TY - JOUR
T1 - Production of Formate via Oxidation of Glyoxal Promoted by Particulate Nitrate Photolysis
AU - Zhang, Ruifeng
AU - Gen, Masao
AU - Fu, Tzung May
AU - Chan, Chak K.
N1 - Funding Information:
We gratefully acknowledge support from the National Natural Science Foundation of China (42075100 and 41875142) and the Guangdong Basic and Applied Basic Research Foundation (2020B1515130003). This work was also supported in part by the Japan Society for the Promotion of Science KAKENHI Grant-in-Aid for Research Activity Start-up (20K23363), the Kurita Water and Environment Foundation (20A030), the Steel Foundation for Environmental Protection Technology, and The Sumitomo Foundation (203113).
Publisher Copyright:
© 2021 American Chemical Society. All rights reserved.
PY - 2021/5/4
Y1 - 2021/5/4
N2 - Particulate nitrate photolysis can produce oxidants (i.e., OH, NO2, and NO2-/HNO2) in aqueous droplets and may play a potential role in increased atmospheric oxidative capacity. Our earlier works have reported on the SO2 oxidation promoted by nitrate photolysis to produce sulfate. Here, we used glyoxal as a model precursor to examine the role of particulate nitrate photolysis in the formation of secondary organic aerosol (SOA) from particle-phase oxidation of glyoxal by OH radicals. Particles containing sodium nitrate and glyoxal were irradiated at 300 nm. Interestingly, typical oxidation products of oxalic acid, glyoxylic acid, and higher-molecular-weight products reported in the literature were not found in the photooxidation process of glyoxal during nitrate photolysis in the particle phase. Instead, formic acid/formate production was found as the main oxidation product. At glyoxal concentration higher than 3 M, we found that the formic acid/formate production rate increases significantly with increasing glyoxal concentration. Such results suggest that oxidation of glyoxal at high concentrations by OH radicals produced from nitrate photolysis in aqueous particles may not contribute significantly to SOA formation since formic acid is a volatile species. Furthermore, recent predictions of formic acid/formate concentration from the most advanced chemical models are lower than ambient observations at both the ground level and high altitude. The present study reveals a new insight into the production of formic acid/formate as well as a sink of glyoxal in the atmosphere, which may partially narrow the gap between model predictions and field measurements in both species.
AB - Particulate nitrate photolysis can produce oxidants (i.e., OH, NO2, and NO2-/HNO2) in aqueous droplets and may play a potential role in increased atmospheric oxidative capacity. Our earlier works have reported on the SO2 oxidation promoted by nitrate photolysis to produce sulfate. Here, we used glyoxal as a model precursor to examine the role of particulate nitrate photolysis in the formation of secondary organic aerosol (SOA) from particle-phase oxidation of glyoxal by OH radicals. Particles containing sodium nitrate and glyoxal were irradiated at 300 nm. Interestingly, typical oxidation products of oxalic acid, glyoxylic acid, and higher-molecular-weight products reported in the literature were not found in the photooxidation process of glyoxal during nitrate photolysis in the particle phase. Instead, formic acid/formate production was found as the main oxidation product. At glyoxal concentration higher than 3 M, we found that the formic acid/formate production rate increases significantly with increasing glyoxal concentration. Such results suggest that oxidation of glyoxal at high concentrations by OH radicals produced from nitrate photolysis in aqueous particles may not contribute significantly to SOA formation since formic acid is a volatile species. Furthermore, recent predictions of formic acid/formate concentration from the most advanced chemical models are lower than ambient observations at both the ground level and high altitude. The present study reveals a new insight into the production of formic acid/formate as well as a sink of glyoxal in the atmosphere, which may partially narrow the gap between model predictions and field measurements in both species.
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U2 - 10.1021/acs.est.0c08199
DO - 10.1021/acs.est.0c08199
M3 - Article
C2 - 33861585
AN - SCOPUS:85105106632
SN - 0013-936X
VL - 55
SP - 5711
EP - 5720
JO - Environmental Science & Technology
JF - Environmental Science & Technology
IS - 9
ER -