Grain size and topographical differences between static and mobile armour layers-Reference-Cited by-同舟云学术

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Grain size and topographical differences between static and mobile armour layers

Published:2011-03-28 Issue:10 Volume:36 Page:1321-1334
ISSN:0197-9337
Container-title:Earth Surface Processes and Landforms
language:en
Short-container-title:Earth Surf. Process. Landforms

Author:

Mao Luca¹,Cooper James R.²,Frostick Lynne E.³

Affiliation:

1. Faculty of Science and Technology; Free University of Bozen-Bolzano; Bozen-Bolzano; Italy

2. Department of Geography; University of Sheffield; Sheffield; UK

3. Centre for Adaptive Science and Sustainability and Department of Geography; University of Hull; Hull; UK

Publisher

Wiley

Subject

Earth and Planetary Sciences (miscellaneous),Earth-Surface Processes,Geography, Planning and Development

Reference58 articles.

1. Statistical properties of armored gravel bed surfaces;Aberle;Water Resources Research,2006

2. The influence of roughness structure on flow resistance on steep slopes;Aberle;Journal of Hydraulic Research,2003

3. Framework dilation, winnowing, and matrix particle size: the behaviour of some sand-gravel mixtures in a laboratory flume;Allan;Journal of Sedimentary Research,1999

4. Persistence in the size distribution of surficial bed material during an extreme snowmelt flood;Andrews;Water Resources Research,1986

5. A general power equation for predicting bed-load transport rates in gravel bed rivers;Barry;Water Resources Research,2004

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