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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>Tyler B. Coplen</dc:contributor>
  <dc:contributor>Stanley J. Mroczkowski</dc:contributor>
  <dc:contributor>Willi A. Brand</dc:contributor>
  <dc:contributor>Lauren Brandes</dc:contributor>
  <dc:contributor>Heike Geilmann</dc:contributor>
  <dc:contributor>Arndt Schimmelmann</dc:contributor>
  <dc:creator>Haiping Qi</dc:creator>
  <dc:date>2016</dc:date>
  <dc:description>&lt;h3&gt;Rationale&lt;/h3&gt;&lt;p&gt;The widely used &lt;span class="smallCaps"&gt;l&lt;/span&gt;-glutamic acid isotopic reference material USGS41, enriched in both &lt;sup&gt;13&lt;/sup&gt;C and &lt;sup&gt;15&lt;/sup&gt;N, is nearly exhausted. A new material, USGS41a, has been prepared as a replacement for USGS41.&lt;/p&gt;&lt;h3&gt;Methods&lt;/h3&gt;&lt;p&gt;USGS41a was prepared by dissolving analytical grade &lt;span class="smallCaps"&gt;l&lt;/span&gt;-glutamic acid enriched in &lt;sup&gt;13&lt;/sup&gt;C and &lt;sup&gt;15&lt;/sup&gt;N together with &lt;span class="smallCaps"&gt;l&lt;/span&gt;-glutamic acid of normal isotopic composition. The &lt;i&gt;δ&lt;/i&gt;&lt;sup&gt;13&lt;/sup&gt;C and &lt;i&gt;δ&lt;/i&gt;&lt;sup&gt;15&lt;/sup&gt;N values of USGS41a were directly or indirectly normalized with the international reference materials NBS 19 calcium carbonate (&lt;i&gt;δ&lt;/i&gt;&lt;sup&gt;13&lt;/sup&gt;C&lt;sub&gt;VPDB&lt;/sub&gt; = +1.95 mUr, where milliurey = 0.001 = 1 ‰), LSVEC lithium carbonate (&lt;i&gt;δ&lt;/i&gt;&lt;sup&gt;13&lt;/sup&gt;C&lt;sub&gt;VPDB&lt;/sub&gt; = −46.6 mUr), and IAEA-N-1 ammonium sulfate (&lt;i&gt;δ&lt;/i&gt;&lt;sup&gt;15&lt;/sup&gt;N&lt;sub&gt;Air&lt;/sub&gt; = +0.43 mUr) and USGS32 potassium nitrate (&lt;i&gt;δ&lt;/i&gt;&lt;sup&gt;15&lt;/sup&gt;N = +180 mUr exactly) by on-line combustion, continuous-flow isotope-ratio mass spectrometry, and off-line dual-inlet isotope-ratio mass spectrometry.&lt;/p&gt;&lt;h3&gt;Results&lt;/h3&gt;&lt;p&gt;USGS41a is isotopically homogeneous; the reproducibility of &lt;i&gt;δ&lt;/i&gt;&lt;sup&gt;13&lt;/sup&gt;C and &lt;i&gt;δ&lt;/i&gt;&lt;sup&gt;15&lt;/sup&gt;N is better than 0.07 mUr and 0.09 mUr, respectively, in 200-μg amounts. It has a &lt;i&gt;δ&lt;/i&gt;&lt;sup&gt;13&lt;/sup&gt;C value of +36.55 mUr relative to VPDB and a &lt;i&gt;δ&lt;/i&gt;&lt;sup&gt;15&lt;/sup&gt;N value of +47.55 mUr relative to N&lt;sub&gt;2&lt;/sub&gt; in air. USGS41 was found to be hydroscopic, probably due to the presence of pyroglutamic acid. Experimental results indicate that the chemical purity of USGS41a is substantially better than that of USGS41.&lt;/p&gt;&lt;h3&gt;Conclusions&lt;/h3&gt;&lt;p&gt;The new isotopic reference material USGS41a can be used with USGS40 (having a &lt;i&gt;δ&lt;/i&gt;&lt;sup&gt;13&lt;/sup&gt;C&lt;sub&gt;VPDB&lt;/sub&gt; value of −26.39 mUr and a &lt;i&gt;δ&lt;/i&gt;&lt;sup&gt;15&lt;/sup&gt;N&lt;sub&gt;Air&lt;/sub&gt; value of −4.52 mUr) for (i) analyzing local laboratory isotopic reference materials, and (ii) quantifying drift with time, mass-dependent isotopic fractionation, and isotope-ratio-scale contraction for isotopic analysis of biological and organic materials. Published in 2016. This article is a U.S. Government work and is in the public domain in the USA.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1002/rcm.7510</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Wiley</dc:publisher>
  <dc:title>A new organic reference material, L-glutamic acid, USGS41a, for δ&lt;sup&gt;13&lt;/sup&gt;C and δ&lt;sup&gt;15&lt;/sup&gt;N measurements − a replacement for USGS41</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>