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<front>
<journal-meta>
<journal-id journal-id-type="publisher">BG</journal-id>
<journal-title-group>
<journal-title>Biogeosciences</journal-title>
<abbrev-journal-title abbrev-type="publisher">BG</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Biogeosciences</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1726-4189</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/bg-10-7323-2013</article-id>
<title-group>
<article-title>Solute-specific scaling of inorganic nitrogen and phosphorus uptake in streams</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hall Jr.</surname>
<given-names>R. O.</given-names>
<ext-link>https://orcid.org/0000-0002-0763-5346</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Baker</surname>
<given-names>M. A.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Rosi-Marshall</surname>
<given-names>E. J.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Tank</surname>
<given-names>J. L.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Newbold</surname>
<given-names>J. D.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of Zoology and Physiology, University of Wyoming, Laramie, Wyoming, 82071, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Biology and Ecology Center, Utah State University, Logan, Utah, 84322, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Cary Institute of Ecosystem Studies, Box AB, Millbrook, New York, 12545, USA</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Department of Biological Sciences, University of Notre Dame, Notre Dame, Indiana, 46556, USA</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Stroud Water Research Center, 970 Spencer Road, Avondale, Pennsylvania, 19311, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>15</day>
<month>11</month>
<year>2013</year>
</pub-date>
<volume>10</volume>
<issue>11</issue>
<fpage>7323</fpage>
<lpage>7331</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2013 R. O. Hall Jr. et al.</copyright-statement>
<copyright-year>2013</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://bg.copernicus.org/articles/10/7323/2013/bg-10-7323-2013.html">This article is available from https://bg.copernicus.org/articles/10/7323/2013/bg-10-7323-2013.html</self-uri>
<self-uri xlink:href="https://bg.copernicus.org/articles/10/7323/2013/bg-10-7323-2013.pdf">The full text article is available as a PDF file from https://bg.copernicus.org/articles/10/7323/2013/bg-10-7323-2013.pdf</self-uri>
<abstract>
<p>Stream ecosystem processes such as nutrient cycling may vary with stream
position in the network. Using a scaling approach, we examined the
relationship between stream size and nutrient uptake length, which represents
the mean distance that a dissolved solute travels prior to removal from the
water column. Ammonium (NH&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;+&lt;/sup&gt;) uptake length increased proportionally
with stream size measured as specific discharge (discharge/stream width) with
a scaling exponent = 1.01. In contrast, uptake lengths for nitrate
(NO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;&amp;minus;&lt;/sup&gt;) and soluble reactive phosphorus (SRP) increased more rapidly
than increases in specific discharge (scaling exponents = 1.19 for
NO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;&amp;minus;&lt;/sup&gt; and 1.35 for SRP). Additionally, the ratio of inorganic nitrogen
(N) uptake length to SRP uptake length declined with stream size; there was
relatively lower demand for SRP compared to N as stream size increased.
Finally, we related the scaling of uptake length with specific discharge to
that of stream length using Hack&apos;s law and downstream hydraulic geometry.
Ammonium uptake length increased less than proportionally with distance from
the headwaters, suggesting a strong role for larger streams and rivers in
regulating nutrient transport.</p>
</abstract>
<counts><page-count count="9"/></counts>
</article-meta>
</front>
<body/>
<back>
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