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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