Observations of aerosol volatility and elemental composition at Macquarie Island during the First Aerosol Characterization Experiment (ACE 1)
A combined thermal/electron microscopy technique was used to analyze marine aerosol samples from Macquarie Island, obtained during November and December 1995 as part of the First Aerosol Characterization Experiment (ACE 1). The analyses were performed for two size fractions, Dp between 80 and 200 nm...
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Veröffentlicht in: | Journal of Geophysical Research 1998-07, Vol.103 (D13), p.16 |
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creator | Kreidenweis, S M McInnes, L M Brechtel, F J |
description | A combined thermal/electron microscopy technique was used to analyze marine aerosol samples from Macquarie Island, obtained during November and December 1995 as part of the First Aerosol Characterization Experiment (ACE 1). The analyses were performed for two size fractions, Dp between 80 and 200 nm and Dp larger than 200 nm. Sulfate particles were primarily observed in the former fraction and were deduced to be present also at smaller sizes from the volatile response of the aerosol. In two of the samples early in the experiment, sulfate particles appeared to be partially or fully neutralized, but the particles in later samples from clean marine air masses were more volatile, suggesting a sulfuric or methane-sulfonic acid composition. Sea-salt particles dominated the number concentrations of particles with Dp larger than 200 nm and also contributed significantly to the number concentrations in the Dp between 80 and 200 nm fraction. Evidence for increased sea-salt number concentrations at higher wind speeds was found. (Author) |
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The analyses were performed for two size fractions, Dp between 80 and 200 nm and Dp larger than 200 nm. Sulfate particles were primarily observed in the former fraction and were deduced to be present also at smaller sizes from the volatile response of the aerosol. In two of the samples early in the experiment, sulfate particles appeared to be partially or fully neutralized, but the particles in later samples from clean marine air masses were more volatile, suggesting a sulfuric or methane-sulfonic acid composition. Sea-salt particles dominated the number concentrations of particles with Dp larger than 200 nm and also contributed significantly to the number concentrations in the Dp between 80 and 200 nm fraction. Evidence for increased sea-salt number concentrations at higher wind speeds was found. (Author)</description><identifier>ISSN: 0148-0227</identifier><language>eng</language><ispartof>Journal of Geophysical Research, 1998-07, Vol.103 (D13), p.16</ispartof><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,777,781</link.rule.ids></links><search><creatorcontrib>Kreidenweis, S M</creatorcontrib><creatorcontrib>McInnes, L M</creatorcontrib><creatorcontrib>Brechtel, F J</creatorcontrib><title>Observations of aerosol volatility and elemental composition at Macquarie Island during the First Aerosol Characterization Experiment (ACE 1)</title><title>Journal of Geophysical Research</title><description>A combined thermal/electron microscopy technique was used to analyze marine aerosol samples from Macquarie Island, obtained during November and December 1995 as part of the First Aerosol Characterization Experiment (ACE 1). The analyses were performed for two size fractions, Dp between 80 and 200 nm and Dp larger than 200 nm. Sulfate particles were primarily observed in the former fraction and were deduced to be present also at smaller sizes from the volatile response of the aerosol. In two of the samples early in the experiment, sulfate particles appeared to be partially or fully neutralized, but the particles in later samples from clean marine air masses were more volatile, suggesting a sulfuric or methane-sulfonic acid composition. Sea-salt particles dominated the number concentrations of particles with Dp larger than 200 nm and also contributed significantly to the number concentrations in the Dp between 80 and 200 nm fraction. Evidence for increased sea-salt number concentrations at higher wind speeds was found. 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The analyses were performed for two size fractions, Dp between 80 and 200 nm and Dp larger than 200 nm. Sulfate particles were primarily observed in the former fraction and were deduced to be present also at smaller sizes from the volatile response of the aerosol. In two of the samples early in the experiment, sulfate particles appeared to be partially or fully neutralized, but the particles in later samples from clean marine air masses were more volatile, suggesting a sulfuric or methane-sulfonic acid composition. Sea-salt particles dominated the number concentrations of particles with Dp larger than 200 nm and also contributed significantly to the number concentrations in the Dp between 80 and 200 nm fraction. Evidence for increased sea-salt number concentrations at higher wind speeds was found. (Author)</abstract></addata></record> |
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title | Observations of aerosol volatility and elemental composition at Macquarie Island during the First Aerosol Characterization Experiment (ACE 1) |
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