Channel adjustment of a gravel-bed stream under episodic sediment supply regimes

Sediment supply is a key control on sediment transport rates and bed evolution in a stream. This study examined the adjustment of a gravel-bed stream under episodic sediment supply regimes by conducting a flume experiment in the Mountain Channel Hydraulic Experimental Laboratory at the University of...

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Main Author: Elgueta, Maria Alejandra
Language:English
Published: University of British Columbia 2014
Online Access:http://hdl.handle.net/2429/45882
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spelling ndltd-LACETR-oai-collectionscanada.gc.ca-BVAU.2429-458822014-03-26T03:40:05Z Channel adjustment of a gravel-bed stream under episodic sediment supply regimes Elgueta, Maria Alejandra Sediment supply is a key control on sediment transport rates and bed evolution in a stream. This study examined the adjustment of a gravel-bed stream under episodic sediment supply regimes by conducting a flume experiment in the Mountain Channel Hydraulic Experimental Laboratory at the University of British Columbia. The experiment consisted of a sequence of runs with no feed, constant feed and episodic supply regimes; but constant water discharge and feed texture. The observations indicated that sediment transport rates, the texture of bedload and the bed surface, sediment storage, bed slope, and bed topography adjusted to changes in sediment supply. The relative mobility of sediment instead did not change significantly. Under constant feed, transport rates showed a slow and small increase. The texture of the surface was fluctuating, the same as of the bedload. Sediment storage was relatively large, and the bed slope presented small changes. If the same amount of sediment entered in one or few pulses, transport rates and the texture of the surface exhibited pronounced changes just after the pulse, and returned to conditions similar to previous the pulse after some time. The size of the pulses influenced the results, and larger pulses caused larger increases of transport rates and finer textures on the bed surface. Cumulative storage, bed slope and bed morphology adjusted to episodic supply; but did not return to the conditions before the pulse, revealing that the effects of sediment supply over the bed were cumulative and persisted under periods of no feed. During these periods, transport rates decreased, the bed texture coarsened, and there was little change in the bed slope. After few hours of no feed, transport rates were relatively low and changes in elevation were small. Our results suggested that episodic supply produced interesting patterns of channel adjustment (different from constant feed regimes) that depend on the size and frequency of the supply. 2014-01-27T16:20:33Z 2014-01-27T16:20:33Z 2014 2014-01-27 2014-05 Electronic Thesis or Dissertation http://hdl.handle.net/2429/45882 eng http://creativecommons.org/publicdomain/zero/1.0/ CC0 1.0 Universal University of British Columbia
collection NDLTD
language English
sources NDLTD
description Sediment supply is a key control on sediment transport rates and bed evolution in a stream. This study examined the adjustment of a gravel-bed stream under episodic sediment supply regimes by conducting a flume experiment in the Mountain Channel Hydraulic Experimental Laboratory at the University of British Columbia. The experiment consisted of a sequence of runs with no feed, constant feed and episodic supply regimes; but constant water discharge and feed texture. The observations indicated that sediment transport rates, the texture of bedload and the bed surface, sediment storage, bed slope, and bed topography adjusted to changes in sediment supply. The relative mobility of sediment instead did not change significantly. Under constant feed, transport rates showed a slow and small increase. The texture of the surface was fluctuating, the same as of the bedload. Sediment storage was relatively large, and the bed slope presented small changes. If the same amount of sediment entered in one or few pulses, transport rates and the texture of the surface exhibited pronounced changes just after the pulse, and returned to conditions similar to previous the pulse after some time. The size of the pulses influenced the results, and larger pulses caused larger increases of transport rates and finer textures on the bed surface. Cumulative storage, bed slope and bed morphology adjusted to episodic supply; but did not return to the conditions before the pulse, revealing that the effects of sediment supply over the bed were cumulative and persisted under periods of no feed. During these periods, transport rates decreased, the bed texture coarsened, and there was little change in the bed slope. After few hours of no feed, transport rates were relatively low and changes in elevation were small. Our results suggested that episodic supply produced interesting patterns of channel adjustment (different from constant feed regimes) that depend on the size and frequency of the supply.
author Elgueta, Maria Alejandra
spellingShingle Elgueta, Maria Alejandra
Channel adjustment of a gravel-bed stream under episodic sediment supply regimes
author_facet Elgueta, Maria Alejandra
author_sort Elgueta, Maria Alejandra
title Channel adjustment of a gravel-bed stream under episodic sediment supply regimes
title_short Channel adjustment of a gravel-bed stream under episodic sediment supply regimes
title_full Channel adjustment of a gravel-bed stream under episodic sediment supply regimes
title_fullStr Channel adjustment of a gravel-bed stream under episodic sediment supply regimes
title_full_unstemmed Channel adjustment of a gravel-bed stream under episodic sediment supply regimes
title_sort channel adjustment of a gravel-bed stream under episodic sediment supply regimes
publisher University of British Columbia
publishDate 2014
url http://hdl.handle.net/2429/45882
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