<?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:creator>Aaron J. Slowey</dc:creator>
  <dc:date>2010</dc:date>
  <dc:description>Mercury is a global contaminant of concern due to its transformation by microorganisms to form methylmercury, a toxic species that accumulates in biological tissues. The effect of dissolved organic matter (DOM) isolated from natural waters on reactions between mercury(II) (Hg) and sulfide (S(-II)) to form HgS&lt;sub&gt;(s)&lt;/sub&gt; nanoparticles across a range of Hg and S(-II) concentrations was investigated. Hg was equilibrated with DOM, after which S(-II) was added. Dissolved Hg (Hg&lt;sub&gt;aq&lt;/sub&gt;) was periodically quantified using ultracentrifugation and chemical analysis following the addition of S(-II). Particle size and identity were determined using dynamic light scattering and X-ray absorption spectroscopy. S(-II) reacts with Hg to form 20 to 200nm aggregates consisting of 1-2 nm HgS&lt;sub&gt;(s)&lt;/sub&gt; subunits that are more structurally disordered than metacinnabar in the presence of 2 x 10&lt;sup&gt;-9&lt;/sup&gt; to 8 x 10&lt;sup&gt;-6&lt;/sup&gt;M Hg and 10 (mg C)L&lt;sup&gt;-1&lt;/sup&gt; DOM. Some of the HgS(s) nanoparticle aggregates are subsequently dissolved by DOM and (re)precipitated by S(-II) over periods of hours to days. At least three fractions of Hg-DOM species were observed with respect to reactivity toward S(-II): 0.3 &amp;mu;mol reactive Hg per mmol C (60 percent), 0.1 &amp;mu;mol per mmol C (20 percent) that are kinetically hindered, and another 0.1 &amp;mu;mol Hg per mmol C (20 percent) that are inert to reaction with S(-II). Following an initial S(-II)-driven precipitation of HgS&lt;sub&gt;(s)&lt;/sub&gt;, HgS&lt;sub&gt;(s)&lt;/sub&gt; was dissolved by DOM or organic sulfur compounds. HgS&lt;sub&gt;(s)&lt;/sub&gt; formation during this second phase was counterintuitively favored by lower S(-II) concentrations, suggesting surface association of DOM moieties that are less capable of dissolving HgS&lt;sub&gt;(s)&lt;/sub&gt;. DOM partially inhibits HgS(s) formation and mediates reactions between Hg and S(-II) such that HgS&lt;sub&gt;(s)&lt;/sub&gt; is susceptible to dissolution. These findings indicate that Hg accessibility to microorganisms could be controlled by kinetic (intermediate) species in the presence of S(-II) and DOM, undermining the premise that equilibrium Hg species distributions should correlate to the extent or rate of Hg methylation in soils and sediments.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1016/j.gca.2010.05.012</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Elsevier</dc:publisher>
  <dc:title>Rate of formation and dissolution of mercury sulfide nanoparticles: The dual role of natural organic matter</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>