The importance of a small ephemeral tributary for fine sediment dynamics in a main‐stem river

dc.contributor.author
Marteau, Baptiste
dc.contributor.author
Batalla, Ramon J.
dc.contributor.author
Vericat Querol, Damià
dc.contributor.author
Gibbins, Chris N.
dc.date.accessioned
2024-12-05T22:37:01Z
dc.date.available
2024-12-05T22:37:01Z
dc.date.issued
2020-07-24T10:36:34Z
dc.date.issued
2020-07-24T10:36:34Z
dc.date.issued
2017-07-21
dc.identifier
https://doi.org/10.1002/rra.3177
dc.identifier
1535-1459
dc.identifier
http://hdl.handle.net/10459.1/69373
dc.identifier.uri
http://hdl.handle.net/10459.1/69373
dc.description.abstract
Studies of ephemeral streams have focused mainly in arid and semi‐arid regions. Such streams also occur widely in temperate regions, but much less is known about their influence on fluvial processes in main‐stem rivers here. In this paper, we present evidence of the importance of a small ephemeral temperate stream for main‐stem fine sediment dynamics. The paper focuses on a restoration project (River Ehen, North West England) which involved the reconnection of a headwater tributary to the main‐stem river. We present data on suspended sediment transport 2 years prior to and 2 years following the reconnection. Despite the small size and non‐perennial flow of the tributary, its reconnection resulted in an increase of 65% in the main‐stem sediment yield. During both the pre‐reconnection and post‐reconnection periods, a higher proportion of the annual yield was conveyed during short events with relatively high suspended sediment concentrations. Following the reconnection, the magnitude and frequency of such events increased, primarily due to sediment being delivered from the tributary at times when main‐stem flows were not elevated. Overall, the main‐stem remains supply limited and so is highly dependent on sediment delivered from the tributary. The study helps stress that even non‐perennial tributaries yielding only a small increase in catchment size (+1.2% in this case) can have a major influence on main‐stem fluvial dynamics. Their role as sediment sources may be especially important where, as in the case of the Ehen, the main‐stem is regulated and the system is otherwise starved of sediment.
dc.description.abstract
Damià Vericat is funded by a Ramon y Cajal Fellowship (RYC‐2010‐06264). Authors acknowledge the support from the Economy and Knowledge Department of the Catalan Government through the Consolidated Research Group “Fluvial Dynamics Research Group”—RIUS (2014 SGR 645), and the additional support provided by the CERCA Programme, also from the Catalan Government.
dc.language
eng
dc.publisher
John Wiley & Sons
dc.relation
Versió postprint del document publicat a: https://doi.org/10.1002/rra.3177
dc.relation
River Research and Applications, 2017, vol. 33, núm. 10, p. 1564-1574
dc.rights
(c) John Wiley & Sons, 2017
dc.rights
info:eu-repo/semantics/openAccess
dc.subject
Channel reconnection
dc.subject
Ephemeral stream
dc.subject
Regulated river
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River restoration
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Suspended fine sediment
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Temperate region
dc.title
The importance of a small ephemeral tributary for fine sediment dynamics in a main‐stem river
dc.type
info:eu-repo/semantics/article
dc.type
info:eu-repo/semantics/acceptedVersion


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