<?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:creator>R. E. Stauffer</dc:creator>
  <dc:date>1977</dc:date>
  <dc:description>&lt;p&gt;A flame atomic absorption procedure utilizing an electrodeless discharge lamp is described for determining total solute antimony in silica-rich geothermal waters. Following NaNO&lt;sub&gt;2&lt;/sub&gt; oxidation of Sb&lt;sup&gt;+3&lt;/sup&gt;, SbCl&lt;sub&gt;5&lt;/sub&gt; is extracted from 6 &lt;i&gt;N&lt;/i&gt; HCl solution by using MIBK (methyl isobutyl ketone) ; silica in the organic layer is removed by centrifugation. The analytical detection limit for antimony is about 6 micrograms per liter in the original sample; the coefficient of variation is 4 percent at the 250 &lt;i&gt;&lt;span&gt;μ&lt;/span&gt;&lt;/i&gt;g/L Sb level. Comparable total antimony levels were found in sample splits which had been either filtered and acidified (to pH less than 1.5) with HNO&lt;sub&gt;3&lt;/sub&gt; or left untreated at the time of sample collection.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Measuring total antimony in geothermal waters by flame atomic absorption spectrometry</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>