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<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>R. B. Wanty</dc:contributor>
  <dc:contributor>W.I. Ridley</dc:contributor>
  <dc:contributor>D.M. Borrok</dc:contributor>
  <dc:creator>M.J. Pribil</dc:creator>
  <dc:date>2010</dc:date>
  <dc:description>An increased interest in high precision Cu isotope ratio measurements using multi-collector inductively coupled plasma mass spectrometry (MC-ICP-MS) has developed recently for various natural geologic systems and environmental applications, these typically contain high concentrations of sulfur, particularly in the form of sulfate (SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2-&lt;/sup&gt;) and sulfide (S). For example, Cu, Fe, and Zn concentrations in acid mine drainage (AMD) can range from 100??g/L to greater than 50mg/L with sulfur species concentrations reaching greater than 1000mg/L. Routine separation of Cu, Fe and Zn from AMD, Cu-sulfide minerals and other geological matrices usually incorporates single anion exchange resin column chromatography for metal separation. During chromatographic separation, variable breakthrough of SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2-&lt;/sup&gt; during anion exchange resin column chromatography into the Cu fractions was observed as a function of the initial sulfur to Cu ratio, column properties, and the sample matrix. SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2-&lt;/sup&gt; present in the Cu fraction can form a polyatomic &lt;sup&gt;32&lt;/sup&gt;S-&lt;sup&gt;14&lt;/sup&gt;N-&lt;sup&gt;16&lt;/sup&gt;O-&lt;sup&gt;1&lt;/sup&gt;H species causing a direct mass interference with &lt;sup&gt;63&lt;/sup&gt;Cu and producing artificially light ??&lt;sup&gt;65&lt;/sup&gt;Cu values. Here we report the extent of the mass interference caused by SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2-&lt;/sup&gt; breakthrough when measuring ??&lt;sup&gt;65&lt;/sup&gt;Cu on natural samples and NIST SRM 976 Cu isotope spiked with SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2-&lt;/sup&gt; after both single anion column chromatography and double anion column chromatography. A set of five 100??g/L Cu SRM 976 samples spiked with 500mg/L SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2-&lt;/sup&gt; resulted in an average ??&lt;sup&gt;65&lt;/sup&gt;Cu of -3.50?????5.42??? following single anion column separation with variable SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2-&lt;/sup&gt; breakthrough but an average concentration of 770??g/L. Following double anion column separation, the average SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2-&lt;/sup&gt;concentration of 13??g/L resulted in better precision and accuracy for the measured ??&lt;sup&gt;65&lt;/sup&gt;Cu value of 0.01?????0.02??? relative to the expected 0??? for SRM 976. We conclude that attention to SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2-&lt;/sup&gt; breakthrough on sulfur-rich samples is necessary for accurate and precise measurements of ??&lt;sup&gt;65&lt;/sup&gt;Cu and may require the use of a double ion exchange column procedure. ?? 2010.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1016/j.chemgeo.2010.02.003</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>Influence of sulfur-bearing polyatomic species on high precision measurements of Cu isotopic composition</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>