Processes and effects of reversing currents on the erosion stability of wide-graded grain material

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  • University of Ottawa
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Original languageEnglish
Title of host publicationRiver Sedimentation
Subtitle of host publicationProceedings of the 13th International Symposium on River Sedimentation, ISRS 2016
EditorsSilke Wieprecht, Stefan Haun, Karolin Weber, Markus Noack, Kristina Terheiden
Pages402-410
Number of pages9
ISBN (electronic)9781138029453
Publication statusPublished - 2017
Event13th International Symposium on River Sedimentation, ISRS 2016 - Stuttgart, Germany
Duration: 19 Sept 201622 Sept 2016

Abstract

Physical model tests were carried out in a closed-circuit flume to investigate the overall erosion stability of wide-graded bed material in estuarine and coastal conditions by means of simulating tidal flow conditions with reversing currents. As a result of the reversing flow conditions, previously protected sediment eventually becomes exposed again, leading to bidirectional displacement processes in dependency of the flow direction. Furthermore, sediment fractions are slightly coarser under the following reversed flow than under the initial flow. This indicates higher critical shear stresses and thus erosion stability for the initial flow direction. In comparison to unidirectional current, this study finds a higher erosion stability for sediment fractions smaller than the median d50 diameter of the initial bed material under reversed current conditions.

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Cite this

Processes and effects of reversing currents on the erosion stability of wide-graded grain material. / Schendel, A.; Goseberg, N.; Schlurmann, T.
River Sedimentation: Proceedings of the 13th International Symposium on River Sedimentation, ISRS 2016. ed. / Silke Wieprecht; Stefan Haun; Karolin Weber; Markus Noack; Kristina Terheiden. 2017. p. 402-410.

Research output: Chapter in book/report/conference proceedingConference contributionResearchpeer review

Schendel, A, Goseberg, N & Schlurmann, T 2017, Processes and effects of reversing currents on the erosion stability of wide-graded grain material. in S Wieprecht, S Haun, K Weber, M Noack & K Terheiden (eds), River Sedimentation: Proceedings of the 13th International Symposium on River Sedimentation, ISRS 2016. pp. 402-410, 13th International Symposium on River Sedimentation, ISRS 2016, Stuttgart, Germany, 19 Sept 2016. <https://www.researchgate.net/profile/Alexander_Schendel/publication/308750270_Processes_and_Effects_of_Reversing_Currents_on_the_Erosion_Stability_of_Wide-graded_Grain_Material/links/5b114601a6fdcc4611da2b88/Processes-and-Effects-of-Reversing-Currents-on-the-Erosion-Stability-of-Wide-graded-Grain-Material.pdf>
Schendel A, Goseberg N, Schlurmann T. Processes and effects of reversing currents on the erosion stability of wide-graded grain material. In Wieprecht S, Haun S, Weber K, Noack M, Terheiden K, editors, River Sedimentation: Proceedings of the 13th International Symposium on River Sedimentation, ISRS 2016. 2017. p. 402-410
Schendel, A. ; Goseberg, N. ; Schlurmann, T. / Processes and effects of reversing currents on the erosion stability of wide-graded grain material. River Sedimentation: Proceedings of the 13th International Symposium on River Sedimentation, ISRS 2016. editor / Silke Wieprecht ; Stefan Haun ; Karolin Weber ; Markus Noack ; Kristina Terheiden. 2017. pp. 402-410
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abstract = "Physical model tests were carried out in a closed-circuit flume to investigate the overall erosion stability of wide-graded bed material in estuarine and coastal conditions by means of simulating tidal flow conditions with reversing currents. As a result of the reversing flow conditions, previously protected sediment eventually becomes exposed again, leading to bidirectional displacement processes in dependency of the flow direction. Furthermore, sediment fractions are slightly coarser under the following reversed flow than under the initial flow. This indicates higher critical shear stresses and thus erosion stability for the initial flow direction. In comparison to unidirectional current, this study finds a higher erosion stability for sediment fractions smaller than the median d50 diameter of the initial bed material under reversed current conditions.",
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AU - Schlurmann, T.

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