Influence of lateral embayments on suspended sediment transport under unsteady flow conditions

Local widening in a channelized river is a common practice in restoration projects. The lateral embayments built for this purpose in the river banks are partially filled up by fine sediments. This allows the formation of aquatic habitats with hydraulic and morphologic diversity. However, the design...

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Main Authors: Juez Carmelo, Thalmann Matthias, Schleiss Anton J., Franca Mário J.
Format: Article
Language:English
Published: EDP Sciences 2018-01-01
Series:E3S Web of Conferences
Online Access:https://doi.org/10.1051/e3sconf/20184003017
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spelling doaj-70aa7c855e084705b376c2242ca8c2872021-04-02T14:40:16ZengEDP SciencesE3S Web of Conferences2267-12422018-01-01400301710.1051/e3sconf/20184003017e3sconf_riverflow2018_03017Influence of lateral embayments on suspended sediment transport under unsteady flow conditionsJuez CarmeloThalmann MatthiasSchleiss Anton J.Franca Mário J.Local widening in a channelized river is a common practice in restoration projects. The lateral embayments built for this purpose in the river banks are partially filled up by fine sediments. This allows the formation of aquatic habitats with hydraulic and morphologic diversity. However, the design of these lateral cavities may be compromised by the fluctuations in the water discharge. To address this problem, systematic experimental investigations have been carried out with five different fluctuating hydrograph scenarios. Water depth, sediment concentration and area covered by the settled sediments are analysed in each experiment. The process of sedimentation in the lateral embayments proved to be, in general, resilient to flow fluctuations. However, there were several differences observed during the high flow phase fluctuation phase depending on the geometric configuration of the embayments and the applied hydrograph: (i) a higher peak in discharge means that more sediments are resuspended and a complete remobilization of the in-cavity sediment deposits is possible. (ii) Long and short cavities are more resilient to high flow events than cavities with an intermediate length.https://doi.org/10.1051/e3sconf/20184003017
collection DOAJ
language English
format Article
sources DOAJ
author Juez Carmelo
Thalmann Matthias
Schleiss Anton J.
Franca Mário J.
spellingShingle Juez Carmelo
Thalmann Matthias
Schleiss Anton J.
Franca Mário J.
Influence of lateral embayments on suspended sediment transport under unsteady flow conditions
E3S Web of Conferences
author_facet Juez Carmelo
Thalmann Matthias
Schleiss Anton J.
Franca Mário J.
author_sort Juez Carmelo
title Influence of lateral embayments on suspended sediment transport under unsteady flow conditions
title_short Influence of lateral embayments on suspended sediment transport under unsteady flow conditions
title_full Influence of lateral embayments on suspended sediment transport under unsteady flow conditions
title_fullStr Influence of lateral embayments on suspended sediment transport under unsteady flow conditions
title_full_unstemmed Influence of lateral embayments on suspended sediment transport under unsteady flow conditions
title_sort influence of lateral embayments on suspended sediment transport under unsteady flow conditions
publisher EDP Sciences
series E3S Web of Conferences
issn 2267-1242
publishDate 2018-01-01
description Local widening in a channelized river is a common practice in restoration projects. The lateral embayments built for this purpose in the river banks are partially filled up by fine sediments. This allows the formation of aquatic habitats with hydraulic and morphologic diversity. However, the design of these lateral cavities may be compromised by the fluctuations in the water discharge. To address this problem, systematic experimental investigations have been carried out with five different fluctuating hydrograph scenarios. Water depth, sediment concentration and area covered by the settled sediments are analysed in each experiment. The process of sedimentation in the lateral embayments proved to be, in general, resilient to flow fluctuations. However, there were several differences observed during the high flow phase fluctuation phase depending on the geometric configuration of the embayments and the applied hydrograph: (i) a higher peak in discharge means that more sediments are resuspended and a complete remobilization of the in-cavity sediment deposits is possible. (ii) Long and short cavities are more resilient to high flow events than cavities with an intermediate length.
url https://doi.org/10.1051/e3sconf/20184003017
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AT thalmannmatthias influenceoflateralembaymentsonsuspendedsedimenttransportunderunsteadyflowconditions
AT schleissantonj influenceoflateralembaymentsonsuspendedsedimenttransportunderunsteadyflowconditions
AT francamarioj influenceoflateralembaymentsonsuspendedsedimenttransportunderunsteadyflowconditions
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