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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-7-1441-2007</article-id>
<title-group>
<article-title>The tropospheric processing of acidic gases and hydrogen sulphide in volcanic gas plumes as inferred from field and model investigations</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Aiuppa</surname>
<given-names>A.</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>Franco</surname>
<given-names>A.</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>von Glasow</surname>
<given-names>R.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</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>Allen</surname>
<given-names>A. G.</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>D&apos;Alessandro</surname>
<given-names>W.</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>Mather</surname>
<given-names>T. A.</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>Pyle</surname>
<given-names>D. M.</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>Valenza</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-group><aff id="aff1">
<label>1</label>
<addr-line>Dipartimento CFTA, Università di Palermo, Palermo, Italy</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>INGV &amp;ndash; Sezione di Palermo, Palermo, Italy</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Institut für Umweltphysik, University of Heidelberg, Germany</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>School of Geography, Earth and Environmental Sciences, University of Birmingham, UK</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Earth Science Department, University of Oxford, UK</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>now at: School of Environmental Sciences, University of East Anglia, Norwich, UK</addr-line>
</aff>
<pub-date pub-type="epub">
<day>13</day>
<month>03</month>
<year>2007</year>
</pub-date>
<volume>7</volume>
<issue>5</issue>
<fpage>1441</fpage>
<lpage>1450</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>
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<abstract>
<p>Improving the constraints on the atmospheric fate and depletion rates of
acidic compounds persistently emitted by non-erupting (quiescent) volcanoes
is important for quantitatively predicting the environmental impact of
volcanic gas plumes. Here, we present new experimental data coupled with
modelling studies to investigate the chemical processing of acidic
volcanogenic species during tropospheric dispersion. Diffusive tube samplers
were deployed at Mount Etna, a very active open-conduit basaltic volcano in
eastern Sicily, and Vulcano Island, a closed-conduit quiescent volcano in
the Aeolian Islands (northern Sicily). Sulphur dioxide (SO&lt;sub&gt;2&lt;/sub&gt;), hydrogen
sulphide (H&lt;sub&gt;2&lt;/sub&gt;S), hydrogen chloride (HCl) and hydrogen fluoride (HF)
concentrations in the volcanic plumes (typically several minutes to a few
hours old) were repeatedly determined at distances from the summit vents
ranging from 0.1 to ~10 km, and under different environmental
conditions. At both volcanoes, acidic gas concentrations were found to
decrease exponentially with distance from the summit vents (e.g., SO&lt;sub&gt;2&lt;/sub&gt;
decreases from ~10 000 &amp;mu;g/m&lt;sup&gt;3&lt;/sup&gt;at 0.1 km from Etna&apos;s vents
down to ~7 &amp;mu;g/m&lt;sup&gt;3&lt;/sup&gt; at ~10 km distance),
reflecting the atmospheric dilution of the plume within the acid gas-free
background troposphere. Conversely, SO&lt;sub&gt;2&lt;/sub&gt;/HCl, SO&lt;sub&gt;2&lt;/sub&gt;/HF, and
SO&lt;sub&gt;2&lt;/sub&gt;/H&lt;sub&gt;2&lt;/sub&gt;S ratios in the plume showed no systematic changes with
plume aging, and fit source compositions within analytical error. Assuming
that SO&lt;sub&gt;2&lt;/sub&gt; losses by reaction are small during short-range atmospheric
transport within quiescent (ash-free) volcanic plumes, our observations
suggest that, for these short transport distances, atmospheric reactions for
H&lt;sub&gt;2&lt;/sub&gt;S and halogens are also negligible. The one-dimensional model MISTRA
was used to simulate quantitatively the evolution of halogen and sulphur
compounds in the plume of Mt. Etna. Model predictions support the hypothesis
of minor HCl chemical processing during plume transport, at least in
cloud-free conditions. Larger variations in the modelled SO&lt;sub&gt;2&lt;/sub&gt;/HCl ratios
were predicted under cloudy conditions, due to heterogeneous chlorine
cycling in the aerosol phase. The modelled evolution of the
SO&lt;sub&gt;2&lt;/sub&gt;/H&lt;sub&gt;2&lt;/sub&gt;S ratios is found to be substantially dependent on whether
or not the interactions of H&lt;sub&gt;2&lt;/sub&gt;S with halogens are included in the model.
In the former case, H&lt;sub&gt;2&lt;/sub&gt;S is assumed to be oxidized in the atmosphere
mainly by OH, which results in minor chemical loss for H&lt;sub&gt;2&lt;/sub&gt;S during plume
aging and produces a fair match between modelled and measured
SO&lt;sub&gt;2&lt;/sub&gt;/H&lt;sub&gt;2&lt;/sub&gt;S ratios. In the latter case, fast oxidation of H&lt;sub&gt;2&lt;/sub&gt;S by
Cl leads to H&lt;sub&gt;2&lt;/sub&gt;S chemical lifetimes in the early plume of a few seconds,
and thus SO&lt;sub&gt;2&lt;/sub&gt; to H&lt;sub&gt;2&lt;/sub&gt;S ratios that increase sharply during plume
transport. This disagreement between modelled and observed plume
compositions suggests that more in-detail kinetic investigations are
required for a proper evaluation of H&lt;sub&gt;2&lt;/sub&gt;S chemical processing in volcanic
plumes.</p>
</abstract>
<counts><page-count count="10"/></counts>
</article-meta>
</front>
<body/>
<back>
<ref-list>
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