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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>Paul R. Bierman</dc:contributor>
  <dc:contributor>Lucas J. Reusser</dc:contributor>
  <dc:contributor>Milan J. Pavich</dc:contributor>
  <dc:creator>Joseph A. Graly</dc:creator>
  <dc:date>2010</dc:date>
  <dc:description>In order to assess current understanding of meteoric &lt;sup&gt;10&lt;/sup&gt;Be dynamics and distribution in terrestrial soils, we assembled a database of all published meteoric &lt;sup&gt;10&lt;/sup&gt;Be soil depth profiles, including 104 profiles from 27 studies in globally diverse locations, collectively containing 679 individual measurements. This allows for the systematic comparison of meteoric &lt;sup&gt;10&lt;/sup&gt;Be concentration to other soil characteristics and the comparison of profile depth distributions between geologic settings. Percent clay, &lt;sup&gt;9&lt;/sup&gt;Be, and dithionite-citrate extracted Al positively correlate to meteoric &lt;sup&gt;10&lt;/sup&gt;Be in more than half of the soils where they were measured, but the lack of significant correlation in other soils suggests that no one soil factor controls meteoric &lt;sup&gt;10&lt;/sup&gt;Be distribution with depth. Dithionite-citrate extracted Fe and cation exchange capacity are only weakly correlated to meteoric &lt;sup&gt;10&lt;/sup&gt;Be. Percent organic carbon and pH are not significantly related to meteoric &lt;sup&gt;10&lt;/sup&gt;Be concentration when all data are complied.The compilation shows that meteoric &lt;sup&gt;10&lt;/sup&gt;Be concentration is seldom uniform with depth in a soil profile. In young or rapidly eroding soils, maximum meteoric &lt;sup&gt;10&lt;/sup&gt;Be concentrations are typically found in the uppermost 20 cm. In older, more slowly eroding soils, the highest meteoric &lt;sup&gt;10&lt;/sup&gt;Be concentrations are found at depth, usually between 50 and 200 cm. We find that the highest measured meteoric &lt;sup&gt;10&lt;/sup&gt;Be concentration in a soil profile is an important metric, as both the value and the depth of the maximum meteoric 10Be concentration correlate with the total measured meteoric &lt;sup&gt;10&lt;/sup&gt;Be inventory of the soil profile.In order to refine the use of meteoric &lt;sup&gt;10&lt;/sup&gt;Be as an estimator of soil erosion rate, we compare near-surface meteoric &lt;sup&gt;10&lt;/sup&gt;Be concentrations to total meteoric 10Be soil inventories. These trends are used to calibrate models of meteoric &lt;sup&gt;10&lt;/sup&gt;Be loss by soil erosion. Erosion rates calculated using this method vary based on the assumed depth and timing of erosional events and on the reference data selected.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1016/j.gca.2010.08.036</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Elsevier</dc:publisher>
  <dc:title>Meteoric &lt;sup&gt;10&lt;/sup&gt;Be in soil profiles - A global meta-analysis</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>