<?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:contributor>M. S. Schulz</dc:contributor>
  <dc:contributor>D.V. Vivit</dc:contributor>
  <dc:contributor>A.E. Blum</dc:contributor>
  <dc:contributor>David A. Stonestrom</dc:contributor>
  <dc:creator>A. F. White</dc:creator>
  <dc:date>2006</dc:date>
  <dc:description>&lt;div id="abstracts" class="Abstracts"&gt;&lt;div id="aep-abstract-id17" class="abstract author"&gt;&lt;div id="aep-abstract-sec-id18"&gt;&lt;p&gt;&lt;span&gt;Spatial and&amp;nbsp;temporal variations&amp;nbsp;in&amp;nbsp;pore water&amp;nbsp;compositions are characterized for a deep&amp;nbsp;regolith&amp;nbsp;profile developed on a&amp;nbsp;marine terrace&amp;nbsp;&lt;/span&gt;chronosequence&lt;span&gt;&amp;nbsp;near Santa Cruz California. Variations are resolved in terms of the dominance of either a lithogenic process, i.e.&amp;nbsp;chemical weathering, or a biogenic process, i.e. plant&amp;nbsp;nutrient cycling. The concept of elemental&amp;nbsp;fractionation&amp;nbsp;is introduced describing the extent that specific elements are mobilized and cycled as a result of these processes.&lt;/span&gt;&lt;/p&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1016/j.gexplo.2005.08.076</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Elsevier</dc:publisher>
  <dc:title>Controls on soil pore water solutes: An approach for distinguishing between biogenic and lithogenic processes</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>