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Data Associated with "Logjam Characteristics as Drivers of Transient Storage in Headwater Streams"

dc.contributor.authorMarshall, Anna
dc.contributor.authorZhang, Xiaolang
dc.contributor.authorSawyer, Audrey Hucks
dc.contributor.authorWohl, Ellen
dc.contributor.authorSingha, Kamini
dc.coverage.spatialEngineering Research Center Hydraulics Lab, Colorado State Universityen_US
dc.coverage.temporal2020-01-01, 2021-09-01en_US
dc.date.accessioned2022-07-15T21:55:50Z
dc.date.available2022-07-15T21:55:50Z
dc.date.issued2022
dc.descriptionThis repository contains data for the experimental flume and numerical model runs referenced in Marshall et al., 2022. Source code, data csv files for statistical analysis, and calculated temporal moments are included.en_US
dc.descriptionDepartment of Geosciences
dc.description.abstractLogjams in a stream create backwater conditions and locally force water to flow through the streambed, creating zones of transient storage within the surface and subsurface of a stream. We investigate the relative importance of logjam distribution density, logjam permeability, and discharge on transient storage in a simplified experimental channel. We use physical flume experiments in which we inject a salt tracer, monitor fluid conductivity breakthrough curves in surface water, and use breakthrough-curve skew to characterize transient storage. We then develop numerical models in HydroGeoSphere to reveal flow paths through the subsurface (or hyporheic zone) that contribute to some of the longest transient-storage timescales. In both the flume and numerical model, we observe an increase in backwater and hyporheic exchange at logjams. Observed complexities in transient storage behavior may depend largely on surface water flow in the backwater zone. As expected, multiple successive logjams provide more pervasive hyporheic exchange by distributing the head drop at each jam, leading to distributed but shallow flow paths. Decreasing the permeability of a logjam or increasing the discharge both facilitate more surface water storage and elevate the surface water level upstream of a logjam, thus increasing hyporheic exchange. Multiple logjams with low permeability result in the greatest magnitude of transient storage, suggesting that this configuration maximizes solute retention in backwater zones, while hyporheic exchange rates also increase. Understanding how logjam characteristics affect solute transport through both the channel and hyporheic zone has important management implications for rivers in forested, or historically forested, environments.en_US
dc.description.sponsorshipThis research was supported by National Science Foundation Hydrologic Sciences (award 1819068).en_US
dc.format.mediumPDF
dc.format.mediumCSV
dc.format.mediumMATLAB
dc.identifier.urihttps://hdl.handle.net/10217/235436
dc.identifier.urihttp://dx.doi.org/10.25675/10217/235436
dc.languageEnglishen_US
dc.language.isoengen_US
dc.publisherColorado State University. Librariesen_US
dc.relation.ispartofResearch Data
dc.relation.isreferencedbyMarshall, A., Zhang, X., Sawyer, A. H., Wohl, E., & Singha, K. (2023). Logjam characteristics as drivers of transient storage in headwater streams. Water Resources Research, 59, e2022WR033139. https://doi.org/10.1029/2022WR033139en_US
dc.rights.licenseThe material is open access and distributed under the terms and conditions of the Creative Commons Public Domain "No rights reserved" (https://creativecommons.org/share-your-work/public-domain/cc0/).
dc.rights.urihttps://creativecommons.org/share-your-work/public-domain/cc0/
dc.subjectfluvial geomorphologyen_US
dc.subjectlogjamsen_US
dc.subjectlarge wooden_US
dc.subjecttransient storageen_US
dc.subjecthyporheic exchangeen_US
dc.titleData Associated with "Logjam Characteristics as Drivers of Transient Storage in Headwater Streams"en_US
dc.typeDataseten_US

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