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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>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-10-5625-2010</article-id>
<title-group>
<article-title>Hygroscopic properties of Amazonian biomass burning and European background HULIS and investigation of their effects on surface tension with two models linking H-TDMA to CCNC data</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Fors</surname>
<given-names>E. O.</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>Rissler</surname>
<given-names>J.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff7">
<sup>7</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Massling</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff8">
<sup>8</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Svenningsson</surname>
<given-names>B.</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>Andreae</surname>
<given-names>M. O.</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>Dusek</surname>
<given-names>U.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff9">
<sup>9</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Frank</surname>
<given-names>G. P.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff10">
<sup>10</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hoffer</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff11">
<sup>11</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Bilde</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>Kiss</surname>
<given-names>G.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Janitsek</surname>
<given-names>S.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Henning</surname>
<given-names>S.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</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="aff6">
<sup>6</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="aff6">
<sup>6</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Swietlicki</surname>
<given-names>E.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Lund University, Department of Physics, Division of Nuclear Physics, Lund, Sweden</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Max Planck Institute for Chemistry, Department of Biogeochemistry, Mainz, Germany</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>University of Copenhagen, Department of Chemistry, Copenhagen, Denmark</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>University of Pannonia, Air Chemistry Group of the Hungarian Academy of Sciences, Veszprém, Hungary</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Leibniz-Institute for Tropospheric Research, Department of Physics, Leipzig, Germany</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>Istituto di Scienze dell&apos;Atmosfera e del Clima – CNR, Bologna, Italy</addr-line>
</aff>
<aff id="aff7">
<label>7</label>
<addr-line>now at: Lund University, Department of Design Sciences, Division of Ergonomics and Aerosol Technology, Lund, Sweden</addr-line>
</aff>
<aff id="aff8">
<label>8</label>
<addr-line>now at: Aarhus University, National Environmental Research Institute, Department of Atmospheric Environment, Roskilde, Denmark</addr-line>
</aff>
<aff id="aff9">
<label>9</label>
<addr-line>now at: Utrecht University, Institute for Marine and Atmospheric Research, Utrecht, The Netherlands</addr-line>
</aff>
<aff id="aff10">
<label>10</label>
<addr-line>now at: Lund University, Department of Physics, Division of Nuclear Physics, Lund, Sweden</addr-line>
</aff>
<aff id="aff11">
<label>11</label>
<addr-line>now at: University of Pannonia, Air Chemistry Group of the Hungarian Academy of Sciences, Veszprém, Hungary</addr-line>
</aff>
<pub-date pub-type="epub">
<day>28</day>
<month>06</month>
<year>2010</year>
</pub-date>
<volume>10</volume>
<issue>12</issue>
<fpage>5625</fpage>
<lpage>5639</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/10/5625/2010/acp-10-5625-2010.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/10/5625/2010/acp-10-5625-2010.pdf</self-uri>
<abstract>
<p>HUmic-LIke Substances (HULIS) have been identified as major
contributors to the organic carbon in atmospheric aerosol. The term
&quot;HULIS&quot; is used to describe the organic material found in aerosol
particles that resembles the humic organic material in rivers and
sea water and in soils. In this study, two sets of filter samples
from atmospheric aerosols were collected at different sites. One set
of samples was collected at the K-puszta rural site in Hungary,
about 80 km SE of Budapest, and a second was collected at a site in
Rondônia, Amazonia, Brazil, during the Large-Scale
Biosphere-Atmosphere Experiment in Amazonia – Smoke Aerosols,
Clouds, Rainfall and Climate (LBA-SMOCC) biomass burning season
experiment. HULIS were extracted from the samples and their
hygroscopic properties were studied using a Hygroscopicity Tandem
Differential Mobility Analyzer (H-TDMA) at relative humidity (RH)
&lt;100%, and a cloud condensation nucleus counter (CCNC) at RH
&gt;100%. The H-TDMA measurements were carried out at a dry diameter
of 100 nm and for RH ranging from 30 to 98%. At 90% RH the HULIS
samples showed diameter growth factors between 1.04 and 1.07,
reaching values of 1.4 at 98% RH. The cloud nucleating properties
of the two sets of aerosol samples were analysed using two types of
thermal static cloud condensation nucleus counters. Two different
parameterization models were applied to investigate the potential
effect of HULIS surface activity, both yielding similar results. For
the K-puszta winter HULIS sample, the surface tension at the point
of activation was estimated to be lowered by between 34%
(47.7 mN/m) and 31% (50.3 mN/m) for dry sizes between 50 and
120 nm in comparison to pure water. A moderate lowering was also
observed for the entire water soluble aerosol sample, including both
organic and inorganic compounds, where the surface tension was
decreased by between 2% (71.2 mN/m) and 13% (63.3 mN/m).</p>
</abstract>
<counts><page-count count="15"/></counts>
</article-meta>
</front>
<body/>
<back>
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