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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACPD</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACPD</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7375</issn>
<publisher><publisher-name>Copernicus GmbH</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acpd-5-9447-2005</article-id>
<title-group>
<article-title>Functional group analysis by H NMR/ chemical derivatization for the characterization of organic aerosol from the SMOCC field campaign</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Tagliavini</surname>
<given-names>E.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Moretti</surname>
<given-names>F.</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>Decesari</surname>
<given-names>S.</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>Facchini</surname>
<given-names>M. C.</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>Fuzzi</surname>
<given-names>S.</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>Maenhaut</surname>
<given-names>W.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Dipartimento di Chimica “G. Ciamician&quot;, Università di Bologna, Bologna, Italy</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Centro di Ricerche per le Scienze Ambientali, Università di Bologna, Ravenna, Italy</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Istituto di Scienze dell’Atmosfera e del Clima – C.N.R., Bologna, Italy</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Department of Analytical Chemistry, Institute for Nuclear Sciences, Ghent University, Gent, Belgium</addr-line>
</aff>
<pub-date pub-type="epub">
<day>29</day>
<month>09</month>
<year>2005</year>
</pub-date>
<volume>5</volume>
<issue>5</issue>
<fpage>9447</fpage>
<lpage>9491</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-discuss.net/5/9447/2005/acpd-5-9447-2005.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/5/9447/2005/acpd-5-9447-2005.pdf</self-uri>
<abstract>
<p>Water soluble organic compounds (WSOC) in aerosol samples collected in the
Amazon Basin in a period encompassing the middle/late dry season and the
beginning of the wet season, were investigated by H NMR spectroscopy. HiVol
filter samples (PM&lt;sub&gt;2.5&lt;/sub&gt; and PM&amp;gt;2.5) and size-segregated samples from
multistage impactor were subjected to H NMR characterization. The H NMR
methodology, recently developed for the analysis of organic aerosol samples,
has been improved exploiting chemical methylation of carboxylic groups
with diazomethane, which allows the direct determination of the carboxylic
acid content of WSOC. The content of carboxylic carbons for the different
periods and sizes ranged from 12% to 20% of total measured carbon
depending on the season and aerosol size, with higher contents for the fine
particles in the transition and wet periods with respect to the dry period.
A comprehensive picture is presented of WSOC functional groups in aerosol
samples representative of the biomass burning period, as well as of
transition and semi-clean atmospheric conditions. A difference in
composition between fine (PM&lt;sub&gt;2.5&lt;/sub&gt;) and coarse (PM&amp;gt;2.5) size fractions
emerged from the NMR data, the former showing higher alkylic content, the
latter being largely dominated by R-O-H (or R-O-R&apos;) functional groups,
likely coming from polyols. Very small particles (&amp;lt;0.14 &amp;micro;m),
however, present higher alkyl-chain content and less oxygenated carbons than
larger fine particles (0.42&amp;ndash;1.2 &amp;micro;m). More limited variations were found
between the average compositions in the different periods of the campaign.</p>
</abstract>
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