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Multicomponent new particle formation from sulfuric acid, ammonia, and biogenic vapors.


ABSTRACT: A major fraction of atmospheric aerosol particles, which affect both air quality and climate, form from gaseous precursors in the atmosphere. Highly oxygenated organic molecules (HOMs), formed by oxidation of biogenic volatile organic compounds, are known to participate in particle formation and growth. However, it is not well understood how they interact with atmospheric pollutants, such as nitrogen oxides (NO x ) and sulfur oxides (SO x ) from fossil fuel combustion, as well as ammonia (NH3) from livestock and fertilizers. Here, we show how NO x suppresses particle formation, while HOMs, sulfuric acid, and NH3 have a synergistic enhancing effect on particle formation. We postulate a novel mechanism, involving HOMs, sulfuric acid, and ammonia, which is able to closely reproduce observations of particle formation and growth in daytime boreal forest and similar environments. The findings elucidate the complex interactions between biogenic and anthropogenic vapors in the atmospheric aerosol system.

SUBMITTER: Lehtipalo K 

PROVIDER: S-EPMC6291317 | biostudies-literature | 2018 Dec

REPOSITORIES: biostudies-literature

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Multicomponent new particle formation from sulfuric acid, ammonia, and biogenic vapors.

Lehtipalo Katrianne K   Yan Chao C   Dada Lubna L   Bianchi Federico F   Bianchi Federico F   Xiao Mao M   Wagner Robert R   Stolzenburg Dominik D   Ahonen Lauri R LR   Amorim Antonio A   Baccarini Andrea A   Bauer Paulus S PS   Baumgartner Bernhard B   Bergen Anton A   Bernhammer Anne-Kathrin AK   Breitenlechner Martin M   Brilke Sophia S   Buchholz Angela A   Mazon Stephany Buenrostro SB   Chen Dexian D   Chen Xuemeng X   Dias Antonio A   Dommen Josef J   Draper Danielle C DC   Duplissy Jonathan J   Ehn Mikael M   Finkenzeller Henning H   Fischer Lukas L   Frege Carla C   Fuchs Claudia C   Garmash Olga O   Gordon Hamish H   Hakala Jani J   He Xucheng X   Heikkinen Liine L   Heinritzi Martin M   Helm Johanna C JC   Hofbauer Victoria V   Hoyle Christopher R CR   Jokinen Tuija T   Kangasluoma Juha J   Kerminen Veli-Matti VM   Kim Changhyuk C   Kirkby Jasper J   Kontkanen Jenni J   Kürten Andreas A   Lawler Michael J MJ   Mai Huajun H   Mathot Serge S   Mauldin Roy L RL   Molteni Ugo U   Nichman Leonid L   Nie Wei W   Nieminen Tuomo T   Ojdanic Andrea A   Onnela Antti A   Passananti Monica M   Petäjä Tuukka T   Piel Felix F   Pospisilova Veronika V   Quéléver Lauriane L J LLJ   Rissanen Matti P MP   Rose Clémence C   Sarnela Nina N   Schallhart Simon S   Schuchmann Simone S   Sengupta Kamalika K   Simon Mario M   Sipilä Mikko M   Tauber Christian C   Tomé António A   Tröstl Jasmin J   Väisänen Olli O   Vogel Alexander L AL   Volkamer Rainer R   Wagner Andrea C AC   Wang Mingyi M   Weitz Lena L   Wimmer Daniela D   Ye Penglin P   Ylisirniö Arttu A   Zha Qiaozhi Q   Carslaw Kenneth S KS   Curtius Joachim J   Donahue Neil M NM   Flagan Richard C RC   Hansel Armin A   Riipinen Ilona I   Virtanen Annele A   Winkler Paul M PM   Baltensperger Urs U   Kulmala Markku M   Worsnop Douglas R DR  

Science advances 20181212 12


A major fraction of atmospheric aerosol particles, which affect both air quality and climate, form from gaseous precursors in the atmosphere. Highly oxygenated organic molecules (HOMs), formed by oxidation of biogenic volatile organic compounds, are known to participate in particle formation and growth. However, it is not well understood how they interact with atmospheric pollutants, such as nitrogen oxides (NO <sub><i>x</i></sub> ) and sulfur oxides (SO <sub><i>x</i></sub> ) from fossil fuel co  ...[more]

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