Photolysis of pyruvic acid in ice: Possible relevance to CO and CO_2 ice core record anomalies

The abnormal spikes detected in some CO and CO_2 polar ice core records indicate persistent chemical activity in glacial ice. Since CO and CO_2 spikes are correlated, and their amplitudes scale with reported CO/CO_2 yields for the photolysis of dissolved natural organic matter, a common photochemica...

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Published in:Journal of Geophysical Research: Atmospheres
Main Authors: Guzmán, M. I., Hoffmann, M. R., Colussi, A. J.
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union 2007
Subjects:
Online Access:https://authors.library.caltech.edu/58466/
https://authors.library.caltech.edu/58466/1/jgrd13447.pdf
https://resolver.caltech.edu/CaltechAUTHORS:20150623-154752526
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spelling ftcaltechauth:oai:authors.library.caltech.edu:58466 2023-05-15T16:38:51+02:00 Photolysis of pyruvic acid in ice: Possible relevance to CO and CO_2 ice core record anomalies Guzmán, M. I. Hoffmann, M. R. Colussi, A. J. 2007-05-26 application/pdf https://authors.library.caltech.edu/58466/ https://authors.library.caltech.edu/58466/1/jgrd13447.pdf https://resolver.caltech.edu/CaltechAUTHORS:20150623-154752526 en eng American Geophysical Union https://authors.library.caltech.edu/58466/1/jgrd13447.pdf Guzmán, M. I. and Hoffmann, M. R. and Colussi, A. J. (2007) Photolysis of pyruvic acid in ice: Possible relevance to CO and CO_2 ice core record anomalies. Journal of Geophysical Research D, 112 (D10). Art. No. D10123. ISSN 0148-0227. doi:10.1029/2006JD007886. https://resolver.caltech.edu/CaltechAUTHORS:20150623-154752526 <https://resolver.caltech.edu/CaltechAUTHORS:20150623-154752526> other Article PeerReviewed 2007 ftcaltechauth https://doi.org/10.1029/2006JD007886 2021-11-11T19:04:52Z The abnormal spikes detected in some CO and CO_2 polar ice core records indicate persistent chemical activity in glacial ice. Since CO and CO_2 spikes are correlated, and their amplitudes scale with reported CO/CO_2 yields for the photolysis of dissolved natural organic matter, a common photochemical source is implicated. Given that sufficient actinic radiation is constantly generated throughout ice by cosmic muons (Colussi and Hoffmann, 2003), it remains to be shown that the photolyses of typical organic contaminants proceed by similar mechanisms in water and ice. Here we report that the photodecarboxylation of pyruvic acid (PA, an ubiquitous ice contaminant) indeed leads to the same products nearly as efficiently in both media. CO_2 is promptly released from frozen PA/H_2O films upon illumination and continues to evolve after photolysis. By analogy with our studies in water (Guzmán et al., 2006b), we infer that ^3PA* reacts with PA in ice producing CH_3C(O)C(O)O· and (CH_3C•(OH)C(O)OH) radicals. The barrierless decarboxylation, CH3C(O)C(O)O· → CH_3C(O)· + CO_2, accounts for prompt CO_2 emissions down to ∼140 K. Bimolecular radical reactions subsequently ensue in fluid molecular environments, both in water and ice, leading to metastable intermediates that decarboxylate immediately in water, but protractedly in ice. The overall quantum yield of CO_2 production in the λ ~313 nm photolysis of PA in ice at 250 K is ∼60% of that in water at 293 K. The in situ photolysis of natural organic matter is, therefore, a plausible explanation of CO and CO_2 ice core record anomalies. Article in Journal/Newspaper ice core Caltech Authors (California Institute of Technology) Guzmán ENVELOPE(-62.850,-62.850,-64.817,-64.817) Journal of Geophysical Research: Atmospheres 112 D10
institution Open Polar
collection Caltech Authors (California Institute of Technology)
op_collection_id ftcaltechauth
language English
description The abnormal spikes detected in some CO and CO_2 polar ice core records indicate persistent chemical activity in glacial ice. Since CO and CO_2 spikes are correlated, and their amplitudes scale with reported CO/CO_2 yields for the photolysis of dissolved natural organic matter, a common photochemical source is implicated. Given that sufficient actinic radiation is constantly generated throughout ice by cosmic muons (Colussi and Hoffmann, 2003), it remains to be shown that the photolyses of typical organic contaminants proceed by similar mechanisms in water and ice. Here we report that the photodecarboxylation of pyruvic acid (PA, an ubiquitous ice contaminant) indeed leads to the same products nearly as efficiently in both media. CO_2 is promptly released from frozen PA/H_2O films upon illumination and continues to evolve after photolysis. By analogy with our studies in water (Guzmán et al., 2006b), we infer that ^3PA* reacts with PA in ice producing CH_3C(O)C(O)O· and (CH_3C•(OH)C(O)OH) radicals. The barrierless decarboxylation, CH3C(O)C(O)O· → CH_3C(O)· + CO_2, accounts for prompt CO_2 emissions down to ∼140 K. Bimolecular radical reactions subsequently ensue in fluid molecular environments, both in water and ice, leading to metastable intermediates that decarboxylate immediately in water, but protractedly in ice. The overall quantum yield of CO_2 production in the λ ~313 nm photolysis of PA in ice at 250 K is ∼60% of that in water at 293 K. The in situ photolysis of natural organic matter is, therefore, a plausible explanation of CO and CO_2 ice core record anomalies.
format Article in Journal/Newspaper
author Guzmán, M. I.
Hoffmann, M. R.
Colussi, A. J.
spellingShingle Guzmán, M. I.
Hoffmann, M. R.
Colussi, A. J.
Photolysis of pyruvic acid in ice: Possible relevance to CO and CO_2 ice core record anomalies
author_facet Guzmán, M. I.
Hoffmann, M. R.
Colussi, A. J.
author_sort Guzmán, M. I.
title Photolysis of pyruvic acid in ice: Possible relevance to CO and CO_2 ice core record anomalies
title_short Photolysis of pyruvic acid in ice: Possible relevance to CO and CO_2 ice core record anomalies
title_full Photolysis of pyruvic acid in ice: Possible relevance to CO and CO_2 ice core record anomalies
title_fullStr Photolysis of pyruvic acid in ice: Possible relevance to CO and CO_2 ice core record anomalies
title_full_unstemmed Photolysis of pyruvic acid in ice: Possible relevance to CO and CO_2 ice core record anomalies
title_sort photolysis of pyruvic acid in ice: possible relevance to co and co_2 ice core record anomalies
publisher American Geophysical Union
publishDate 2007
url https://authors.library.caltech.edu/58466/
https://authors.library.caltech.edu/58466/1/jgrd13447.pdf
https://resolver.caltech.edu/CaltechAUTHORS:20150623-154752526
long_lat ENVELOPE(-62.850,-62.850,-64.817,-64.817)
geographic Guzmán
geographic_facet Guzmán
genre ice core
genre_facet ice core
op_relation https://authors.library.caltech.edu/58466/1/jgrd13447.pdf
Guzmán, M. I. and Hoffmann, M. R. and Colussi, A. J. (2007) Photolysis of pyruvic acid in ice: Possible relevance to CO and CO_2 ice core record anomalies. Journal of Geophysical Research D, 112 (D10). Art. No. D10123. ISSN 0148-0227. doi:10.1029/2006JD007886. https://resolver.caltech.edu/CaltechAUTHORS:20150623-154752526 <https://resolver.caltech.edu/CaltechAUTHORS:20150623-154752526>
op_rights other
op_doi https://doi.org/10.1029/2006JD007886
container_title Journal of Geophysical Research: Atmospheres
container_volume 112
container_issue D10
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