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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>
<abbrev-journal-title abbrev-type="nlm-ta">Atmos. Chem. Phys.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7324</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/acp-9-5921-2009</article-id>
<title-group>
<article-title>Measurements of particle masses of inorganic salt particles for calibration of cloud condensation nuclei counters</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kuwata</surname>
<given-names>M.</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>Kondo</surname>
<given-names>Y.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Research Center for Advanced Science and Technology, the University of Tokyo, Tokyo, Japan</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>currently at: School of Engineering and Applied Sciences, Harvard University, Cambridge, MA, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>19</day>
<month>08</month>
<year>2009</year>
</pub-date>
<volume>9</volume>
<issue>16</issue>
<fpage>5921</fpage>
<lpage>5932</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2009 M. Kuwata</copyright-statement>
<copyright-year>2009</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://acp.copernicus.org/articles/9/5921/2009/acp-9-5921-2009.html">This article is available from https://acp.copernicus.org/articles/9/5921/2009/acp-9-5921-2009.html</self-uri>
<self-uri xlink:href="https://acp.copernicus.org/articles/9/5921/2009/acp-9-5921-2009.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/articles/9/5921/2009/acp-9-5921-2009.pdf</self-uri>
<abstract>
<p>We measured the mobility equivalent critical dry diameter for cloud
condensation nuclei (CCN) activation (&lt;i&gt;d&lt;sub&gt;c_me&lt;/sub&gt;&lt;/i&gt;) and the particle mass of
size-selected (NH&lt;sub&gt;4&lt;/sub&gt;)&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt; and NaCl particles to calibrate a CCN
counter (CCNC) precisely. The CCNC was operated downstream of a differential
mobility analyzer (DMA) for the measurement of &lt;i&gt;d&lt;sub&gt;c_me&lt;/sub&gt;&lt;/i&gt;. The particle mass
was measured using an aerosol particle mass analyzer (APM) operated
downstream of the DMA. The measurement of particle mass was conducted for
50–150-nm particles. Effective densities (&amp;rho;&lt;sub&gt;eff&lt;/sub&gt;) of
(NH&lt;sub&gt;4&lt;/sub&gt;)&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt; particles were 1.67–1.75 g cm&lt;sup&gt;&amp;minus;3&lt;/sup&gt;, which
correspond to dynamic shape factors (χ) of 1.01–1.04. This shows
that (NH&lt;sub&gt;4&lt;/sub&gt;)&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt; particles are not completely spherical. In the
case of NaCl particles, &amp;rho;&lt;sub&gt;eff&lt;/sub&gt; was 1.75–1.99 g cm&lt;sup&gt;&amp;minus;3&lt;/sup&gt;
and χ was 1.05–1.14, demonstrating that the particle shape was
non-spherical. Using these experimental data, the volume equivalent critical
dry diameter (&lt;i&gt;d&lt;sub&gt;c_ve&lt;/sub&gt;&lt;/i&gt;) was calculated, and it was used as an input
parameter for calculations of critical supersaturation (&lt;i&gt;S&lt;/i&gt;). Several
thermodynamics models were used for the calculation of water activity. When
the Pitzer model was employed for the calculations, the critical &lt;i&gt;S&lt;/i&gt; calculated
for (NH&lt;sub&gt;4&lt;/sub&gt;)&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt; and NaCl agreed to well within the uncertainty
of 2% (relative). This result demonstrates that the use of the Pitzer
model for the calibration of CCNCs gives the most accurate value of &lt;i&gt;S&lt;/i&gt;.</p>
</abstract>
<counts><page-count count="12"/></counts>
</article-meta>
</front>
<body/>
<back>
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