<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>David Damby</dc:contributor>
  <dc:contributor>Claire J. Horwell</dc:contributor>
  <dc:contributor>Paul M Ayris</dc:contributor>
  <dc:contributor>Pierre Delmelle</dc:contributor>
  <dc:contributor>Christopher J Ottley</dc:contributor>
  <dc:contributor>Pablo Cubillas</dc:contributor>
  <dc:contributor>Ana S Casas</dc:contributor>
  <dc:contributor>Christoph Bisig</dc:contributor>
  <dc:contributor>Alke Petri-Fink</dc:contributor>
  <dc:contributor>Donald B. Dingwell</dc:contributor>
  <dc:contributor>Martin J D Clift</dc:contributor>
  <dc:contributor>Barbara Drasler</dc:contributor>
  <dc:contributor>Barbara Rothen-Rutishauser</dc:contributor>
  <dc:creator>Ines Tomasek</dc:creator>
  <dc:date>2019</dc:date>
  <dc:description>&lt;div id="abssec0010"&gt;&lt;h3 id="sectitle0015" class="u-h4 u-margin-m-top u-margin-xs-bottom"&gt;Background&lt;/h3&gt;&lt;p id="abspara0010"&gt;&lt;span&gt;Volcanic plumes are complex environments composed of gases and ash particles, where chemical and physical processes occur at different temperature and compositional regimes. Commonly, soluble sulphate- and chloride-bearing salts are formed on ash as gases interact with ash surfaces. Exposure to respirable volcanic ash following an eruption is potentially a significant health concern. The impact of such gas-ash interactions on ash toxicity is wholly un-investigated. Here, we study, for the first time, whether the interaction of volcanic particles with&amp;nbsp;sulphur dioxide&amp;nbsp;(SO&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;) gas, and the resulting presence of&amp;nbsp;sulphate&amp;nbsp;salt deposits on particle surfaces, influences toxicity to the respiratory system, using an advanced&amp;nbsp;&lt;/span&gt;&lt;i&gt;in vitro&lt;/i&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;approach.&lt;/p&gt;&lt;/div&gt;&lt;div id="abssec0015"&gt;&lt;h3 id="sectitle0020" class="u-h4 u-margin-m-top u-margin-xs-bottom"&gt;Methods&lt;/h3&gt;&lt;p id="abspara0015"&gt;To emplace surface sulphate salts on particles,&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;via&lt;/i&gt;&lt;span&gt;&amp;nbsp;replication of the physicochemical reactions that occur between pristine ash surfaces and volcanic gas, analogue substrates (powdered synthetic&amp;nbsp;volcanic glass&amp;nbsp;and natural pumice) were exposed to SO&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;&amp;nbsp;at 500 °C, in a novel Advanced Gas-Ash Reactor, resulting in salt-laden particles. The solubility of surface salt deposits was then assessed by leaching in water and geochemical modelling. A human multicellular lung model was exposed to aerosolised salt-laden and pristine (salt-free) particles, and incubated for 24 h. Cell cultures were subsequently assessed for biological endpoints, including cytotoxicity (lactate&amp;nbsp;dehydrogenase&amp;nbsp;release),&amp;nbsp;oxidative stress&amp;nbsp;(oxidative stress-related gene expression; heme oxygenase 1 and NAD(P)H dehydrogenase [quinone] 1) and its (pro-)inflammatory response (tumour necrosis factor α,&amp;nbsp;interleukin&amp;nbsp;8 and interleukin 1β at gene and protein levels).&lt;/span&gt;&lt;/p&gt;&lt;/div&gt;&lt;div id="abssec0020"&gt;&lt;h3 id="sectitle0025" class="u-h4 u-margin-m-top u-margin-xs-bottom"&gt;Results&lt;/h3&gt;&lt;p id="abspara0020"&gt;In the lung cell model no significant effects were observed between the pristine and SO&lt;sub&gt;2&lt;/sub&gt;-exposed particles, indicating that the surface salt deposits, and the underlying alterations to the substrate, do not cause acute adverse effects&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;in vitro&lt;/i&gt;. Based on the leachate data, the majority of the sulphate salts from the ash surfaces are likely to dissolve in the lungs prior to cellular uptake.&lt;/p&gt;&lt;/div&gt;&lt;div id="abssec0025"&gt;&lt;h3 id="sectitle0030" class="u-h4 u-margin-m-top u-margin-xs-bottom"&gt;Conclusions&lt;/h3&gt;&lt;p id="abspara0025"&gt;The findings of this study indicate that interaction of volcanic ash with SO&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;during ash generation and transport does not significantly affect the respiratory toxicity of volcanic ash&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;in vitro&lt;/i&gt;. Therefore, sulphate salts are unlikely a dominant factor controlling variability in&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;in vitro&lt;/i&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;toxicity assessments observed during previous eruption response efforts.&lt;/p&gt;&lt;/div&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1016/j.envres.2019.108798</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Elsevier</dc:publisher>
  <dc:title>Assessment of the potential for in-plume sulphur dioxide gas-ash interactions to influence the respiratory toxicity of volcanic ash</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>