<?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>Christoph Kern</dc:contributor>
  <dc:contributor>Salvatore Inguaggiato</dc:contributor>
  <dc:creator>Fabio Vita</dc:creator>
  <dc:date>2014</dc:date>
  <dc:description>&lt;p&gt;&lt;span class="pb_abstract"&gt; Active long-path differential optical absorption spectroscopy (LP-DOAS) has been an effective tool for measuring atmospheric trace gases for several decades. However, instruments were large, heavy and power-inefficient, making their application to remote environments extremely challenging. Recent developments in fibre-coupling telescope technology and the availability of ultraviolet light emitting diodes (UV-LEDS) have now allowed us to design and construct a lightweight, portable, low-power LP-DOAS instrument for use at remote locations and specifically for measuring degassing from active volcanic systems. The LP-DOAS was used to measure sulfur dioxide (SO&lt;sub&gt;2&lt;/sub&gt;) emissions from La Fossa crater, Vulcano, Italy, where column densities of up to 1.2 &amp;times; 10&lt;sup&gt;18&lt;/sup&gt; molec cm&lt;sup&gt;&amp;minus;2&lt;/sup&gt; (~ 500 ppmm) were detected along open paths of up to 400 m in total length. The instrument's SO&lt;sub&gt;2&lt;/sub&gt; detection limit was determined to be 2 &amp;times; 10&lt;sup&gt;16&lt;/sup&gt; molec cm&lt;sup&gt;&amp;minus;2&lt;/sup&gt; (~ 8 ppmm), thereby making quantitative detection of even trace amounts of SO&lt;sub&gt;2&lt;/sub&gt; possible. The instrument is capable of measuring other volcanic volatile species as well. Though the spectral evaluation of the recorded data showed that chlorine monoxide (ClO) and carbon disulfide (CS&lt;sub&gt;2&lt;/sub&gt;) were both below the instrument's detection limits during the experiment, the upper limits for the X / SO&lt;sub&gt;2&lt;/sub&gt; ratio (X = ClO, CS&lt;sub&gt;2&lt;/sub&gt;) could be derived, and yielded 2 &amp;times; 10&lt;sup&gt;&amp;minus;3&lt;/sup&gt; and 0.1, respectively. The robust design and versatility of the instrument make it a promising tool for monitoring of volcanic degassing and understanding processes in a range of volcanic systems.&lt;/span&gt;&lt;span class="pb_toc_link"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.5194/jsss-3-355-2014</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>AMA Verband für Sensorik und Messtechnik</dc:publisher>
  <dc:title>Development of a portable active long-path differential optical absorption spectroscopy system for volcanic gas measurements</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>