<?xml version="1.0"?>
<oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" 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:title>River mixing in the Amazon as a driver of concentration-discharge relationships</dc:title>
  <dc:creator>Bouchez, J.</dc:creator>
  <dc:creator>Moquet, J. S.</dc:creator>
  <dc:creator>Espinoza, J. C.</dc:creator>
  <dc:creator>/Martinez, Jean-Michel</dc:creator>
  <dc:creator>/Guyot, Jean-Loup</dc:creator>
  <dc:creator>/Lagane, Christelle</dc:creator>
  <dc:creator>Filizola, N.</dc:creator>
  <dc:creator>Noriega, L.</dc:creator>
  <dc:creator>Sanchez, L. H.</dc:creator>
  <dc:creator>Pombosa, R.</dc:creator>
  <dc:subject>concentration-discharge (C-Q) relationships</dc:subject>
  <dc:subject>Amazon River</dc:subject>
  <dc:subject>C-Q</dc:subject>
  <dc:subject>hysteresis loops</dc:subject>
  <dc:subject>tributary mixing</dc:subject>
  <dc:subject>spectral analysis</dc:subject>
  <dc:description>Large hydrological systems aggregate compositionally different waters derived from a variety of pathways. In the case of continental-scale rivers, such aggregation occurs noticeably at confluences between tributaries. Here we explore how such aggregation can affect solute concentration-discharge (C-Q) relationships and thus obscure the message carried by these relationships in terms of weathering properties of the Critical Zone. We build up a simple model for tributary mixing to predict the behavior of C-Q relationships during aggregation. We test a set of predictions made in the context of the largest world's river, the Amazon. In particular, we predict that the C-Q relationships of the rivers draining heterogeneous catchments should be the most "dilutional" and should display the widest hysteresis loops. To check these predictions, we compute 10 day-periodicity time series of Q and major solute (Si, Ca2+, Mg2+, K+, Na+, Cl-, SO42-) C and fluxes (F) for 13 gauging stations located throughout the Amazon basin. In agreement with the model predictions, C-Q relationships of most solutes shift from a fairly "chemostatic" behavior (nearly constant C) at the Andean mountain front and in pure lowland areas, to more "dilutional" patterns (negative C-Q relationship) toward the system mouth. More prominent C-Q hysteresis loops are also observed at the most downstream stations. Altogether, this study suggests that mixing of water and solutes between different flowpaths exerts a strong control on C-Q relationships of large-scale hydrological systems.</dc:description>
  <dc:date>2017</dc:date>
  <dc:type>text</dc:type>
  <dc:identifier>https://www.documentation.ird.fr/hor/fdi:010071962</dc:identifier>
  <dc:identifier>fdi:010071962</dc:identifier>
  <dc:identifier>Bouchez J., Moquet J. S., Espinoza J. C., Martinez Jean-Michel, Guyot Jean-Loup, Lagane Christelle, Filizola N., Noriega L., Sanchez L. H., Pombosa R.. River mixing in the Amazon as a driver of concentration-discharge relationships. 2017, 53 (11),  8660-8685</dc:identifier>
  <dc:language>EN</dc:language>
</oai_dc:dc>
