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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-8-3427-2008</article-id>
<title-group>
<article-title>Modelling the optical properties of fresh biomass burning  aerosol produced in a smoke chamber: results from the EFEU campaign</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hungershoefer</surname>
<given-names>K.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</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>Zeromskiene</surname>
<given-names>K.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Iinuma</surname>
<given-names>Y.</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>Helas</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>Trentmann</surname>
<given-names>J.</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>Trautmann</surname>
<given-names>T.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Parmar</surname>
<given-names>R. S.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</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>Wiedensohler</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>Andreae</surname>
<given-names>M. O.</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>Schmid</surname>
<given-names>O.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
<xref ref-type="aff" rid="aff7">
<sup>7</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Institute for Meteorology, University of Leipzig,  Leipzig, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Leibniz-Institute for Tropospheric Research,  Leipzig, Germany</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Max Planck Institute for  Chemistry, Biogeochemistry Dept., Mainz, Germany</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Centre for Atmospheric Chemistry, York University, Toronto, Canada</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Institute for Atmospheric Physics, Johannes Gutenberg University Mainz, Mainz, Germany</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>Remote Sensing Technology Institute, German Aerospace Centre, Wessling, Germany</addr-line>
</aff>
<aff id="aff7">
<label>7</label>
<addr-line>Institute for Inhalation Biology, GSF-National Research Centre for Environment and Health, Neuherberg, Germany</addr-line>
</aff>
<aff id="aff8">
<label>8</label>
<addr-line>IIMT Engineering College, Department of Applied Science, Ganga Nagar, Meerut, India</addr-line>
</aff>
<aff id="aff9">
<label>9</label>
<addr-line>now at: Laboratoire Inter-Universitaire des Systèmes Atmosphériques (LISA), Université Paris 7/12 and CNRS (UMR 7583), Créteil, France</addr-line>
</aff>
<pub-date pub-type="epub">
<day>02</day>
<month>07</month>
<year>2008</year>
</pub-date>
<volume>8</volume>
<issue>13</issue>
<fpage>3427</fpage>
<lpage>3439</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>
<self-uri xlink:href="http://www.atmos-chem-phys.net/8/3427/2008/acp-8-3427-2008.html">This article is available from http://www.atmos-chem-phys.net/8/3427/2008/acp-8-3427-2008.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/8/3427/2008/acp-8-3427-2008.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/8/3427/2008/acp-8-3427-2008.pdf</self-uri>
<abstract>
<p>A better characterisation of the optical properties of biomass
  burning aerosol as a function of the burning conditions is required
  in order to quantify their effects on climate and atmospheric
  chemistry. Controlled laboratory combustion experiments with
  different fuel types were carried out at the combustion facility of
  the Max Planck Institute for Chemistry (Mainz, Germany) as part of
  the &quot;Impact of Vegetation Fires on the Composition and Circulation
  of the Atmosphere&quot; (EFEU) project. The combustion conditions were
  monitored with concomitant CO&lt;sub&gt;2&lt;/sub&gt; and CO measurements. The mass
  scattering efficiencies of 8.9&amp;plusmn;0.2 m&lt;sup&gt;2&lt;/sup&gt; g&lt;sup&gt;&amp;minus;1&lt;/sup&gt; and
  9.3&amp;plusmn;0.3 m&lt;sup&gt;2&lt;/sup&gt; g&lt;sup&gt;&amp;minus;1&lt;/sup&gt; obtained for aerosol particles from the
  combustion of savanna grass and an African hardwood (musasa),
  respectively, are larger than typically reported mainly due to
  differences in particle size distribution. The photoacoustically
  measured mass absorption efficiencies of
  0.51&amp;plusmn;0.02 m&lt;sup&gt;2&lt;/sup&gt; g&lt;sup&gt;&amp;minus;1&lt;/sup&gt; and 0.50&amp;plusmn;0.02 m&lt;sup&gt;2&lt;/sup&gt; g&lt;sup&gt;&amp;minus;1&lt;/sup&gt;
  were at the lower end of the literature values. Using the measured
  size distributions as well as the mass scattering and absorption
  efficiencies, Mie calculations provided effective refractive indices
  of 1.60&amp;minus;0.010&lt;i&gt;i&lt;/i&gt; (savanna grass) and 1.56&amp;minus;0.010&lt;i&gt;i&lt;/i&gt; (musasa)
  (λ=0.55 μm).
  The apparent discrepancy between the low imaginary part of the
  refractive index and the high apparent elemental carbon
  (EC&lt;sub&gt;a&lt;/sub&gt;) fractions (8 to 15%) obtained from
  the thermographic analysis of impactor samples can be explained by a
  positive bias in the elemental carbon data due to the presence of
  high molecular weight organic substances.  Potential artefacts in
  optical properties due to instrument bias, non-natural burning
  conditions and unrealistic dilution history of the laboratory smoke
  cannot be ruled out and are also discussed in this study.</p>
</abstract>
<counts><page-count count="13"/></counts>
</article-meta>
</front>
<body/>
<back>
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