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<front>
<journal-meta>
<journal-id journal-id-type="publisher">PIAHS</journal-id>
<journal-title-group>
<journal-title>Proceedings of the International Association of Hydrological Sciences</journal-title>
<abbrev-journal-title abbrev-type="publisher">PIAHS</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Proc. IAHS</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">2199-899X</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/piahs-367-185-2015</article-id>
<title-group>
<article-title>Bedload flux in southern Brazilian basalt scarp</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Merten</surname>
<given-names>G. H.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Minella</surname>
<given-names>J. P. G.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Visiting Research Professor, Department of Civil Engineering, University of Minnesota, Minnesota, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Soils, Federal University of Santa Maria, 97105-900, Santa Maria, Brazil</addr-line>
</aff>
<pub-date pub-type="epub">
<day>03</day>
<month>03</month>
<year>2015</year>
</pub-date>
<volume>367</volume>
<fpage>185</fpage>
<lpage>192</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2015 G. H. Merten</copyright-statement>
<copyright-year>2015</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://piahs.copernicus.org/articles/367/185/2015/piahs-367-185-2015.html">This article is available from https://piahs.copernicus.org/articles/367/185/2015/piahs-367-185-2015.html</self-uri>
<self-uri xlink:href="https://piahs.copernicus.org/articles/367/185/2015/piahs-367-185-2015.pdf">The full text article is available as a PDF file from https://piahs.copernicus.org/articles/367/185/2015/piahs-367-185-2015.pdf</self-uri>
<abstract>
<p>Frequently, to assess the life expectancy of Brazilian reservoirs, bedload flux has been estimated by using formulas (e.g. the Einstein equations) or by assuming that bedload represents a fixed percentage of the suspended load. This study was carried out to characterize the bedload flux on the basalt scarps of southern Brazil. The bedload was measured over the course of 12 stormflows. The results demonstrated that the bedload flux–streamflow relationship was adequately described by a potential mathematical function. Bedload flux selectively transported particles smaller than D&lt;sub&gt;50&lt;/sub&gt; surface and subsurface bedstream sediments. When considering the bedload flux–streamflow relationship, the flux ranged from a minimum of 0.24 g m&lt;sup&gt;&amp;minus;1&lt;/sup&gt; s&lt;sup&gt;&amp;minus;1&lt;/sup&gt; for a streamflow of 0.53 m&lt;sup&gt;3&lt;/sup&gt; s&lt;sup&gt;&amp;minus;1&lt;/sup&gt; to a maximum of 44 g m&lt;sup&gt;&amp;minus;1&lt;/sup&gt; s&lt;sup&gt;&amp;minus;1&lt;/sup&gt; for a streamflow of 1.3 m&lt;sup&gt;3&lt;/sup&gt; s&lt;sup&gt;&amp;minus;1&lt;/sup&gt;. The percentage of bedload/suspended load varied between &lt;1% up to 60%, and this variation was strongly associated with peak flow.</p>
</abstract>
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