A flume experiment on the effect of constriction shape on the formation of forced pools

A series of 18 flume runs were conducted in a 6-m long, 0.5-m wide recirculating flume with a bed gradient of 0.8% to determine the influence of obstruction shape on the formation and characteristics of forced pools. Six different-shaped obstructions were added to the flume with the maximum width of...

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Main Authors: D. M. Thompson, C. R. McCarrick
Format: Article
Language:English
Published: Copernicus Publications 2010-07-01
Series:Hydrology and Earth System Sciences
Online Access:http://www.hydrol-earth-syst-sci.net/14/1321/2010/hess-14-1321-2010.pdf
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spelling doaj-9f86f418ba194fb381c4815226428a1c2020-11-24T22:59:01ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382010-07-011471321133010.5194/hess-14-1321-2010A flume experiment on the effect of constriction shape on the formation of forced poolsD. M. ThompsonC. R. McCarrickA series of 18 flume runs were conducted in a 6-m long, 0.5-m wide recirculating flume with a bed gradient of 0.8% to determine the influence of obstruction shape on the formation and characteristics of forced pools. Six different-shaped obstructions were added to the flume with the maximum width of the obstruction held constant at 20 cm, which equaled a 40% constriction of flow. The obstruction shapes used included a square, a rectangle, a right triangle with the hypotenuse-facing upstream, a right triangle with the hypotenuse-facing downstream, a combination of a square and triangle with the hypotenuse-facing upstream, and a rectangle and semi-circle shape. Three flume runs were conducted with each obstruction shape. A profile of the flume bed was taken after each experiment and a grid measurement of bed elevations for the last run were conducted to create topographic maps of the flume bed to compare pool-riffle morphologies. ANOVA results indicate pool depth, pool location, and the distance between the pool center and the riffle crest all vary with the obstruction shape. Obstructions with a more blunt upstream face created deeper pools, more total scour and longer pool-riffle sequence lengths than pools formed by obstructions with a more gradual narrowing of flow. The increased volume of scour associated with obstructions that rapidly narrow flow also creates larger volume riffles that cover a greater extent of the channel bed. http://www.hydrol-earth-syst-sci.net/14/1321/2010/hess-14-1321-2010.pdf
collection DOAJ
language English
format Article
sources DOAJ
author D. M. Thompson
C. R. McCarrick
spellingShingle D. M. Thompson
C. R. McCarrick
A flume experiment on the effect of constriction shape on the formation of forced pools
Hydrology and Earth System Sciences
author_facet D. M. Thompson
C. R. McCarrick
author_sort D. M. Thompson
title A flume experiment on the effect of constriction shape on the formation of forced pools
title_short A flume experiment on the effect of constriction shape on the formation of forced pools
title_full A flume experiment on the effect of constriction shape on the formation of forced pools
title_fullStr A flume experiment on the effect of constriction shape on the formation of forced pools
title_full_unstemmed A flume experiment on the effect of constriction shape on the formation of forced pools
title_sort flume experiment on the effect of constriction shape on the formation of forced pools
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2010-07-01
description A series of 18 flume runs were conducted in a 6-m long, 0.5-m wide recirculating flume with a bed gradient of 0.8% to determine the influence of obstruction shape on the formation and characteristics of forced pools. Six different-shaped obstructions were added to the flume with the maximum width of the obstruction held constant at 20 cm, which equaled a 40% constriction of flow. The obstruction shapes used included a square, a rectangle, a right triangle with the hypotenuse-facing upstream, a right triangle with the hypotenuse-facing downstream, a combination of a square and triangle with the hypotenuse-facing upstream, and a rectangle and semi-circle shape. Three flume runs were conducted with each obstruction shape. A profile of the flume bed was taken after each experiment and a grid measurement of bed elevations for the last run were conducted to create topographic maps of the flume bed to compare pool-riffle morphologies. ANOVA results indicate pool depth, pool location, and the distance between the pool center and the riffle crest all vary with the obstruction shape. Obstructions with a more blunt upstream face created deeper pools, more total scour and longer pool-riffle sequence lengths than pools formed by obstructions with a more gradual narrowing of flow. The increased volume of scour associated with obstructions that rapidly narrow flow also creates larger volume riffles that cover a greater extent of the channel bed.
url http://www.hydrol-earth-syst-sci.net/14/1321/2010/hess-14-1321-2010.pdf
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