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Changes in ripple migration rates and hydraulic resistance with increasing mud-to-sand ratios

Changes in ripple migration rates and hydraulic resistance with increasing mud-to-sand ratios
Changes in ripple migration rates and hydraulic resistance with increasing mud-to-sand ratios
Coasts, estuaries, and lowland river environments are some of the most sensitive systems to climate-induced environmental change. In order to manage these systems, and adapt to future changes, we need to be able to predict how they might change. However, most available models have formulations based on assumptions that these systems are composed of only non-cohesive sands, even if mud is the most common sediment on Earth. Therefore, we need to find ways to incorporate the effect of sticky mud in predictors of flow resistance, sediment transport rates, and bedform geometries associated with form drag. In this paper, we show results from seven experiments conducted with different mud contents (0% - 12.6%) under the combined action of waves and currents. Experiments were conducted over a time period that was greater than the time needed for the bedform ripples to be at equilibrium with the imposed flow conditions. Our results reveal a mud content threshold above which friction coefficients are 4-6 times smaller than for clean sand and lower mud content counterparts. Below this threshold, flow resistance decreases with increasing mud content even though ripple migration rates are similar. Near the threshold, ripple migration rates increase as shorter ripples form and travel faster; the associated bedload transport rates also increase near the threshold and decrease beyond it. The threshold mud content, likely to vary with substrate composition and hydrodynamic conditions, is key to better estimating the behavior of different systems and needs further studies to properly incorporate it into predictors.
International Association for Hydro-Environment Engineering and Research
Fernandez, Roberto
65dcecb9-9a9f-4d12-8285-7b6842217cb4
Kassem, Hachem
658efa7a-a02c-4b29-9d07-5d57e95a4b51
Wu, Xuxu
688e0888-0b13-47f2-b222-cd5315834ed2
Parsons, Daniel
0c3761b8-053f-42b1-91c1-268f9eef1ae8
Fernandez, Roberto
65dcecb9-9a9f-4d12-8285-7b6842217cb4
Kassem, Hachem
658efa7a-a02c-4b29-9d07-5d57e95a4b51
Wu, Xuxu
688e0888-0b13-47f2-b222-cd5315834ed2
Parsons, Daniel
0c3761b8-053f-42b1-91c1-268f9eef1ae8

Fernandez, Roberto, Kassem, Hachem, Wu, Xuxu and Parsons, Daniel (2022) Changes in ripple migration rates and hydraulic resistance with increasing mud-to-sand ratios. In Proceedings of the 39th IAHR World Congress (Granada, 2022). International Association for Hydro-Environment Engineering and Research.. (doi:10.3850/IAHR-39WC2521711920221870).

Record type: Conference or Workshop Item (Paper)

Abstract

Coasts, estuaries, and lowland river environments are some of the most sensitive systems to climate-induced environmental change. In order to manage these systems, and adapt to future changes, we need to be able to predict how they might change. However, most available models have formulations based on assumptions that these systems are composed of only non-cohesive sands, even if mud is the most common sediment on Earth. Therefore, we need to find ways to incorporate the effect of sticky mud in predictors of flow resistance, sediment transport rates, and bedform geometries associated with form drag. In this paper, we show results from seven experiments conducted with different mud contents (0% - 12.6%) under the combined action of waves and currents. Experiments were conducted over a time period that was greater than the time needed for the bedform ripples to be at equilibrium with the imposed flow conditions. Our results reveal a mud content threshold above which friction coefficients are 4-6 times smaller than for clean sand and lower mud content counterparts. Below this threshold, flow resistance decreases with increasing mud content even though ripple migration rates are similar. Near the threshold, ripple migration rates increase as shorter ripples form and travel faster; the associated bedload transport rates also increase near the threshold and decrease beyond it. The threshold mud content, likely to vary with substrate composition and hydrodynamic conditions, is key to better estimating the behavior of different systems and needs further studies to properly incorporate it into predictors.

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Published date: 24 June 2022

Identifiers

Local EPrints ID: 478596
URI: http://eprints.soton.ac.uk/id/eprint/478596
PURE UUID: 2348bff6-f611-42c0-b43a-17d3439d54e1
ORCID for Hachem Kassem: ORCID iD orcid.org/0000-0002-5936-6037

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Date deposited: 05 Jul 2023 17:20
Last modified: 17 Mar 2024 03:33

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Contributors

Author: Roberto Fernandez
Author: Hachem Kassem ORCID iD
Author: Xuxu Wu
Author: Daniel Parsons

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