<?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:contributor>Chris Torres</dc:contributor>
  <dc:contributor>Lucia Rodriguez-Freire</dc:contributor>
  <dc:contributor>Johanna M. Blake</dc:contributor>
  <dc:contributor>Cherie L. De Vore</dc:contributor>
  <dc:contributor>Adrian J. Brearley</dc:contributor>
  <dc:contributor>Michael N. Spilde</dc:contributor>
  <dc:contributor>Stephen Cabaniss</dc:contributor>
  <dc:contributor>Abdul-Mehdi S. Ali</dc:contributor>
  <dc:contributor>Jose M. Cerrato</dc:contributor>
  <dc:creator>Eliane El Hayek</dc:creator>
  <dc:date>2018</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;We integrated field measurements, hydroponic experiments, microscopy, and spectroscopy to investigate the effect of Ca(II) on dissolved U(VI) uptake by plants in 1 mM HCO&lt;/span&gt;&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;–&lt;/sup&gt;&lt;span&gt;&amp;nbsp;solutions at circumneutral pH. The accumulation of U in plants (3.1–21.3 mg kg&lt;/span&gt;&lt;sup&gt;–1&lt;/sup&gt;&lt;span&gt;) from the stream bank of the Rio Paguate, Jackpile Mine, New Mexico served as a motivation for this study.&amp;nbsp;&lt;/span&gt;&lt;i&gt;Brassica juncea&lt;/i&gt;&lt;span&gt;was the model plant used for the laboratory experiments conducted over a range of U (30–700 μg L&lt;/span&gt;&lt;sup&gt;–1&lt;/sup&gt;&lt;span&gt;) and Ca (0–240 mg L&lt;/span&gt;&lt;sup&gt;–1&lt;/sup&gt;&lt;span&gt;) concentrations. The initial U uptake followed pseudo-second-order kinetics. The initial U uptake rate (&lt;/span&gt;&lt;i&gt;V&lt;/i&gt;&lt;sub&gt;0&lt;/sub&gt;&lt;span&gt;) ranged from 4.4 to 62 μg g&lt;/span&gt;&lt;sup&gt;–1&lt;/sup&gt;&lt;span&gt;&amp;nbsp;h&lt;/span&gt;&lt;sup&gt;–1&lt;/sup&gt;&lt;span&gt;&amp;nbsp;in experiments with no added Ca and from 0.73 to 2.07 μg g&lt;/span&gt;&lt;sup&gt;–1&lt;/sup&gt;&lt;span&gt;&amp;nbsp;h&lt;/span&gt;&lt;sup&gt;–1&lt;/sup&gt;&lt;span&gt;&amp;nbsp;in experiments with 12 mg L&lt;/span&gt;&lt;sup&gt;–1&lt;/sup&gt;&lt;span&gt;&amp;nbsp;Ca. No measurable U uptake over time was detected for experiments with 240 mg L&lt;/span&gt;&lt;sup&gt;–1&lt;/sup&gt;&lt;span&gt;&amp;nbsp;Ca. Ternary Ca–U–CO&lt;/span&gt;&lt;sub&gt;3&lt;/sub&gt;&lt;span&gt;complexes may affect the decrease in U bioavailability observed in this study. Elemental X-ray mapping using scanning transmission electron microscopy–energy-dispersive spectrometry detected U–P-bearing precipitates within root cell walls in water free of Ca. These results suggest that root interactions with Ca and carbonate in solution affect the bioavailability of U in plants. This study contributes relevant information to applications related to U transport and remediation of contaminated sites.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1021/acs.est.8b02724</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>ACS</dc:publisher>
  <dc:title>Effect of calcium on the bioavailability of dissolved uranium(VI) in plant roots under circumneutral pH</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>