Thermally Initiated Formation of Criegee Intermediate CH<sub>2</sub>OO in the Oxidation of Ethane

Criegee intermediates (CIs) play an important role in atmospheric chemistry as a transient source of the OH radical through their formation by the ozonolysis of unsaturated organic compounds. Here, we report thermally initiated formation of the smallest CI (CH<sub>2</sub>OO) in the oxidation of ethane (CH<sub>3</sub>CH<sub>3</sub>) that may be relevant to combustion and flames. The SiO<sub>2</sub>/SiC oxidation microreactor is heated to 1800 K and has a short residence time of ∼100 μs. The CH<sub>2</sub>OO we observe is likely formed in a lower-temperature region near the microreactor's exit. Plausible mechanisms for CH<sub>2</sub>OO formation and retention under these conditions mediated by methylperoxy (CH<sub>3</sub>OO) radicals are discussed. Pure rotational spectra of CH<sub>2</sub>OO and other intermediates (HO<sub>2</sub>, CH<sub>3</sub>CHO, CH<sub>2</sub>CHOH, <i>c-</i>CH<sub>2</sub>OCH<sub>2</sub>, CH<sub>3</sub>CH<sub>2</sub>CHO, CH<sub>3</sub>OOH, and HCOOH) are detected with a chirped-pulse Fourier transform millimeter-wave spectrometer operating in the frequency range of 60-90 GHz. Detection occurs in a molecular beam, where the species are supersonically cooled to 5 K.

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Journal
The Journal of Physical Chemistry Letters
Published
2024-12-12
DOI
https://doi.org/10.1021/acs.jpclett.4c02445
Primary Topic
Atmospheric Ozone and Climate
Type
article
Field-Weighted Citation Impact
0.00

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article

Thermally Initiated Formation of Criegee Intermediate CH2OO in the Oxidation of Ethane

Kirill Prozument, Raghu Sivaramakrishnan, Rizalina Tama Saragi, Nathan A. Seifert
The Journal of Physical Chemistry Letters
Atmospheric Ozone and Climate
article

Thermally Initiated Formation of Criegee Intermediate CH2OO in the Oxidation of Ethane

Kirill Prozument, Raghu Sivaramakrishnan, Rizalina Tama Saragi, Nathan A. Seifert
article en

Abstract

Criegee intermediates (CIs) play an important role in atmospheric chemistry as a transient source of the OH radical through their formation by the ozonolysis of unsaturated organic compounds. Here, we report thermally initiated formation of the smallest CI (CH<sub>2</sub>OO) in the oxidation of ethane (CH<sub>3</sub>CH<sub>3</sub>) that may be relevant to combustion and flames. The SiO<sub>2</sub>/SiC oxidation microreactor is heated to 1800 K and has a short residence time of ∼100 μs. The CH<sub>2</sub>OO we observe is likely formed in a lower-temperature region near the microreactor's exit. Plausible mechanisms for CH<sub>2</sub>OO formation and retention under these conditions mediated by methylperoxy (CH<sub>3</sub>OO) radicals are discussed. Pure rotational spectra of CH<sub>2</sub>OO and other intermediates (HO<sub>2</sub>, CH<sub>3</sub>CHO, CH<sub>2</sub>CHOH, <i>c-</i>CH<sub>2</sub>OCH<sub>2</sub>, CH<sub>3</sub>CH<sub>2</sub>CHO, CH<sub>3</sub>OOH, and HCOOH) are detected with a chirped-pulse Fourier transform millimeter-wave spectrometer operating in the frequency range of 60-90 GHz. Detection occurs in a molecular beam, where the species are supersonically cooled to 5 K.

The Journal of Physical Chemistry LettersVol. 15(50)
Argonne National Laboratory (US), University of New Haven (US)
Basic Energy Sciences
Clean water and sanitation
Openalex Percentile: Top 74%
Atmospheric Ozone and Climate
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