Generalized sorting profile of alluvial fans
Alluvial rivers often exhibit self‐similar gravel size distributions and abrupt gravel‐sand transitions. Experiments suggest that these sorting patterns are established rapidly, but how—and how fast—this convergence occurs in the field is unknown. We examine the establishment of downstream sorting p...
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Published in | Geophysical research letters Vol. 41; no. 20; pp. 7191 - 7199 |
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Main Authors | , , |
Format | Journal Article |
Language | English |
Published |
Washington
Blackwell Publishing Ltd
28.10.2014
John Wiley & Sons, Inc |
Subjects | |
Online Access | Get full text |
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Summary: | Alluvial rivers often exhibit self‐similar gravel size distributions and abrupt gravel‐sand transitions. Experiments suggest that these sorting patterns are established rapidly, but how—and how fast—this convergence occurs in the field is unknown. We examine the establishment of downstream sorting patterns in a kilometer‐scale alluvial fan. The sharp transition from canyon to unconfined, channelized fan provides a well‐defined boundary condition. The channel changes from deep and entrenched at the fan apex to shallow and depositional over a short distance, exhibiting nonequilibrium behavior. The resulting gravel‐fining profile is not self‐similar; the particle size distribution narrows until approximate equal mobility is achieved. Downfan, the gravel‐sand transition appears to exhibit a self‐similar form; field and laboratory data collapse when downstream distance is normalized by the location of the transition. Results suggest a generalized sorting profile for alluvial fans as a consequence of the threshold of motion and nonequilibrium channels.
Key Points
Gravel sorting is limited by equal mobility of the grain size distributionThe gravel‐sand transition exhibit a self‐similar formTransient dynamics control channel geometry on fan |
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Bibliography: | istex:3EF59A4ABA977DCA739765359406EF1BEDA16087 ArticleID:GRL52241 ark:/67375/WNG-DPK2P8C6-P |
ISSN: | 0094-8276 1944-8007 |
DOI: | 10.1002/2014GL060991 |