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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>Tongwei Zhang</dc:contributor>
  <dc:contributor>Paul G. Kralert</dc:contributor>
  <dc:contributor>Yongchun Tang</dc:contributor>
  <dc:creator>Geoffrey S. Ellis</dc:creator>
  <dc:date>2019</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;Although sulfur-containing compounds are known to play a significant role in the diagenic and catagenic processes that generate oil and gas, relatively little is known about the kinetics of reactions between elemental S and petroleum hydrocarbons. To investigate this subject, a series of closed-system pyrolysis experiments using paraffin, a low-sulfur oil, and a high-sulfur oil with and without elemental S were conducted, and first-order chemical kinetics were fit to the experimental results. The average value for the activation energy required to reduce elemental S to H&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;S and to thermochemically alter higher molecular weight hydrocarbons to methane was calculated to be 193 kJ mol&lt;/span&gt;&lt;sup&gt;-1&lt;/sup&gt;&lt;span&gt;&amp;nbsp;(46 kcal mol&lt;/span&gt;&lt;sup&gt;-1&lt;/sup&gt;&lt;span&gt;). The results of this study demonstrate that under typical geologic conditions the rate of reduction of elemental S to H&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;S by petroleum hydrocarbons is quite rapid. The maximum time for substantial amounts of elemental S to persist in contact with petroleum hydrocarbons is estimated to be no more than a few million years in cool reservoirs (e.g., &amp;lt;80 °C), and in hotter reservoirs (e.g., &amp;gt;120 °C) the half-life of elemental S may be as short as hundreds of years. Additionally, the presence of elemental S substantially lowers the onset temperature of hydrocarbon thermal chemical alteration (TCA). The activation energy for TCA of a low-sulfur oil to generate methane is estimated to be lowered by 92 kJ mol&lt;/span&gt;&lt;sup&gt;-1&lt;/sup&gt;&lt;span&gt;&amp;nbsp;(22 kcal mol&lt;/span&gt;&lt;sup&gt;-1&lt;/sup&gt;&lt;span&gt;) due to the presence of elemental sulfur. Consequently, the presence of elemental S in petroleum reservoirs is expected to lower the thermal stability of oil and decrease the maximum depth at which oil occurs within a basin (thermal deadline). The observed acceleration of hydrocarbon TCA is possibly due to organic sulfur compounds (e.g., thiols and sulfides) that form through the reaction of H&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;S or polysulfides with hydrocarbons and subsequently thermally degrade leading to the formation of sulfur radicals that in turn enhance TCA reactions.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1016/j.gca.2019.02.023</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Elsevier</dc:publisher>
  <dc:title>Kinetics of elemental sulfur reduction by petroleum hydrocarbons and the implications for hydrocarbon thermal chemical alteration</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>