chemistry |
Identification Number: | 10.1039/c8cp03115k |
Open Archives Initiative ID (OAI ID): | oai:eprints.whiterose.ac.uk:134840 |