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<article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" article-type="research-article" dtd-version="3.0" xml:lang="en">
<front>
<journal-meta>
<journal-id journal-id-type="publisher">AMT</journal-id>
<journal-title-group>
<journal-title>Atmospheric Measurement Techniques</journal-title>
<abbrev-journal-title abbrev-type="publisher">AMT</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Atmos. Meas. Tech.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1867-8548</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/amt-4-445-2011</article-id>
<title-group>
<article-title>Characterization of aerosol photooxidation flow reactors: heterogeneous oxidation, secondary organic aerosol formation and cloud condensation nuclei activity measurements</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Lambe</surname>
<given-names>A. T.</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>Ahern</surname>
<given-names>A. T.</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>Williams</surname>
<given-names>L. R.</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>Slowik</surname>
<given-names>J. 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>Wong</surname>
<given-names>J. P. 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>Abbatt</surname>
<given-names>J. P. D.</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>Brune</surname>
<given-names>W. H.</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>Ng</surname>
<given-names>N. L.</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>Wright</surname>
<given-names>J. P.</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>Croasdale</surname>
<given-names>D. 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>Worsnop</surname>
<given-names>D. R.</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>Davidovits</surname>
<given-names>P.</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>Onasch</surname>
<given-names>T. B.</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-group><aff id="aff1">
<label>1</label>
<addr-line>Chemistry Department, Boston College, Chestnut Hill, MA, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Aerodyne Research Inc., Billerica, MA, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Department of Chemistry, University of Toronto, Toronto, ON, Canada</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Department of Meteorology and Atmospheric Sciences, The Pennsylvania State University, State College, PA, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>04</day>
<month>03</month>
<year>2011</year>
</pub-date>
<volume>4</volume>
<issue>3</issue>
<fpage>445</fpage>
<lpage>461</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2011 A. T. Lambe et al.</copyright-statement>
<copyright-year>2011</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://amt.copernicus.org/articles/4/445/2011/amt-4-445-2011.html">This article is available from https://amt.copernicus.org/articles/4/445/2011/amt-4-445-2011.html</self-uri>
<self-uri xlink:href="https://amt.copernicus.org/articles/4/445/2011/amt-4-445-2011.pdf">The full text article is available as a PDF file from https://amt.copernicus.org/articles/4/445/2011/amt-4-445-2011.pdf</self-uri>
<abstract>
<p>Motivated by the need to develop instrumental techniques for
      characterizing organic aerosol aging, we report on the
      performance of the Toronto Photo-Oxidation Tube (TPOT) and
      Potential Aerosol Mass (PAM) flow tube reactors under
      a variety of experimental conditions. The PAM system was designed with lower surface-area-to-volume (SA/V) ratio to
      minimize wall effects; the TPOT reactor was designed
      to study heterogeneous aerosol chemistry where wall loss can be independently measured. The following
      studies were performed: (1) transmission efficiency
      measurements for CO&lt;sub&gt;2&lt;/sub&gt;, SO&lt;sub&gt;2&lt;/sub&gt;, and bis(2-ethylhexyl)
      sebacate (BES) particles, (2) H&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt; yield
      measurements from the oxidation of SO&lt;sub&gt;2&lt;/sub&gt;, (3) residence
      time distribution (RTD) measurements for CO&lt;sub&gt;2&lt;/sub&gt;, SO&lt;sub&gt;2&lt;/sub&gt;,
      and BES particles, (4) aerosol mass spectra, O/C and H/C ratios, and cloud
      condensation nuclei (CCN) activity measurements of BES
      particles exposed to OH radicals, and (5) aerosol mass spectra, O/C and H/C ratios, CCN activity, and yield measurements of secondary
      organic aerosol (SOA) generated from gas-phase OH oxidation of
      &lt;i&gt;m&lt;/i&gt;-xylene and α-pinene. OH exposures ranged from
      (2.0 &amp;plusmn; 1.0) × 10&lt;sup&gt;10&lt;/sup&gt; to (1.8 ± 0.3) × 10&lt;sup&gt;12&lt;/sup&gt; molec cm&lt;sup&gt;−3&lt;/sup&gt; s. Where applicable, data from the flow tube
      reactors are compared with published results from the Caltech
      smog chamber. The TPOT yielded narrower RTDs. However, its
      transmission efficiency for SO&lt;sub&gt;2&lt;/sub&gt; was lower than that for
      the PAM. Transmission efficiency for BES and H&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt;
      particles was size-dependent and was similar for the two flow
      tube designs. Oxidized BES particles had similar O/C and H/C ratios and CCN activity at OH exposures greater than
      10&lt;sup&gt;11&lt;/sup&gt; molec cm&lt;sup&gt;−3&lt;/sup&gt; s, but different CCN activity at
      lower OH exposures. The O/C ratio, H/C ratio, and yield of &lt;i&gt;m&lt;/i&gt;-xylene and
      α-pinene SOA was strongly affected by reactor design
      and operating conditions, with wall interactions seemingly
      having the strongest influence on SOA yield. At comparable OH
      exposures, flow tube SOA was more oxidized than smog chamber
      SOA, possibly because of faster gas-phase oxidation relative to particle
      nucleation. SOA yields were lower in the TPOT than in the PAM,
      but CCN activity of flow-tube-generated SOA particles was
      similar. For comparable OH exposures, α-pinene SOA
      yields were similar in the PAM and Caltech chambers, but
      &lt;i&gt;m&lt;/i&gt;-xylene SOA yields were much lower in the PAM compared to the
      Caltech chamber.</p>
</abstract>
<counts><page-count count="17"/></counts>
</article-meta>
</front>
<body/>
<back>
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