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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>Jens M. Turowski</dc:contributor>
  <dc:contributor>Matthew Winnick</dc:contributor>
  <dc:contributor>Mathieu Dellinger</dc:contributor>
  <dc:contributor>Patrick Schleppi</dc:contributor>
  <dc:contributor>Kenneth H. Williams</dc:contributor>
  <dc:contributor>Corey Lawrence</dc:contributor>
  <dc:contributor>Katharine Maher</dc:contributor>
  <dc:contributor>Martin West</dc:contributor>
  <dc:contributor>Amanda Hayton</dc:contributor>
  <dc:creator>Robert Hilton</dc:creator>
  <dc:date>2021</dc:date>
  <dc:description>&lt;div class="article-section__content en main"&gt;&lt;p&gt;Oxidative weathering of sedimentary rocks plays an important role in the global carbon cycle. Rhenium (Re) has been proposed as a tracer of rock organic carbon (OC&lt;sub&gt;petro&lt;/sub&gt;) oxidation. However, the sources of Re and its mobilization by hydrological processes remain poorly constrained. Here we examine dissolved Re as a function of water discharge, using samples collected from three alpine catchments that drain sedimentary rocks in Switzerland (Erlenbach, Vogelbach) and Colorado, USA (East River). The Swiss catchments reveal a higher Re flux in the catchment with higher erosion rates, but have similar [Re]/[Na&lt;sup&gt;+&lt;/sup&gt;] and [Re]/[SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2-&lt;/sup&gt;] ratios, which indicate a dominance of Re from OC&lt;sub&gt;petro&lt;/sub&gt;. Despite differences in rock type and hydro-climatic setting, the three catchments have a positive correlation between river water [Re]/[Na&lt;sup&gt;+&lt;/sup&gt;] and [Re]/[SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2-&lt;/sup&gt;] and water discharge. We propose that this reflects preferential routing of Re from a near-surface, oxidative weathering zone. The observations support the use of Re as a proxy to trace rock-organic carbon oxidation, and suggest it may be a hydrological tracer of vadose zone processes. We apply the Re proxy, and estimate CO&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;release by OC&lt;sub&gt;petro&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;oxidation of 5.7&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;sup&gt;+6.6&lt;/sup&gt;/&lt;sub&gt;-2.0&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;tC km&lt;sup&gt;-2&lt;/sup&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;yr&lt;sup&gt;-1&lt;/sup&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;for the Erlenbach. The overall weathering intensity was ∼40%, meaning that the corresponding export of un-weathered OC&lt;sub&gt;petro&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;in river sediments is large, and the findings call for more measurements of OC&lt;sub&gt;petro&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;oxidation in mountains and rivers as thet cross floodplains.&lt;/p&gt;&lt;/div&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1029/2021WR029844</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>American Geophysical Union</dc:publisher>
  <dc:title>Concentration-discharge relationships of dissolved rhenium in Alpine catchments reveal its use as a tracer of oxidative weathering</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>