SOA formation from naphthalene, 1-methylnaphthalene, and 2-methylnaphthalene photooxidation
The SOA yield and chemical characteristics of SOA formation from naphthalene and two methyl substituted naphthalenes, 1-methylnaphthalene and 2-methylnaphthalene, were studied for high NOx, low NOx, and ultra-low NOx conditions. The SOA yields are high compared to previous studies for all three PAHs...
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Veröffentlicht in: | Atmospheric environment (1994) 2016-04, Vol.131, p.424-433 |
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description | The SOA yield and chemical characteristics of SOA formation from naphthalene and two methyl substituted naphthalenes, 1-methylnaphthalene and 2-methylnaphthalene, were studied for high NOx, low NOx, and ultra-low NOx conditions. The SOA yields are high compared to previous studies for all three PAHs precursors: 1-methylnaphthalene > 2-methylnaphthalene ∼ naphthalene for all atmospheric conditions studied. The SOA yields range from 0.03 to 0.60 for naphthalene, 0.21–1.52 for 1-methylnaphthalene, and 0.34–0.55 for 2-methylnaphthalene under high NOx with HONO (initial PAH:NO ratio = 0.03–0.17) conditions. The SOA yield ranges from 0.04 to 0.31 for naphthalene, 0.14–0.72 for 1-methylnaphthalene, and 0.06–0.49 for 2-methylnaphthalene under low NOx (initial PAH:NO ratio = 0.54–2.20) conditions. SOA yields were substantially greater than 1.0 under H2O2 (ultra low NOx) and low NOx + H2O2 conditions for all three PAH precursors. The system reactivity influenced by OH radicals, NOx levels, initial PAH/NO ratios, NO2/NO ratios, and all impacted the SOA formation from the PAH precursors. Fractal-like SOA is observed for the methylnaphthalene isomers during high NOx photooxidation experiments, implying that researchers studying SOA formation from this precursor must carefully account for particle shape or effective density. A m/z 104 (C7H4O+,104.026) peak, consistent with SOA products phthalic acid from earlier studies, was observed as a potential marker of PAH oxidation during HR-ToF-AMS analysis.
•High SOA yields from 2-ring PAH photooxidation were found.•Fractal-like and solid SOA was observed for the methylnaphthalene isomers during high NOx photooxidation.•A m/z 104 peak was observed as a marker of phthalic acid from PAH photoxidation by HR-ToF-AMS analysis. |
doi_str_mv | 10.1016/j.atmosenv.2016.02.007 |
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•High SOA yields from 2-ring PAH photooxidation were found.•Fractal-like and solid SOA was observed for the methylnaphthalene isomers during high NOx photooxidation.•A m/z 104 peak was observed as a marker of phthalic acid from PAH photoxidation by HR-ToF-AMS analysis.</description><identifier>ISSN: 1352-2310</identifier><identifier>EISSN: 1873-2844</identifier><identifier>DOI: 10.1016/j.atmosenv.2016.02.007</identifier><language>eng</language><publisher>Elsevier Ltd</publisher><subject>Fractal agglomerate ; m/z 104 ; Methylnaphthalene ; Naphthalene ; PAH ; SOA yield</subject><ispartof>Atmospheric environment (1994), 2016-04, Vol.131, p.424-433</ispartof><rights>2016 Elsevier Ltd</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c459t-7e9ec1175c73e362a7fac055a9a9f22e77340fc06f9adc111c42ad7289d40b0f3</citedby><cites>FETCH-LOGICAL-c459t-7e9ec1175c73e362a7fac055a9a9f22e77340fc06f9adc111c42ad7289d40b0f3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/j.atmosenv.2016.02.007$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,780,784,3550,27924,27925,45995</link.rule.ids></links><search><creatorcontrib>Chen, Chia-Li</creatorcontrib><creatorcontrib>Kacarab, Mary</creatorcontrib><creatorcontrib>Tang, Ping</creatorcontrib><creatorcontrib>Cocker, David R.</creatorcontrib><title>SOA formation from naphthalene, 1-methylnaphthalene, and 2-methylnaphthalene photooxidation</title><title>Atmospheric environment (1994)</title><description>The SOA yield and chemical characteristics of SOA formation from naphthalene and two methyl substituted naphthalenes, 1-methylnaphthalene and 2-methylnaphthalene, were studied for high NOx, low NOx, and ultra-low NOx conditions. The SOA yields are high compared to previous studies for all three PAHs precursors: 1-methylnaphthalene > 2-methylnaphthalene ∼ naphthalene for all atmospheric conditions studied. The SOA yields range from 0.03 to 0.60 for naphthalene, 0.21–1.52 for 1-methylnaphthalene, and 0.34–0.55 for 2-methylnaphthalene under high NOx with HONO (initial PAH:NO ratio = 0.03–0.17) conditions. The SOA yield ranges from 0.04 to 0.31 for naphthalene, 0.14–0.72 for 1-methylnaphthalene, and 0.06–0.49 for 2-methylnaphthalene under low NOx (initial PAH:NO ratio = 0.54–2.20) conditions. SOA yields were substantially greater than 1.0 under H2O2 (ultra low NOx) and low NOx + H2O2 conditions for all three PAH precursors. The system reactivity influenced by OH radicals, NOx levels, initial PAH/NO ratios, NO2/NO ratios, and all impacted the SOA formation from the PAH precursors. Fractal-like SOA is observed for the methylnaphthalene isomers during high NOx photooxidation experiments, implying that researchers studying SOA formation from this precursor must carefully account for particle shape or effective density. A m/z 104 (C7H4O+,104.026) peak, consistent with SOA products phthalic acid from earlier studies, was observed as a potential marker of PAH oxidation during HR-ToF-AMS analysis.
•High SOA yields from 2-ring PAH photooxidation were found.•Fractal-like and solid SOA was observed for the methylnaphthalene isomers during high NOx photooxidation.•A m/z 104 peak was observed as a marker of phthalic acid from PAH photoxidation by HR-ToF-AMS analysis.</description><subject>Fractal agglomerate</subject><subject>m/z 104</subject><subject>Methylnaphthalene</subject><subject>Naphthalene</subject><subject>PAH</subject><subject>SOA yield</subject><issn>1352-2310</issn><issn>1873-2844</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2016</creationdate><recordtype>article</recordtype><recordid>eNqFkDtPwzAUhS0EEqXwF1BGBhKu7SRONqqKl1SpAzAxWMa5VlwlcbFdRP89KYUBMTDd1zlHuh8h5xQyCrS8WmUq9i7g8J6xcc6AZQDigExoJXjKqjw_HHtesJRxCsfkJIQVAHBRiwl5eVzOEuN8r6J1Q2K865NBrdvYqg4HvExo2mNst92vpRqahP09JOvWRec-bPOVdkqOjOoCnn3XKXm-vXma36eL5d3DfLZIdV7UMRVYo6ZUFFpw5CVTwigNRaFqVRvGUAieg9FQmlo1o5DqnKlGsKpucngFw6fkYp-79u5tgyHK3gaNXacGdJsgaQWMQS7KepSWe6n2LgSPRq697ZXfSgpyR1Ou5A9NuaMpgcmR5mi83htxfOTdopdBWxw0NtajjrJx9r-IT_M4gvg</recordid><startdate>201604</startdate><enddate>201604</enddate><creator>Chen, Chia-Li</creator><creator>Kacarab, Mary</creator><creator>Tang, Ping</creator><creator>Cocker, David R.</creator><general>Elsevier Ltd</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope></search><sort><creationdate>201604</creationdate><title>SOA formation from naphthalene, 1-methylnaphthalene, and 2-methylnaphthalene photooxidation</title><author>Chen, Chia-Li ; Kacarab, Mary ; Tang, Ping ; Cocker, David R.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c459t-7e9ec1175c73e362a7fac055a9a9f22e77340fc06f9adc111c42ad7289d40b0f3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2016</creationdate><topic>Fractal agglomerate</topic><topic>m/z 104</topic><topic>Methylnaphthalene</topic><topic>Naphthalene</topic><topic>PAH</topic><topic>SOA yield</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Chen, Chia-Li</creatorcontrib><creatorcontrib>Kacarab, Mary</creatorcontrib><creatorcontrib>Tang, Ping</creatorcontrib><creatorcontrib>Cocker, David R.</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Atmospheric environment (1994)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Chen, Chia-Li</au><au>Kacarab, Mary</au><au>Tang, Ping</au><au>Cocker, David R.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>SOA formation from naphthalene, 1-methylnaphthalene, and 2-methylnaphthalene photooxidation</atitle><jtitle>Atmospheric environment (1994)</jtitle><date>2016-04</date><risdate>2016</risdate><volume>131</volume><spage>424</spage><epage>433</epage><pages>424-433</pages><issn>1352-2310</issn><eissn>1873-2844</eissn><abstract>The SOA yield and chemical characteristics of SOA formation from naphthalene and two methyl substituted naphthalenes, 1-methylnaphthalene and 2-methylnaphthalene, were studied for high NOx, low NOx, and ultra-low NOx conditions. The SOA yields are high compared to previous studies for all three PAHs precursors: 1-methylnaphthalene > 2-methylnaphthalene ∼ naphthalene for all atmospheric conditions studied. The SOA yields range from 0.03 to 0.60 for naphthalene, 0.21–1.52 for 1-methylnaphthalene, and 0.34–0.55 for 2-methylnaphthalene under high NOx with HONO (initial PAH:NO ratio = 0.03–0.17) conditions. The SOA yield ranges from 0.04 to 0.31 for naphthalene, 0.14–0.72 for 1-methylnaphthalene, and 0.06–0.49 for 2-methylnaphthalene under low NOx (initial PAH:NO ratio = 0.54–2.20) conditions. SOA yields were substantially greater than 1.0 under H2O2 (ultra low NOx) and low NOx + H2O2 conditions for all three PAH precursors. The system reactivity influenced by OH radicals, NOx levels, initial PAH/NO ratios, NO2/NO ratios, and all impacted the SOA formation from the PAH precursors. Fractal-like SOA is observed for the methylnaphthalene isomers during high NOx photooxidation experiments, implying that researchers studying SOA formation from this precursor must carefully account for particle shape or effective density. A m/z 104 (C7H4O+,104.026) peak, consistent with SOA products phthalic acid from earlier studies, was observed as a potential marker of PAH oxidation during HR-ToF-AMS analysis.
•High SOA yields from 2-ring PAH photooxidation were found.•Fractal-like and solid SOA was observed for the methylnaphthalene isomers during high NOx photooxidation.•A m/z 104 peak was observed as a marker of phthalic acid from PAH photoxidation by HR-ToF-AMS analysis.</abstract><pub>Elsevier Ltd</pub><doi>10.1016/j.atmosenv.2016.02.007</doi><tpages>10</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Fractal agglomerate m/z 104 Methylnaphthalene Naphthalene PAH SOA yield |
title | SOA formation from naphthalene, 1-methylnaphthalene, and 2-methylnaphthalene photooxidation |
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