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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACP</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACP</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7324</issn>
<publisher><publisher-name>Copernicus GmbH</publisher-name>
<publisher-loc>GÃ¶ttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-10-10111-2010</article-id>
<title-group>
<article-title>Analysis of the chemical composition of organic aerosol at the Mt. Sonnblick observatory using a novel high mass resolution thermal-desorption proton-transfer-reaction mass-spectrometer (hr-TD-PTR-MS)</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Holzinger</surname>
<given-names>R.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kasper-Giebl</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Staudinger</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Schauer</surname>
<given-names>G.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>RÃ¶ckmann</surname>
<given-names>T.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Institute for Marine and Atmospheric research Utrecht, Princetonplein 5, 3584 CC, Utrecht, The Netherlands</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Vienna Univ. Technol., Inst. Chem. Technol. a. Analytics, Vienna, Austria</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Cent. Inst.  Meteorol. &amp; Geodynam., Vienna, Austria</addr-line>
</aff>
<pub-date pub-type="epub">
<day>27</day>
<month>10</month>
<year>2010</year>
</pub-date>
<volume>10</volume>
<issue>20</issue>
<fpage>10111</fpage>
<lpage>10128</lpage>
<permissions>
<license xlink:type="simple">
<license-p>This is an open-access article ditributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.</license-p>
</license>
</permissions>
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<self-uri xlink:href="http://www.atmos-chem-phys.net/10/10111/2010/acp-10-10111-2010.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/10/10111/2010/acp-10-10111-2010.pdf</self-uri>
<abstract>
<p>For the first time a high mass resolution thermal desorption proton transfer
reaction mass spectrometer (hr-TD-PTR-MS) was deployed in the field to
analyze the composition of the organic fraction of aerosols. We report on
measurements from the remote Mt. Sonnblick observatory in the Austrian alps
(3108 m a.s.l.) during a 7 week period in summer 2009. A total of 638 mass
peaks in the range 18â€“392 Da were detected and quantified in aerosols. An
empirical formula was tentatively attributed to 464 of these compounds by
custom-made data analysis routines which consider compounds containing C, H,
O, N, and S atoms. Most of the other (unidentified) compounds must contain
other elements &amp;ndash; most likely halogenated compounds. The mean total
concentration of all detected compounds was 1.1 Î¼g m&lt;sup&gt;âˆ’3&lt;/sup&gt;. Oxygenated
hydrocarbons constitute the bulk of the aerosol mass (75%) followed by
organic nitrogen compounds (9%), inorganic compounds (mostly NH&lt;sub&gt;3&lt;/sub&gt;,
8%), unidentified/halogenated (3.8%), hydrocarbons (2.7%), and
organic sulfur compounds (0.8%). The measured O/C ratios are lower than
expected and suggest a significant effect from charring. Organic carbon
concentrations measured with TD-PTR-MS were about 25% lower than
measurements on high volume filter samples.</p>
</abstract>
<counts><page-count count="18"/></counts>
</article-meta>
</front>
<body/>
<back>
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