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Can Highly Oxidized Organics Contribute to Atmospheric New Particle Formation?

Highly oxidized organic molecules may play a critical role in new-particle formation within Earth’s atmosphere along with sulfuric acid, which has long been considered as a key compound in this process. Here we explore the interactions of these two partners, using quantum chemistry to find the forma...

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Autores principales: Ortega, Ismael K, Donahue, Neil M, Kurtén, Theo, Kulmala, Markku, Focsa, Cristian, Vehkamäki, Hanna
Lenguaje:eng
Publicado: 2015
Materias:
Acceso en línea:https://dx.doi.org/10.1021/acs.jpca.5b07427
http://cds.cern.ch/record/2310550
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author Ortega, Ismael K
Donahue, Neil M
Kurtén, Theo
Kulmala, Markku
Focsa, Cristian
Vehkamäki, Hanna
author_facet Ortega, Ismael K
Donahue, Neil M
Kurtén, Theo
Kulmala, Markku
Focsa, Cristian
Vehkamäki, Hanna
author_sort Ortega, Ismael K
collection CERN
description Highly oxidized organic molecules may play a critical role in new-particle formation within Earth’s atmosphere along with sulfuric acid, which has long been considered as a key compound in this process. Here we explore the interactions of these two partners, using quantum chemistry to find the formation free energies of heterodimers and trimers as well as the fastest evaporation rates of (2,2) tetramers. We find that the heterodimers are more strongly bound than pure sulfuric acid dimers. Their stability correlates well with the oxygen to carbon ratio of the organics, their volatility, and the number of hydrogen bonds formed. Most of the stable trimers contain one sulfuric acid and two organics (1,2), whereas many (2,2) tetramers evaporate quickly, probably due to the stability of (1,2) clusters. This finding agrees with recent experimental studies that show how new-particle formation involving oxidized organics and sulfuric acid may be rate-limited by activation of (1,2) trimers, confirming the importance of this process in the atmosphere.
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spelling oai-inspirehep.net-16638102019-09-30T06:29:59Zdoi:10.1021/acs.jpca.5b07427http://cds.cern.ch/record/2310550engOrtega, Ismael KDonahue, Neil MKurtén, TheoKulmala, MarkkuFocsa, CristianVehkamäki, HannaCan Highly Oxidized Organics Contribute to Atmospheric New Particle Formation?Nuclear Physics - ExperimentHighly oxidized organic molecules may play a critical role in new-particle formation within Earth’s atmosphere along with sulfuric acid, which has long been considered as a key compound in this process. Here we explore the interactions of these two partners, using quantum chemistry to find the formation free energies of heterodimers and trimers as well as the fastest evaporation rates of (2,2) tetramers. We find that the heterodimers are more strongly bound than pure sulfuric acid dimers. Their stability correlates well with the oxygen to carbon ratio of the organics, their volatility, and the number of hydrogen bonds formed. Most of the stable trimers contain one sulfuric acid and two organics (1,2), whereas many (2,2) tetramers evaporate quickly, probably due to the stability of (1,2) clusters. This finding agrees with recent experimental studies that show how new-particle formation involving oxidized organics and sulfuric acid may be rate-limited by activation of (1,2) trimers, confirming the importance of this process in the atmosphere.oai:inspirehep.net:16638102015
spellingShingle Nuclear Physics - Experiment
Ortega, Ismael K
Donahue, Neil M
Kurtén, Theo
Kulmala, Markku
Focsa, Cristian
Vehkamäki, Hanna
Can Highly Oxidized Organics Contribute to Atmospheric New Particle Formation?
title Can Highly Oxidized Organics Contribute to Atmospheric New Particle Formation?
title_full Can Highly Oxidized Organics Contribute to Atmospheric New Particle Formation?
title_fullStr Can Highly Oxidized Organics Contribute to Atmospheric New Particle Formation?
title_full_unstemmed Can Highly Oxidized Organics Contribute to Atmospheric New Particle Formation?
title_short Can Highly Oxidized Organics Contribute to Atmospheric New Particle Formation?
title_sort can highly oxidized organics contribute to atmospheric new particle formation?
topic Nuclear Physics - Experiment
url https://dx.doi.org/10.1021/acs.jpca.5b07427
http://cds.cern.ch/record/2310550
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