Isoprene photochemistry over the Amazon rainforest.

Autor: Liu Y; John A. Paulson School of Engineering and Applied Sciences, Harvard University, Cambridge, MA 02138;, Brito J; Department of Applied Physics, University of São Paulo, São Paulo 05508, Brazil;, Dorris MR; Department of Chemistry, University of Wisconsin-Madison, Madison, WI 53706;, Rivera-Rios JC; Department of Chemistry, University of Wisconsin-Madison, Madison, WI 53706; Department of Chemistry and Chemical Biology, Harvard University, Cambridge, MA 02138;, Seco R; Department of Earth System Science, University of California, Irvine, CA 92697;, Bates KH; Division of Chemistry and Chemical Engineering, California Institute of Technology, Pasadena, CA 91125;, Artaxo P; Department of Applied Physics, University of São Paulo, São Paulo 05508, Brazil;, Duvoisin S Jr; Department of Chemistry, Universidade do Estado do Amazonas, Manaus, AM 69050, Brazil;, Keutsch FN; John A. Paulson School of Engineering and Applied Sciences, Harvard University, Cambridge, MA 02138; Department of Chemistry, University of Wisconsin-Madison, Madison, WI 53706; Department of Chemistry and Chemical Biology, Harvard University, Cambridge, MA 02138;, Kim S; Department of Earth System Science, University of California, Irvine, CA 92697;, Goldstein AH; Department of Environmental Science, Policy, and Management, University of California, Berkeley, CA 94720;, Guenther AB; Department of Earth System Science, University of California, Irvine, CA 92697; Pacific Northwest National Laboratory, Richland, WA 99354;, Manzi AO; Instituto Nacional de Pesquisas da Amazonia, Manaus, AM 69067, Brazil;, Souza RA; Department of Meteorology, Universidade do Estado do Amazonas, Manaus, AM 69050, Brazil;, Springston SR; Department of Environmental and Climate Sciences, Brookhaven National Laboratory, Upton, NY 11973;, Watson TB; Department of Environmental and Climate Sciences, Brookhaven National Laboratory, Upton, NY 11973;, McKinney KA; John A. Paulson School of Engineering and Applied Sciences, Harvard University, Cambridge, MA 02138; kamckinney@seas.harvard.edu scot_martin@harvard.edu., Martin ST; John A. Paulson School of Engineering and Applied Sciences, Harvard University, Cambridge, MA 02138; Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138 kamckinney@seas.harvard.edu scot_martin@harvard.edu.
Jazyk: angličtina
Zdroj: Proceedings of the National Academy of Sciences of the United States of America [Proc Natl Acad Sci U S A] 2016 May 31; Vol. 113 (22), pp. 6125-30. Date of Electronic Publication: 2016 May 16.
DOI: 10.1073/pnas.1524136113
Abstrakt: Isoprene photooxidation is a major driver of atmospheric chemistry over forested regions. Isoprene reacts with hydroxyl radicals (OH) and molecular oxygen to produce isoprene peroxy radicals (ISOPOO). These radicals can react with hydroperoxyl radicals (HO2) to dominantly produce hydroxyhydroperoxides (ISOPOOH). They can also react with nitric oxide (NO) to largely produce methyl vinyl ketone (MVK) and methacrolein (MACR). Unimolecular isomerization and bimolecular reactions with organic peroxy radicals are also possible. There is uncertainty about the relative importance of each of these pathways in the atmosphere and possible changes because of anthropogenic pollution. Herein, measurements of ISOPOOH and MVK + MACR concentrations are reported over the central region of the Amazon basin during the wet season. The research site, downwind of an urban region, intercepted both background and polluted air masses during the GoAmazon2014/5 Experiment. Under background conditions, the confidence interval for the ratio of the ISOPOOH concentration to that of MVK + MACR spanned 0.4-0.6. This result implies a ratio of the reaction rate of ISOPOO with HO2 to that with NO of approximately unity. A value of unity is significantly smaller than simulated at present by global chemical transport models for this important, nominally low-NO, forested region of Earth. Under polluted conditions, when the concentrations of reactive nitrogen compounds were high (>1 ppb), ISOPOOH concentrations dropped below the instrumental detection limit (<60 ppt). This abrupt shift in isoprene photooxidation, sparked by human activities, speaks to ongoing and possible future changes in the photochemistry active over the Amazon rainforest.
Databáze: MEDLINE