Abstract
Photolysis of nitrous acid generates hydroxyl radicals—a key atmospheric oxidant—in the lower atmosphere. Significant concentrations of nitrous acid have been reported in the rural atmospheric boundary layer during the day, where photolysis of nitrous acid accounts for up to 42% of sunlight-induced radical production1,2,3,4,5,6,7. The observed concentrations of nitrous acid are thought to be sustained by heterogeneous reactions involving precursors such as nitrogen oxides1,2,3,8,9,10,11,12 and nitric acid5,6,8,13. Here, we present direct measurements of nitrous acid flux over a rural forest canopy in Michigan, together with surface nitrate loading at the top of the canopy. We report a significant upward flux of nitrous acid during the day, with a peak around noontime. Daytime nitrous acid flux was positively correlated with the product of leaf surface nitrate loading and the rate constant of nitrate photolysis. We suggest that the photolysis of nitric acid on forest canopies is a significant daytime source of nitrous acid to the lower atmosphere in rural environments, and could serve as an important pathway for the remobilization of deposited nitric acid.
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Acknowledgements
We thank fellow PROPHETeers for their assistance and University of Michigan Biological Station for outstanding logistical support during the field deployments. This research was supported by National Science Foundation ATM-0632548.
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X.Z. conceived and initiated the study. X.Z, N.Z. and S.B designed the HONO measurement. N.Z., D.T. and J.H. measured HONO flux and concentration. M.T. measured surface nitrate loading. S.B. and M.A.C. measured Eppley ultraviolet. M.A. and P.B.S. measured NOx. S.G., S.D. and P.S.S. measured OH. X.Z., S.B. and M.A.C. coordinated the study. X.Z. wrote the paper. All the authors discussed the results and commented on the manuscript.
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Zhou, X., Zhang, N., TerAvest, M. et al. Nitric acid photolysis on forest canopy surface as a source for tropospheric nitrous acid. Nature Geosci 4, 440–443 (2011). https://doi.org/10.1038/ngeo1164
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DOI: https://doi.org/10.1038/ngeo1164
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