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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>Juliette N. Rooney-Varga</dc:contributor>
  <dc:contributor>Catherine V. Gaw</dc:contributor>
  <dc:contributor>Derek R. Lovley</dc:contributor>
  <dc:creator>Robert T. Anderson</dc:creator>
  <dc:date>1998</dc:date>
  <dc:description>&lt;div class="article_abstract"&gt;&lt;div class="container container_scaled-down"&gt;&lt;div class="row"&gt;&lt;div class="col-xs-12"&gt;&lt;div id="abstractBox" class="article_abstract-content hlFld-Abstract"&gt;&lt;p class="articleBody_abstractText"&gt;The potential for anaerobic benzene oxidation in the Fe(III)-reduction zone of petroleum-contaminated aquifers was evaluated. Sediments were incubated under strict anaerobic conditions without any amendments in order to simulate in situ conditions. [&lt;sup&gt;14&lt;/sup&gt;C]Benzene was not oxidized to&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;sup&gt;14&lt;/sup&gt;CO&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;at most sites examined, which is consistent with previous studies that have found that benzene tends to persist in unamended, anaerobic aquifer materials and/or long periods of time are required in order to adapt the microbial population for benzene degradation. However, at one site located in Bemidji, MN, [&lt;sup&gt;14&lt;/sup&gt;C]benzene was oxidized to&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;sup&gt;14&lt;/sup&gt;CO&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;in unamended sediments without an apparent lag, suggesting that benzene was anaerobically degraded in situ. Benzene was not significantly oxidized in sediments from nearby Fe(III)-reducing sites nor in sediments collected from an uncontaminated background site in the same aquifer. Culturing and 16S rRNA-based molecular studies of the Bemidji aquifer demonstrated that while all sites contained similar numbers of Fe(III)-reducing microorganisms closely related to&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;Geothrix fermentens&lt;/i&gt;, the site at which anaerobic benzene degradation was observed was greatly enriched with microorganisms in the family&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;Geobacteraceae&lt;/i&gt;. This study provides the first data consistent with in situ anaerobic oxidation of benzene to carbon dioxide in the Fe(III)-reducing zone of a petroleum-contaminated aquifer and suggests that comparative studies on the size of the&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;Geobacteraceae&lt;/i&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;community in petroleum-contaminated aquifers might aid in the location of zones in which benzene degradation coupled to Fe(III) reduction is taking place.&lt;/p&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1021/es9704949</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>American Chemical Society</dc:publisher>
  <dc:title>Anaerobic benzene oxidation in the Fe(III) reduction zone of petroleum-contaminated aquifers</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>