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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>
<abbrev-journal-title abbrev-type="nlm-ta">Atmos. Chem. Phys. Discuss.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7375</issn>
<publisher><publisher-name></publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acpd-13-2313-2013</article-id>
<title-group>
<article-title>Total sulphate vs. sulphuric acid monomer in nucleation studies: which represents the &quot;true&quot; concentration?</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Neitola</surname>
<given-names>K.</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>Brus</surname>
<given-names>D.</given-names>
<ext-link>https://orcid.org/0000-0002-8766-7873</ext-link>
</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>Makkonen</surname>
<given-names>U.</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>Sipilä</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>Mauldin III</surname>
<given-names>R. L.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</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>Kyllönen</surname>
<given-names>K.</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>Lihavainen</surname>
<given-names>H.</given-names>
<ext-link>https://orcid.org/0000-0002-6135-4473</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kulmala</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Finnish Meteorological Institute, Erik Palménin aukio 1, P.O. Box 503, 00100 Helsinki, Finland</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Aerosols and Laser Studies, Institute of Chemical Process Fundamentals Academy of Sciences of the Czech Republic, Rozvojová 135, 165 02 Prague 6, Czech Republic</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Department of Physical Sciences, University of Helsinki, P.O. Box 64, 00014 Helsinki, Finland</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Institute for Arctic and Alpine Research, University of Colorado, Boulder, CO 80309, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>22</day>
<month>01</month>
<year>2013</year>
</pub-date>
<volume>13</volume>
<issue>1</issue>
<fpage>2313</fpage>
<lpage>2350</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2013 K. Neitola et al.</copyright-statement>
<copyright-year>2013</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/preprints/13/2313/2013/acpd-13-2313-2013.html">This article is available from https://acp.copernicus.org/preprints/13/2313/2013/acpd-13-2313-2013.html</self-uri>
<self-uri xlink:href="https://acp.copernicus.org/preprints/13/2313/2013/acpd-13-2313-2013.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/preprints/13/2313/2013/acpd-13-2313-2013.pdf</self-uri>
<abstract>
<p>Sulphuric acid is known to be a key component for atmospheric
nucleation. Precise determination of sulphuric acid concentration is
crucial factor for prediction of nucleation rates and subsequent
growth. In our study, we have noticed a substantial discrepancy
between sulphuric acid monomer and total sulphate concentrations
measured from the same source of sulphuric acid vapour. The
discrepancy of about one to two orders of magnitude was found with
similar formation rates. The reason for this difference is not yet
clear and it can have great impact on predicting atmospheric
nucleation rates as well as growth rates. To investigate this
discrepancy and its effect on nucleation, a method of thermally
controlled saturator filled with pure sulphuric acid (~97%)
for production of sulphuric acid vapour is introduced and
tested. Sulphuric acid-water nucleation experiment was done using
a laminar flow tube. Two independent methods of mass spectrometry and
online ion chromatography were used for detecting sulphuric acid
concentrations. The results are compared to our previous results,
where a method of evaporating weak sulphuric acid-water solution
droplets in a furnace was used to produce sulphuric acid vapour (Brus
et al., 2010, 2011). Measured sulphuric acid concentrations are
compared to theoretical prediction calculated using vapour pressure
and simple mixing law. The calculated prediction of sulphuric acid
concentrations agrees very well with the measured values when total
sulphate is considered. Sulphuric acid monomer concentration was found
to be about two orders of magnitude lower than the prediction, but
with similar temperature dependency as the prediction and the results
obtained with ion chromatograph method. Formation rates agree well
when compared to our previous results with both sulphuric acid
detection and sulphuric acid production methods separately.</p>
</abstract>
<counts><page-count count="38"/></counts>
</article-meta>
</front>
<body/>
<back>
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