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dc.contributor.authorSmith, HGen
dc.contributor.authorBlake, WHen
dc.contributor.authorTaylor, Aen
dc.date.accessioned2017-01-05T10:54:28Z
dc.date.available2017-01-05T10:54:28Z
dc.date.issued2014-01-01en
dc.identifier.issn0197-9337en
dc.identifier.urihttp://hdl.handle.net/10026.1/8200
dc.description.abstract

© 2014 John Wiley & Sons, Ltd. Contemporary patterns in river basin sediment dynamics have been widely investigated but the timescales associated with current sediment delivery processes have received much less attention. Furthermore, no studies have quantified the effect of recent land use change on the residence or travel times of sediment transported through river basins. Such information is crucial for understanding contemporary river basin function and responses to natural and anthropogenic disturbances or management interventions. To address this need, we adopt a process-based modelling approach to quantify changes in spatial patterns and residence times of suspended sediment in response to recent agricultural land cover change. The sediment budget model SedNet was coupled with a mass balance model of particle residence times based on atmospheric and fluvial fluxes of three fallout radionuclide tracers (7Be, excess 210Pb and 137Cs). Mean annual fluxes of suspended sediment were simulated in seven river basins (38-920 km2) in south-west England for three land cover surveys (1990, 2000 and 2007). Suspended sediment flux increased across the basins from 0.5-15 to 1.4-37 kt y-1 in response to increasing arable land area between consecutive surveys. The residence time model divided basins into slow (upper surface soil) and rapid (river channel and connected hillslope sediment source area) transport compartments. Estimated theoretical residence times in the slow compartment decreased from 13-48 to 5.6-14 ky with the increase in basin sediment exports. In contrast, the short residence times for the rapid compartment increased from 185-256 to 260-368 d as the modelled connected source area expanded with increasing sediment supply from more arable land. The increase in sediment residence time was considered to correspond to longer sediment travel distances linked to larger connected source areas. This novel coupled modelling approach provides unique insight into river basin responses to recent environmental change not otherwise available from conventional measurement techniques.

en
dc.format.extent1944 - 1959en
dc.language.isoenen
dc.titleModelling particle residence times in agricultural river basins using a sediment budget model and fallout radionuclide tracersen
dc.typeJournal Article
plymouth.issue14en
plymouth.volume39en
plymouth.publication-statusPublisheden
plymouth.journalEarth Surface Processes and Landformsen
dc.identifier.doi10.1002/esp.3589en
plymouth.organisational-group/Plymouth
plymouth.organisational-group/Plymouth/00 Groups by role
plymouth.organisational-group/Plymouth/00 Groups by role/Academics
plymouth.organisational-group/Plymouth/00 Groups by role/Professional Services staff
plymouth.organisational-group/Plymouth/Faculty of Science and Engineering
plymouth.organisational-group/Plymouth/Faculty of Science and Engineering/School of Geography, Earth and Environmental Sciences
plymouth.organisational-group/Plymouth/REF 2021 Researchers by UoA
plymouth.organisational-group/Plymouth/REF 2021 Researchers by UoA/UoA14 Geography and Environmental Studies
plymouth.organisational-group/Plymouth/Research Groups
plymouth.organisational-group/Plymouth/Research Groups/Centre for Research in Environment and Society (CeRES)
plymouth.organisational-group/Plymouth/Research Groups/Marine Institute
dc.identifier.eissn1096-9837en
dc.rights.embargoperiodNot knownen
rioxxterms.versionofrecord10.1002/esp.3589en
rioxxterms.licenseref.urihttp://www.rioxx.net/licenses/all-rights-reserveden
rioxxterms.typeJournal Article/Reviewen
plymouth.oa-locationhttp://onlinelibrary.wiley.com/doi/10.1002/esp.3589/abstracten


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