Sensitivity of interfacial hydraulics to the microtopographic roughness of water-lain gravels

Flow within the interfacial layer of gravel-bed rivers is poorly understood, but this zone is important because the hydraulics here transport sediment, generate flow structures and interact with benthic organisms. We hypothesized that different gravel-bed microtopographies generate measurable differ...

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Bibliographic Details
Main Authors: Stephen Rice, Thomas Buffin-Belanger, Ian Reid
Format: Default Article
Published: 2014
Subjects:
Geology not elsewhere classified
Other earth sciences not elsewhere classified
Interfacial layer
Gravel-bed roughness
Quadrant analysis
Coherent flow structure
Near-bed hydraulics
Sediment patch
Earth Sciences not elsewhere classified
Geology
Online Access:https://hdl.handle.net/2134/13030
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https://hdl.handle.net/2134/13030

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