Impact of flow variability and sediment characteristics on channel width evolution

Alluvial rivers are shaped by sequences of water flows excavating their channels. Observations show that besides the magnitude, also the frequency and duration of streamflow oscillations might be important for the river channel formation. In addition, the river morphology appears influenced also by...

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Main Authors: Vargas-Luna Andrés, Crosato Alessandra, Byishimo Protogene, Uijttewaal Wim
Format: Article
Language:English
Published: EDP Sciences 2018-01-01
Series:E3S Web of Conferences
Online Access:https://doi.org/10.1051/e3sconf/20184005044
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author Vargas-Luna Andrés
Crosato Alessandra
Byishimo Protogene
Uijttewaal Wim
author_facet Vargas-Luna Andrés
Crosato Alessandra
Byishimo Protogene
Uijttewaal Wim
author_sort Vargas-Luna Andrés
collection DOAJ
description Alluvial rivers are shaped by sequences of water flows excavating their channels. Observations show that besides the magnitude, also the frequency and duration of streamflow oscillations might be important for the river channel formation. In addition, the river morphology appears influenced also by both size and degree of uniformity of the sediment. Nevertheless, many morphodynamic studies still represent the flow regime with a single value of the discharge, often corresponding to the bankfull condition, and the sediment with its median grain size. This work investigates the effects of streamflow variability and sediment characteristics on channel width formation, analysing the evolution of experimental streams with different sediments and discharge hydrographs. Results show that the formative condition of the channel width is not the geometric bankfull flow but a rather frequent peak flow. Remarkably different channel configurations arise from different sediment characteristics in the laboratory, where sediment non-uniformity produces more stable banks.
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spelling doaj.art-c53b6a8b4b9c422daba39ec41317aa592022-12-21T22:22:25ZengEDP SciencesE3S Web of Conferences2267-12422018-01-01400504410.1051/e3sconf/20184005044e3sconf_riverflow2018_05044Impact of flow variability and sediment characteristics on channel width evolutionVargas-Luna AndrésCrosato AlessandraByishimo ProtogeneUijttewaal WimAlluvial rivers are shaped by sequences of water flows excavating their channels. Observations show that besides the magnitude, also the frequency and duration of streamflow oscillations might be important for the river channel formation. In addition, the river morphology appears influenced also by both size and degree of uniformity of the sediment. Nevertheless, many morphodynamic studies still represent the flow regime with a single value of the discharge, often corresponding to the bankfull condition, and the sediment with its median grain size. This work investigates the effects of streamflow variability and sediment characteristics on channel width formation, analysing the evolution of experimental streams with different sediments and discharge hydrographs. Results show that the formative condition of the channel width is not the geometric bankfull flow but a rather frequent peak flow. Remarkably different channel configurations arise from different sediment characteristics in the laboratory, where sediment non-uniformity produces more stable banks.https://doi.org/10.1051/e3sconf/20184005044
spellingShingle Vargas-Luna Andrés
Crosato Alessandra
Byishimo Protogene
Uijttewaal Wim
Impact of flow variability and sediment characteristics on channel width evolution
E3S Web of Conferences
title Impact of flow variability and sediment characteristics on channel width evolution
title_full Impact of flow variability and sediment characteristics on channel width evolution
title_fullStr Impact of flow variability and sediment characteristics on channel width evolution
title_full_unstemmed Impact of flow variability and sediment characteristics on channel width evolution
title_short Impact of flow variability and sediment characteristics on channel width evolution
title_sort impact of flow variability and sediment characteristics on channel width evolution
url https://doi.org/10.1051/e3sconf/20184005044
work_keys_str_mv AT vargaslunaandres impactofflowvariabilityandsedimentcharacteristicsonchannelwidthevolution
AT crosatoalessandra impactofflowvariabilityandsedimentcharacteristicsonchannelwidthevolution
AT byishimoprotogene impactofflowvariabilityandsedimentcharacteristicsonchannelwidthevolution
AT uijttewaalwim impactofflowvariabilityandsedimentcharacteristicsonchannelwidthevolution