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Scour holes and ripples occur below the hydraulic smooth to rough transition of movable beds

Kleinhans, Maarten G.; Leuven, Jasper R. F. W.; Braat, Lisanne; Baar, Anne

Authors

Maarten G. Kleinhans

Jasper R. F. W. Leuven

Lisanne Braat

Dr Anne Baar A.Baar@hull.ac.uk
Post-doctoral Research Associate



Contributors

Jaco Baas
Editor

Abstract

Scour holes often form in shallow flows over sand on the beach and in morphodynamic scale experiments of river reaches, deltas and estuarine landscapes. The scour holes are on average 2 cm deep and 5 cm long, regardless of the flow depth and appear to occur under similar conditions as current ripples: at low boundary Reynolds numbers, in fine sand and under relatively low sediment mobility. In landscape experiments, where the flow is only about 1 cm deep, such scours may be unrealistically large and have unnatural effects on channel formation, bar pattern and stratigraphy. This study tests the hypotheses that both scours and ripples occur in the same conditions and that the roughness added by sediment saltation explains the difference between the ripple–dune transition and the clear‐water hydraulic smooth to rough transition. About 500 experiments are presented with a range of sediment types, sediment mobility and obstructions to provoke scour holes, or removal thereof to assess scour hole persistence. Most experiments confirm that ripples and scour holes both form in the ripple stability field in two different bedform stability diagrams. The experiments also show that scours can be provoked by perturbations even below generalized sediment motion. Moreover, the hydraulic smooth to rough transition modified with saltation roughness depending on sediment mobility was similar in magnitude and in slope to ripple–dune transitions. Given uncertainties in saltation relations, the smooth to rough transitions modified for movable beds are empirically equivalent to the ripple–dune transitions. These results are in agreement with the hypothesis that scours form by turbulence caused by localized flow separation under low boundary Reynolds numbers, and do not form under generalized flow separation over coarser particles and intense sediment saltation. Furthermore, this suggests that ripples are a superposition of two independent forms: periodic bedforms occurring in smooth and rough conditions plus aperiodic scours occurring only in hydraulic smooth conditions.

Citation

Kleinhans, M. G., Leuven, J. R. F. W., Braat, L., & Baar, A. (2017). Scour holes and ripples occur below the hydraulic smooth to rough transition of movable beds. Sedimentology, 64(5), 1381-1401. https://doi.org/10.1111/sed.12358

Journal Article Type Article
Acceptance Date Jan 5, 2017
Online Publication Date Feb 27, 2017
Publication Date 2017-08
Deposit Date Dec 6, 2019
Publicly Available Date Nov 30, -0001
Journal Sedimentology
Print ISSN 0037-0746
Publisher Wiley
Peer Reviewed Peer Reviewed
Volume 64
Issue 5
Pages 1381-1401
DOI https://doi.org/10.1111/sed.12358
Keywords Bedform stability; Landscape experiments; Ripples; Scaling; Scour holes
Public URL https://hull-repository.worktribe.com/output/2851554
Publisher URL https://onlinelibrary.wiley.com/doi/full/10.1111/sed.12358

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Publisher Licence URL
https://creativecommons.org/licenses/by/4.0/

Copyright Statement
© 2017 The Authors





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