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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">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-4-323-2004</article-id>
<title-group>
<article-title>Interaction of aerosol particles composed of protein and saltswith water vapor: hygroscopic growth and microstructural rearrangement</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Mikhailov</surname>
<given-names>E.</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>Vlasenko</surname>
<given-names>S.</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>Niessner</surname>
<given-names>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>Pöschl</surname>
<given-names>U.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Technical University of Munich, Institute of Hydrochemistry, Marchioninistr. 17, D-81377 Munich, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Atmospheric Physics Department, Institute of Physics, St. Petersburg State University, Ulianovskaya 1, 198904 St. Petersburg, Russia</addr-line>
</aff>
<pub-date pub-type="epub">
<day>17</day>
<month>02</month>
<year>2004</year>
</pub-date>
<volume>4</volume>
<issue>2</issue>
<fpage>323</fpage>
<lpage>350</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/4/323/2004/acp-4-323-2004.html">This article is available from http://www.atmos-chem-phys.net/4/323/2004/acp-4-323-2004.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/4/323/2004/acp-4-323-2004.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/4/323/2004/acp-4-323-2004.pdf</self-uri>
<abstract>
<p>The interaction of aerosol particles composed of the protein
bovine serum albumin (BSA) and the inorganic salts sodium chloride
and ammonium nitrate with water vapor has been investigated by
hygroscopicity tandem differential mobility analyzer
(H-TDMA) experiments complemented by transmission electron
microscopy (TEM) and K&amp;#246;hler theory calculations (100-300nm
particle size range, 298K, 960hPa). BSA was chosen as a
well-defined model substance for proteins and other macromolecular
compounds, which constitute a large fraction of the water-soluble
organic component of air particulate matter.

&lt;P  style=&quot;line-height: 20px;&quot;&gt;
Pure BSA particles exhibited deliquescence and efflorescence
transitions at &lt;IMG WIDTH=&quot;15&quot; HEIGHT=&quot;15&quot; ALIGN=&quot;BOTTOM&quot; BORDER=&quot;0&quot;
   src=&quot;acp-4-323-img1.gif&quot;  
 ALT=&quot;$sim$&quot;&gt;35% relative humidity (&lt;IMG WIDTH=&quot;30&quot; HEIGHT=&quot;14&quot; ALIGN=&quot;BOTTOM&quot; BORDER=&quot;0&quot;
   src=&quot;acp-4-323-img2.gif&quot;  
 ALT=&quot;$RH$&quot;&gt;) and a
hygroscopic diameter increase by up to &lt;IMG WIDTH=&quot;15&quot; HEIGHT=&quot;15&quot; ALIGN=&quot;BOTTOM&quot; BORDER=&quot;0&quot;
   src=&quot;acp-4-323-img1.gif&quot;  
 ALT=&quot;$sim$&quot;&gt;10% at 95%
&lt;IMG WIDTH=&quot;30&quot; HEIGHT=&quot;14&quot; ALIGN=&quot;BOTTOM&quot; BORDER=&quot;0&quot;
   src=&quot;acp-4-323-img2.gif&quot;  
 ALT=&quot;$RH$&quot;&gt; in good agreement with model calculations based on a simple
parameterisation of the osmotic coefficient. Pure NaCl particles
were converted from near-cubic to near-spherical shape upon
interaction with water vapor at relative humidities below the
deliquescence threshold (partial surface dissolution and
recrystallisation), and the diameters of pure NH&lt;sub&gt;4&lt;/sub&gt;NO&lt;sub&gt;3&lt;/sub&gt; particles decreased by up to 10% due to chemical decomposition
and evaporation.

&lt;P  style=&quot;line-height: 20px;&quot;&gt;
Mixed NaCl-BSA and NH&lt;sub&gt;4&lt;/sub&gt;NO&lt;sub&gt;3&lt;/sub&gt;-BSA particles interacting
with water vapor exhibited mobility equivalent diameter reductions
of up to 20%, depending on particle generation, conditioning,
size, and chemical composition (BSA dry mass fraction 10-90%).
These observations can be explained by formation of porous
agglomerates (envelope void fractions up to 50%) due to
ion-protein interactions and electric charge effects on the one
hand, and by compaction of the agglomerate structure due to
capillary condensation effects on the other. The size of
NH&lt;sub&gt;4&lt;/sub&gt;NO&lt;sub&gt;3&lt;/sub&gt;-BSA particles was apparently also influenced
by volatilisation of NH&lt;sub&gt;4&lt;/sub&gt;NO&lt;sub&gt;3&lt;/sub&gt;, but not as much as for
pure salt particles, i.e. the protein inhibited the decomposition
of NH&lt;sub&gt;4&lt;/sub&gt;NO&lt;sub&gt;3&lt;/sub&gt; or the evaporation of the decomposition
products NH&lt;sub&gt;3&lt;/sub&gt; and HNO&lt;sub&gt;3&lt;/sub&gt;. The efflorescence
threshold of NaCl-BSA particles decreased with increasing BSA dry
mass fraction, i.e. the protein inhibited the formation of salt
crystals and enhanced the stability of supersaturated solution
droplets.

&lt;P  style=&quot;line-height: 20px;&quot;&gt;
The H-TDMA and TEM results indicate that the protein was enriched
at the surface of the mixed particles and formed an envelope,
which inhibits the access of water vapor to the particle core and
leads to kinetic limitations of hygroscopic growth, phase
transitions, and microstructural rearrangement processes.

&lt;P  style=&quot;line-height: 20px;&quot;&gt;
The K&amp;#246;hler theory calculations performed with different types
of models demonstrate that the hygroscopic growth of particles
composed of inorganic salts and proteins can be efficiently
described with a simple volume additivity approach, provided that
the correct dry solute mass equivalent diameter and composition
are known. A parameterisation for the osmotic coefficient of
macromolecular substances has been derived from an osmotic
pressure virial equation. For its application only the density and
molar mass of the substance have to be known or estimated, and it
is fully compatible with traditional volume additivity models for
salt mixtures.</p>
</abstract>
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