<?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>M. Haitzer</dc:contributor>
  <dc:contributor>J. N. Ryan</dc:contributor>
  <dc:contributor>K. Nagy</dc:contributor>
  <dc:contributor>George Aiken</dc:contributor>
  <dc:contributor>Boutron C.Ferrari C.</dc:contributor>
  <dc:creator>G. Aiken</dc:creator>
  <dc:date>2003</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;Experiments were conducted using organic matter isolated from various surface waters in the Florida Everglades to study the interactions between dissolved organic matter (DOM) and Hg (II). Conditional distribution coefficients (&amp;nbsp;&lt;/span&gt;&lt;img src="https://jp4.journaldephysique.org/articles/jp4/abs/2003/05/jp4pr5p029/img1.gif" border="0" alt="$K_{DOM^\prime}$" width="49" height="26" align="MIDDLE" data-mce-src="https://jp4.journaldephysique.org/articles/jp4/abs/2003/05/jp4pr5p029/img1.gif"&gt;&lt;span&gt;), obtained using an equilibriurn dialysis ligand exchange method, were strongly affected by the Hg/DOM concentration ratio. Very strong interactions (&amp;nbsp;&lt;/span&gt;&lt;img src="https://jp4.journaldephysique.org/articles/jp4/abs/2003/05/jp4pr5p029/img2.gif" border="0" alt="$K_{{\rm DOM}^\prime}$" width="46" height="26" align="MIDDLE" data-mce-src="https://jp4.journaldephysique.org/articles/jp4/abs/2003/05/jp4pr5p029/img2.gif"&gt;&lt;span&gt;&amp;nbsp;= 10&amp;nbsp;&lt;/span&gt;&lt;img src="https://jp4.journaldephysique.org/articles/jp4/abs/2003/05/jp4pr5p029/img3.gif" border="0" alt="$^{23.2 \pm 05}$" width="43" height="15" align="BOTTOM" data-mce-src="https://jp4.journaldephysique.org/articles/jp4/abs/2003/05/jp4pr5p029/img3.gif"&gt;&lt;span&gt;&amp;nbsp;L kg&amp;nbsp;&lt;/span&gt;&lt;sup&gt;-1&lt;/sup&gt;&lt;span&gt;), indicative of Hg-thiol bonds, were observed at Hg/DOM ratios below approximately 1&amp;nbsp;&lt;/span&gt;&lt;img src="https://jp4.journaldephysique.org/articles/jp4/abs/2003/05/jp4pr5p029/img4.gif" border="0" alt="$\mu$" width="11" height="25" align="MIDDLE" data-mce-src="https://jp4.journaldephysique.org/articles/jp4/abs/2003/05/jp4pr5p029/img4.gif"&gt;&lt;span&gt;g Hg per mg DOM. Above approximately 10&amp;nbsp;&lt;/span&gt;&lt;img src="https://jp4.journaldephysique.org/articles/jp4/abs/2003/05/jp4pr5p029/img4.gif" border="0" alt="$\mu$" width="11" height="25" align="MIDDLE" data-mce-src="https://jp4.journaldephysique.org/articles/jp4/abs/2003/05/jp4pr5p029/img4.gif"&gt;&lt;span&gt;g Hg per mg DOM much lower&amp;nbsp;&lt;/span&gt;&lt;img src="https://jp4.journaldephysique.org/articles/jp4/abs/2003/05/jp4pr5p029/img2.gif" border="0" alt="$K_{{\rm DOM}^\prime}$" width="46" height="26" align="MIDDLE" data-mce-src="https://jp4.journaldephysique.org/articles/jp4/abs/2003/05/jp4pr5p029/img2.gif"&gt;&lt;span&gt;&amp;nbsp;values (&amp;nbsp;&lt;/span&gt;&lt;img src="https://jp4.journaldephysique.org/articles/jp4/abs/2003/05/jp4pr5p029/img5.gif" border="0" alt="$10^{10.7\pm 05}$" width="57" height="14" align="BOTTOM" data-mce-src="https://jp4.journaldephysique.org/articles/jp4/abs/2003/05/jp4pr5p029/img5.gif"&gt;&lt;span&gt;&amp;nbsp;L kg&amp;nbsp;&lt;/span&gt;&lt;sup&gt;-1&lt;/sup&gt;&lt;span&gt;) were obtained. DOM-Hg interactions were also studied by HgS (log K&amp;nbsp;&lt;/span&gt;&lt;img src="https://jp4.journaldephysique.org/articles/jp4/abs/2003/05/jp4pr5p029/img6.gif" border="0" alt="$_{\rm sp}=-52.4$" width="68" height="25" align="MIDDLE" data-mce-src="https://jp4.journaldephysique.org/articles/jp4/abs/2003/05/jp4pr5p029/img6.gif"&gt;&lt;span&gt;) dissolution and precipitation experiments. In the dissolution experiments, a significant amount of Hg was released from cinnabar in the presence of DOM, suggesting strong interactions. Conversely, precipitation of HgS was strongly inhibited in the presence of low concentrations (&amp;nbsp;&lt;/span&gt;&lt;img src="https://jp4.journaldephysique.org/articles/jp4/abs/2003/05/jp4pr5p029/img7.gif" border="0" alt="$\leq$" width="14" height="25" align="MIDDLE" data-mce-src="https://jp4.journaldephysique.org/articles/jp4/abs/2003/05/jp4pr5p029/img7.gif"&gt;&lt;span&gt;3 mg C/L) of DOM. In both the dissolution and precipitation experiments, organic matter rich in aromatic moities was more reactive with HgS than less aromatic fractions and sulfur-containing model compounds. These results suggest that DOM can influence the geochemistry of inorganic complexes of Hg in the Everglades, especially HgS, by strong Hg-DOM binding and colloidal stabilization.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1051/jp4:20030235</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>ECO Sciences </dc:publisher>
  <dc:title>Interactions between dissolved organic matter and mercury in the Florida Everglades</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>