<?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>Yaning Chen</dc:contributor>
  <dc:contributor>Yapeng Chen</dc:contributor>
  <dc:contributor>Jonathan M. Friedman</dc:contributor>
  <dc:contributor>Gonghuan Fan</dc:contributor>
  <dc:contributor>Jarre Heng A. Hati</dc:contributor>
  <dc:creator>Shubao Liu</dc:creator>
  <dc:date>2015</dc:date>
  <dc:description>&lt;p class="p1"&gt;&lt;span class="s1"&gt;Investigation of the water sources used by trees of different ages is essential to formulate a conservation strategy for the riparian tree, &lt;i&gt;P&lt;/i&gt;. &lt;i&gt;euphratica&lt;/i&gt;. This study addressed the contributions of different potential water sources to &lt;i&gt;P&lt;/i&gt;. &lt;i&gt;euphratica&lt;/i&gt; based on levels of stable oxygen and hydrogen isotopes (&amp;delta;&lt;/span&gt;&lt;span class="s2"&gt;18&lt;/span&gt;&lt;span class="s1"&gt;O, &amp;delta;&lt;/span&gt;&lt;span class="s2"&gt;2&lt;/span&gt;&lt;span class="s1"&gt;H) in the xylem of different aged &lt;i&gt;P&lt;/i&gt;. &lt;i&gt;euphratica&lt;/i&gt;, as well as in soil water and groundwater along the lower Heihe River. We found significant differences in &amp;delta;&lt;/span&gt;&lt;sup&gt;&lt;span class="s2"&gt;18&lt;/span&gt;&lt;/sup&gt;&lt;span class="s1"&gt;O values in the xylem of different aged &lt;i&gt;P&lt;/i&gt;. &lt;i&gt;euphratica&lt;/i&gt;. Specifically, the &amp;delta;&lt;/span&gt;&lt;sup&gt;&lt;span class="s2"&gt;18&lt;/span&gt;&lt;/sup&gt;&lt;span class="s1"&gt;O values of young, mature and over-mature forests were &amp;minus;5.368(&amp;plusmn;0.252)&amp;nbsp;&amp;permil;, &amp;minus;6.033(&amp;plusmn;&amp;nbsp;0.185)&amp;nbsp;&amp;permil; and &amp;minus;6.924&amp;nbsp;(&amp;plusmn;&amp;nbsp;0.166)&amp;nbsp;&amp;permil;, respectively, reflecting the reliance of older trees on deeper sources of water with a &amp;delta;&lt;/span&gt;&lt;sup&gt;&lt;span class="s2"&gt;18&lt;/span&gt;&lt;/sup&gt;&lt;span class="s1"&gt;O value closer to that of groundwater. Different aged &lt;i&gt;P&lt;/i&gt;. &lt;i&gt;euphratica&lt;/i&gt; used different water sources, with young forests rarely using groundwater (mean &amp;lt;15&amp;nbsp;%) and instead primarily relying on soil water from a depth of 0&amp;ndash;50&amp;nbsp;cm (mean &amp;gt;45&amp;nbsp;%), and mature and over-mature forests using water from deeper than 100&amp;nbsp;cm derived primarily from groundwater.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1007/s11284-015-1270-6</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Springer Japan</dc:publisher>
  <dc:title>Use of &lt;sup&gt;2&lt;/sup&gt;H and &lt;sup&gt;18&lt;/sup&gt;O stable isotopes to investigate water sources for different ages of &lt;i&gt;Populus euphratica&lt;/i&gt; along the lower Heihe River</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>