Formation and erosion of sediment cover in an experimental bedrock-alluvial channel

Hodge, R., Hoey, T. , Maniatis, G. and Lepretre, E. (2016) Formation and erosion of sediment cover in an experimental bedrock-alluvial channel. Earth Surface Processes and Landforms, 41(10), pp. 1409-1420. (doi: 10.1002/esp.3924)

116521.pdf - Accepted Version



Sediment grains in a bedrock-alluvial river will be deposited within or adjacent to a sediment patch, or as isolated grains on the bedrock surface. Previous analysis of grain geometry has demonstrated that these arrangements produce significant differences in grain entrainment shear stress. However, this analysis neglected potential interactions between the sediment patches, local hydraulics and grain entrainment. We present a series of flume experiments that measure the influence of sediment patches on grain entrainment. The flume had a planar bed with roughness that was much smaller than the diameters of the mobile grains. In each experiment sediment was added either as individual grains or as a single sediment pulse. Flow was then increased until the sediment was entrained. Analysis of the experiments demonstrates that: 1) for individual grains, coarse grains are entrained at a higher discharge than fine grains; 2) once sediment patches are present, the different in entrainment discharge between coarse and fine grains is greatly reduced; 3) the sheltering effect of patches also increases the entrainment discharge of isolated grains; 4) entire sediment patches break-up and are eroded quickly, rather than through progressive grain-by-grain erosion, and 5) as discharge increases there is some tendency for patches to become more elongate and flow-aligned, and more randomly distributed across the bed. One implication of this research is that the critical shear stress in bedrock-alluvial channels will be a function of the extent of the sediment cover. Another is that the influence of sediment patches equalises critical shear stresses between different grain sizes and grain locations, meaning that these factors may not need to be accounted for. Further research is needed to quantify interactions between sediment patches, grain entrainment and local hydraulics on rougher bedrock surfaces, and under different types of sediment supply.

Item Type:Articles
Keywords:bedrock river sediment transport bedforms
Glasgow Author(s) Enlighten ID:Hoey, Professor Trevor and Maniatis, Mr Georgios
Authors: Hodge, R., Hoey, T., Maniatis, G., and Lepretre, E.
Subjects:Q Science > QE Geology
College/School:College of Science and Engineering > School of Geographical and Earth Sciences
Journal Name:Earth Surface Processes and Landforms
Journal Abbr.:Earth Surf Proc Landf
Publisher:John Wiley and Sons
ISSN (Online):1096-9837
Published Online:24 February 2016
Copyright Holders:Copyright © 2016 John Wiley and Sons
First Published:First published in Earth Surface Processes and Landforms 41(10): 1409-1420
Publisher Policy:Reproduced in accordance with the copyright policy of the publisher.

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