Record Details
Field | Value |
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Title | Adjustment of the Bed Surface Size Distribution of Gravel-Bed Rivers in Response to Cycled Hydrograph |
Creator | Hassan, G. M. Wilcock, Peter |
Description | Mountain gravel-bed rivers typically display a surface layer that is armored. That is, the surface layer visible at low flow is coarser than both the substrate and mean annual bedload transported. The surface layer is difficult to sample at the high flows that transport most of the gravel. As a result, the question as to whether the surface layer remains armored at high flows is something of a mystery. The few measurements available suggest that some form of armoring may be in place at high... |
Date | 2006-01-01T08:00:00Z |
Type | text |
Identifier | https://digitalcommons.usu.edu/wats_facpub/630 info:doi/10.1016/S0928-2025(07)11127-5 |
Rights | Copyright for this work is held by the author. Transmission or reproduction of materials protected by copyright beyond that allowed by fair use requires the written permission of the copyright owners. Works not in the public domain cannot be commercially exploited without permission of the copyright owner. Responsibility for any use rests exclusively with the user. For more information contact the Institutional Repository Librarian at digitalcommons@usu.edu. |
Source | Watershed Sciences Faculty Publications |
Publisher | Hosted by Utah State University Libraries |
Subject | Bed Surface Size Bed Surface Gravel-Bed Rivers Cycled Hydrograph |