Please use this identifier to cite or link to this item: http://bura.brunel.ac.uk/handle/2438/31425
Title: Coupled effect of river bed and wall roughness on flow resistance
Authors: Whitfield, D
Houseago, R
Hodge, R
Rice, S
Ferguson, R
Hardy, R
Yager, E
Johnson, J
Hoey, T
Hackney, C
Yamasaki, T
Issue Date: 18-Mar-2025
Publisher: Copernicus GmbH on behalf of the European Geosciences Union
Citation: Whitfield, D. et al. (2025) 'Coupled effect of river bed and wall roughness on flow resistance', EGU General Assembly 2025, Vienna, Austria, 27 April-2 May, Abstract EGU25-12560, pp. 1 - 1. doi: 10.5194/egusphere-egu25-12560.
Abstract: Understanding flow resistance in rivers with rough beds and banks is critical in predicting flow velocities and depths for a given discharge; this has important applications in improving estimates of sediment fluxes, flood risk, and the identification of hotspots of geomorphic adjustment in rivers. Previous flume experiments have identified the usefulness of topographically derived bed roughness metrics in evaluating the effect of roughness on flow resistance: (1) standard deviation and (2) skewness of bed elevation distributions, as well as (3) frontal area of in-channel obstacles (σz, γ and λfrespectively). In reality, flow resistance is also provided by channel wall roughness, for example, metre scale fluctuations in bank protrusion, riparian vegetation, or the presence of rough bedrock banks in upland reaches. Here, we extend our physical experiments to include sidewall roughness in addition to bed roughness, to quantify the combined influence of bed and bank roughness on flow hydraulics. Our experimental arrangement uses varying combinations of both bed and bank roughness, both at 1:10 scale. We used two different rough-bed configurations, which comprised a 3D mould of a bedrock riverbed (River Greta, UK), with added scaled boulders at 10% and 40% cover. For the banks we added vertical battens running at regular spacing down the length of the flume walls. Seven sidewall configurations were used (as well as a smooth-walled configuration), with battens varying in protrusion and spacing, to achieve configurations with different combinations of sidewall versus bed roughness. Depth-averaged roughness metrics, ⟨σz⟩, ⟨γ⟩ and ⟨λf⟩ describe the combined roughness of the wetted channel. For each configuration, average water depths were measured for five discharges. Water depths were used to evaluate the Darcy-Weisbach friction factor, f, for each experimental run. We present initial results for the rough-wall experiments, evaluating the combined influence of bed and bank roughness on bulk flow resistance, as well as the relative influences of bed versus bank roughness in each configuration.
Description: Meeting abstract presented at EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, Session GM10.1, Fluvial systems: dynamics and interactions across scales. Convener: Eliisa Lotsari | Co-conveners: Joshua Ahmed, László Bertalan, Sumit Das. Orals | Thu, 01 May, 08:30–10:15 (CEST), 14:00–18:00 (CEST). Posters on site | Attendance Wed, 30 Apr, 10:45–12:30 (CEST) | Display Wed, 30 Apr, 08:30–12:30 (CEST).
URI: https://bura.brunel.ac.uk/handle/2438/31425
DOI: https://doi.org/10.5194/egusphere-egu25-12560
Other Identifiers: ORCiD: David Whitfield https://orcid.org/0000-0003-2340-1045
ORCiD: Robert Houseago https://orcid.org/0000-0001-7646-6489
ORCiD: Rebecca Hodge https://orcid.org/0000-0002-8792-8949
ORCiD: Trevor B. Hoey https://orcid.org/0000-0003-0734-6218
ORCiD: Christopher Hackney https://orcid.org/0000-0001-5390-9136
Abstract EGU25-12560
Appears in Collections:Dept of Civil and Environmental Engineering Research Papers

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