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Dataset associated with "Process-Level Modeling Can Simultaneously Explain Secondary Organic Aerosol Evolution in Chambers and Flow Reactors"

dc.contributor.authorHe, Yicong
dc.date.accessioned2022-04-07T20:02:30Z
dc.date.available2022-04-07T20:02:30Z
dc.date.issued2022
dc.descriptionData for the figures.en_US
dc.description.abstractSecondary organic aerosol (SOA) data gathered in environmental chambers (ECs) have been used extensively to develop parameters to represent SOA formation and evolution. The EC-based parameters are usually constrained to less than one day of photochemical aging, but extrapolated to predict SOA aging over much longer timescales in atmospheric models. Recently, SOA has been increasingly studied in oxidation flow reactors (OFRs) over aging timescales of one to multiple days. However, these OFR data have been rarely used to validate or update the EC-based parameters. The simultaneous use of EC and OFR data is challenging because the processes relevant to SOA formation and evolution proceed over very different timescales and both reactor types exhibit distinct experimental artifacts. In this work, we show that a kinetic SOA chemistry and microphysics model that accounts for various processes, including wall losses, aerosol phase state, heterogeneous oxidation, oligomerization and new particle formation, can simultaneously explain SOA evolution in EC and OFR experiments, using a single consistent set of SOA parameters. With α-pinene as an example, we first developed parameters by fitting the model output to the measured SOA mass concentration and oxygen-to-carbon (O:C) ratio from an EC experiment (<1 day of aging). We then used these parameters to simulate SOA formation in OFR experiments and found that the model overestimated SOA formation (by a factor of 3 to 16) over photochemical ages ranging from 0.4 to 13 days, when excluding the above-mentioned processes. By comprehensively accounting for these processes, the model was able to explain the observed evolution in SOA mass, composition (i.e., O:C), and size distribution in the OFR experiments. This work suggests that EC and OFR SOA data can be modeled consistently and a synergistic use of EC and OFR data can aid in developing more refined SOA parameters for use in atmospheric models.en_US
dc.description.sponsorshipUS Department of Energy, Office of Science; US Environmental Protection Agency.en_US
dc.format.mediumTXT
dc.identifier.urihttps://hdl.handle.net/10217/234640
dc.identifier.urihttp://dx.doi.org/10.25675/10217/234640
dc.languageEnglishen_US
dc.language.isoengen_US
dc.publisherColorado State University. Librariesen_US
dc.relation.ispartofResearch Data
dc.rights.licenseThe material is open access and distributed under the terms and conditions of the Creative Commons Public Domain "No rights reserved" (https://creativecommons.org/share-your-work/public-domain/cc0/).
dc.rights.urihttps://creativecommons.org/share-your-work/public-domain/cc0/
dc.subjectAtmospheric Pollutionen_US
dc.subjectSecondary Organic Aerosolen_US
dc.subjectAtmospheric Chemistryen_US
dc.subjectComputational Modelingen_US
dc.titleDataset associated with "Process-Level Modeling Can Simultaneously Explain Secondary Organic Aerosol Evolution in Chambers and Flow Reactors"en_US
dc.typeDataseten_US

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