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dc.contributor.authorWard, Adam S.es_ES
dc.contributor.authorWondzell, Steven M.es_ES
dc.contributor.authorSchmadel, Noah M.es_ES
dc.contributor.authorHerzog, Skuyleres_ES
dc.contributor.authorZarnetske, Jay P.es_ES
dc.contributor.authorBaranov, Viktores_ES
dc.contributor.authorBlaen, Phillip J.es_ES
dc.contributor.authorBrekenfeld, Nicolaies_ES
dc.contributor.authorChu, Rosaliees_ES
dc.contributor.authorDerelle, Romaines_ES
dc.contributor.authorDrummond, Jennifer D.es_ES
dc.contributor.authorFleckenstein, Jan H.es_ES
dc.contributor.authorGarayburu-Caruso, Vanessaes_ES
dc.contributor.authorGraham, Emilyes_ES
dc.contributor.authorHannah, Davides_ES
dc.contributor.authorHarman, Ciaran J.es_ES
dc.contributor.authorHixson, Jasees_ES
dc.contributor.authorKnapp, Julia L.A.es_ES
dc.contributor.authorKrause, Stefanes_ES
dc.contributor.authorKurz, Marie J.es_ES
dc.contributor.authorLewandowski, Jörges_ES
dc.contributor.authorLi, Anganges_ES
dc.contributor.authorMartí, Eugèniaes_ES
dc.contributor.authorMiller, Melindaes_ES
dc.contributor.authorMilner, Alexander M.es_ES
dc.contributor.authorNeil, Kerryes_ES
dc.contributor.authorOrsini, Luisaes_ES
dc.contributor.authorPackman, Aaron I.es_ES
dc.contributor.authorPlont, Stephenes_ES
dc.contributor.authorRenteria, Lupitaes_ES
dc.contributor.authorRoche, Kevines_ES
dc.contributor.authorRoyer, Toddes_ES
dc.contributor.authorSegura, Catalinaes_ES
dc.contributor.authorStegen, Jameses_ES
dc.contributor.authorToyoda, Jasones_ES
dc.contributor.authorWells, Jacquelinees_ES
dc.contributor.authorWisnoski, Nathan I.es_ES
dc.date.accessioned2020-04-02T16:30:11Z-
dc.date.available2020-04-02T16:30:11Z-
dc.date.issued2019-
dc.identifier.citationHydrology and Earth System Sciences 23 : 5199–5225 (2019)es_ES
dc.identifier.issn1027-5606-
dc.identifier.urihttp://hdl.handle.net/10261/206343-
dc.descriptionEste artículo contiene 28 páginas, 6 figuras, 4 tablas.es_ES
dc.description.abstractAlthough most field and modeling studies of river corridor exchange have been conducted at scales ranging from tens to hundreds of meters, results of these studies are used to predict their ecological and hydrological influences at the scale of river networks. Further complicating prediction, exchanges are expected to vary with hydrologic forcing and the local geomorphic setting. While we desire predictive power, we lack a complete spatiotemporal relationship relating discharge to the variation in geologic setting and hydrologic forcing that is expected across a river basin. Indeed, the conceptual model of Wondzell (2011) predicts systematic variation in river corridor exchange as a function of (1) variation in baseflow over time at a fixed location, (2) variation in discharge with location in the river network, and (3) local geomorphic setting. To test this conceptual model we conducted more than 60 solute tracer studies including a synoptic campaign in the 5th-order river network of the H. J. Andrews Experimental Forest (Oregon, USA) and replicate-intime experiments in four watersheds. We interpret the data using a series of metrics describing river corridor exchange and solute transport, testing for consistent direction and magnitude of relationships relating these metrics to discharge and local geomorphic setting. We confirmed systematic decrease in river corridor exchange space through the river networks, from headwaters to the larger main stem. However, we did not find systematic variation with changes in discharge through time or with local geomorphic setting. While interpretation of our results is complicated by problems with the analytical methods, the results are sufficiently robust for us to conclude that space-for-time and time-for-space substitutions are not appropriate in our study system. Finally, we suggest two strategies that will improve the interpretability of tracer test results and help the hyporheic community develop robust datasets that will enable comparisons across multiple sites and/or discharge conditions.es_ES
dc.description.sponsorshipThis research has been supported by the Leverhulme Trust (Where rivers, groundwater and disciplines meet: a hyporheic research network), the UK Natural Environment Research Council (grant no. NE/L003872/1), the European Commission, H2020 Marie Skłodowska-Curie Actions (HiFreq (grant no. 734317)), the U.S. Department of Energy (Pacific Northwest National Lab and DE-SC0019377), the National Science Foundation (grant nos. DEB-1440409, EAR-1652293, EAR-1417603, and EAR-1446328), and the University of Birmingham (Institute of Advanced Studies).es_ES
dc.language.isoenges_ES
dc.publisherEuropean Geosciences Uniones_ES
dc.relation.isversionofPublisher's versiones_ES
dc.rightsopenAccesses_ES
dc.titleSpatial and temporal variation in river corridor exchange across a 5th-order mountain stream networkes_ES
dc.typeartículoes_ES
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.publisherversionhttp://doi.org/10.5194/hess-23-5199-2019es_ES
dc.identifier.e-issn1607-7938-
dc.relation.csices_ES
oprm.item.hasRevisionno ko 0 false*
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