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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>J.K. Bohlke</dc:contributor>
  <dc:contributor>Neil C. Sturchio</dc:contributor>
  <dc:contributor>John A. Izbicki</dc:contributor>
  <dc:contributor>Nicholas F. Teague</dc:contributor>
  <dc:creator>Paul B. Hatzinger</dc:creator>
  <dc:date>2018</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;Perchlorate&amp;nbsp;(ClO&lt;/span&gt;&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;−&lt;/sup&gt;&lt;span&gt;) in groundwater can be from synthetic or natural sources. Natural sources include ClO&lt;/span&gt;&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;−&lt;/sup&gt;&lt;span&gt;&amp;nbsp;associated with historical application of imported natural nitrate fertilizer from the Atacama Desert of Chile, and indigenous ClO&lt;/span&gt;&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;−&lt;/sup&gt;&lt;span&gt;&amp;nbsp;that accumulates locally in arid regions from&amp;nbsp;atmospheric deposition. The Rialto-Colton groundwater subbasin, 80 km east of Los Angeles, California, includes two mapped ClO&lt;/span&gt;&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;−&lt;/sup&gt;&lt;span&gt;&amp;nbsp;plumes from known military/industrial sources. Larger areas downgradient from those plumes, and in the Chino subbasin to the southwest, also contain ClO&lt;/span&gt;&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;−&lt;/sup&gt;&lt;span&gt;. Perchlorate from wells was analyzed for&amp;nbsp;chlorine&amp;nbsp;and oxygen&amp;nbsp;stable isotope&amp;nbsp;ratios (δ&lt;/span&gt;&lt;sup&gt;37&lt;/sup&gt;&lt;span&gt;Cl, δ&lt;/span&gt;&lt;sup&gt;18&lt;/sup&gt;&lt;span&gt;O, Δ&lt;/span&gt;&lt;sup&gt;17&lt;/sup&gt;&lt;span&gt;O) and radioactive&amp;nbsp;chlorine-36(&lt;/span&gt;&lt;sup&gt;36&lt;/sup&gt;&lt;span&gt;Cl) isotopic abundance, along with other geochemical, isotopic, and hydrogeologic data. Isotopic data show that synthetic ClO&lt;/span&gt;&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;−&lt;/sup&gt;&lt;span&gt;&amp;nbsp;was the dominant source within the mapped plumes. Downgradient from the mapped plumes, and in the Chino subbasin, the dominant source of ClO&lt;/span&gt;&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;−&lt;/sup&gt;&lt;span&gt;&amp;nbsp;was related to past agricultural use of Chilean (Atacama) nitrate fertilizer. The&amp;nbsp;&lt;/span&gt;&lt;sup&gt;36&lt;/sup&gt;&lt;span&gt;Cl and δ&lt;/span&gt;&lt;sup&gt;18&lt;/sup&gt;&lt;span&gt;O data indicate that wells having predominantly synthetic or Atacama ClO&lt;/span&gt;&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;−&lt;/sup&gt;&lt;span&gt;&amp;nbsp;also contained small fractions of indigenous ClO&lt;/span&gt;&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;−&lt;/sup&gt;&lt;span&gt;. Little or no differences were observed in&amp;nbsp;isotopic composition&amp;nbsp;or ClO&lt;/span&gt;&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;−&lt;/sup&gt;&lt;span&gt;&amp;nbsp;source with depth in depth-dependent data from selected wells. Indigenous ClO&lt;/span&gt;&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;−&lt;/sup&gt;&lt;span&gt;&amp;nbsp;was most evident in upgradient wells having ClO&lt;/span&gt;&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;−&lt;/sup&gt;&lt;span&gt;&amp;nbsp;concentrations &amp;lt;1 μg/L, consistent with its occurrence as a background constituent throughout the region. Stable isotope ratios of chlorine and oxygen and&amp;nbsp;&lt;/span&gt;&lt;sup&gt;36&lt;/sup&gt;&lt;span&gt;Cl isotopic abundance data provided relatively unambiguous discrimination of synthetic and Atacama sources in most wells having ClO&lt;/span&gt;&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;−&lt;/sup&gt;&lt;span&gt;&amp;nbsp;concentrations greater than 1 μg/L.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1016/j.apgeochem.2018.08.020</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Elsevier</dc:publisher>
  <dc:title>Four-dimensional isotopic approach to identify perchlorate sources in groundwater: Application to the Rialto-Colton and Chino subbasins, southern California (USA)</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>