Professor Rebecca Hodge rebecca.hodge@durham.ac.uk
Professor
A Froude-scaled model of a bedrock-alluvial channel reach: 2. Sediment cover
Hodge, R.A.; Hoey, T.B.
Authors
T.B. Hoey
Abstract
Previous research into sediment cover in bedrock-alluvial channels has focussed on total sediment cover, rather than the spatial distribution of cover within the channel. The latter is important because it determines the bedrock areas that are protected from erosion and the start and end of sediment transport pathways. We use a 1:10 Froude-scaled model of an 18 by 9 m reach of a bedrock-alluvial channel to study the production and erosion of sediment patches and hence the spatial relationships between flow, bed topography, and sediment dynamics. The hydraulic data from this bed are presented in the companion paper. In these experiments specified volumes of sediment were supplied at the upstream edge of the model reach as single inputs, at each of a range of discharges. This sediment formed patches, and once these stabilized, flow was steadily increased to erode the patches. In summary: (1) patches tend to initiate in the lowest areas of the bed, but areas of topographically induced high flow velocity can inhibit patch development; (2) at low sediment inputs the extent of sediment patches is determined by the bed topography and can be insensitive to the exact volume of sediment supplied; and (3) at higher sediment inputs more extensive patches are produced, stabilized by grain-grain and grain-flow interactions and less influenced by the bed topography. Bedrock topography can therefore be an important constraint on sediment patch dynamics, and topographic metrics are required that incorporate its within-reach variability. The magnitude and timing of sediment input events controls reach-scale sediment cover.
Citation
Hodge, R., & Hoey, T. (2016). A Froude-scaled model of a bedrock-alluvial channel reach: 2. Sediment cover. Journal of Geophysical Research: Earth Surface, 121(9), 1597-1618. https://doi.org/10.1002/2015jf003709
Journal Article Type | Article |
---|---|
Acceptance Date | Jul 23, 2016 |
Online Publication Date | Sep 16, 2016 |
Publication Date | Sep 16, 2016 |
Deposit Date | Aug 4, 2016 |
Publicly Available Date | Mar 16, 2017 |
Journal | Journal of Geophysical Research: Earth Surface |
Print ISSN | 2169-9011 |
Electronic ISSN | 2169-9011 |
Publisher | American Geophysical Union |
Peer Reviewed | Peer Reviewed |
Volume | 121 |
Issue | 9 |
Pages | 1597-1618 |
DOI | https://doi.org/10.1002/2015jf003709 |
Public URL | https://durham-repository.worktribe.com/output/1399703 |
Files
Published Journal Article
(4.9 Mb)
PDF
Published Journal Article (Advance online version)
(4.8 Mb)
PDF
Copyright Statement
Advance online version Hodge, R.A. & Hoey, T.B. (2016). A Froude-scaled model of a bedrock-alluvial channel reach: 2. Sediment cover. Journal of Geophysical Research: Earth Surface, 121(9): 1597-1618, doi: 10.1002/2015jf003709. To view the published open abstract, go to https://doi.org/ and enter the DOI.
You might also like
The Influence of In‐Channel Obstacles on River Sound
(2022)
Journal Article
Babbling brook to thunderous torrent: Using sound to monitor river stage
(2021)
Journal Article
Downloadable Citations
About Durham Research Online (DRO)
Administrator e-mail: dro.admin@durham.ac.uk
This application uses the following open-source libraries:
SheetJS Community Edition
Apache License Version 2.0 (http://www.apache.org/licenses/)
PDF.js
Apache License Version 2.0 (http://www.apache.org/licenses/)
Font Awesome
SIL OFL 1.1 (http://scripts.sil.org/OFL)
MIT License (http://opensource.org/licenses/mit-license.html)
CC BY 3.0 ( http://creativecommons.org/licenses/by/3.0/)
Powered by Worktribe © 2024
Advanced Search