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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>Allison R. Trcka</dc:contributor>
  <dc:contributor>Nick Krohe</dc:contributor>
  <dc:contributor>Genene Lehotsky</dc:contributor>
  <dc:creator>Kerri C. Treinen</dc:creator>
  <dc:date>2024</dc:date>
  <dc:description>&lt;p&gt;Between the 1950s and 1980s, wastewater generated at the Idaho National Laboratory contained Iodine-129 (&lt;sup&gt;129&lt;/sup&gt;I); this wastewater was discharged directly into the eastern Snake River Plain (ESRP) aquifer through a deep disposal well, unlined infiltration ponds, or leaked from distribution systems below industrial facilities. During 2021–22, the U.S. Geological Survey, in cooperation with the U.S. Department of Energy and the Idaho Department of Environmental Quality Idaho National Laboratory Oversight Program, collected groundwater samples from 64 monitoring wells in the ESRP aquifer, 6 of which are part of a multilevel monitoring system, to determine the concentration of &lt;sup&gt;129&lt;/sup&gt;I in the groundwater. These samples were analyzed by accelerator mass spectrometry as part of a long-term ongoing study to track trends and occurrences of this carcinogenic, long-lived radionuclide in the environment. Concentrations ranged from slightly above the locally determined background concentration of 5.4×10&lt;sup&gt;−6&lt;/sup&gt; picocuries per liter, to just below the U.S. Environmental Protection Agency’s maximum contaminant level of 1 picocurie per liter. Discharge of wastewater containing &lt;sup&gt;129&lt;/sup&gt;I has been discontinued to the aquifer, and long-term trends from a subset (n=15) of sampled wells show decreasing &lt;sup&gt;129&lt;/sup&gt;I concentrations over the last three decades. Concentrations of &lt;sup&gt;129&lt;/sup&gt;I in groundwater from monitoring wells near facilities at the Idaho National Laboratory are affected by episodic recharge from an ephemeral surface-water source and by the fracture-flow dominated hydrologic regime in the ESRP aquifer. The spatially focused sampling effort has also identified a low-level &lt;sup&gt;129&lt;/sup&gt;I plume that affects long-term water quality near and downgradient from the Advanced Test Reactor Complex in the southwestern part of the facility that had not been clearly defined in previous sampling efforts, although the definition of the plume is somewhat limited by available data.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/sir20245124</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Iodine-129 in the eastern Snake River Plain aquifer at and near the Idaho National Laboratory, Idaho, 2021–22</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>