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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Bibliographic Details
Published inGeophysical research letters Vol. 41; no. 20; pp. 7191 - 7199
Main Authors Miller, Kimberly Litwin, Reitz, Meredith D., Jerolmack, Douglas J.
Format Journal Article
LanguageEnglish
Published Washington Blackwell Publishing Ltd 28.10.2014
John Wiley & Sons, Inc
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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
Bibliography:istex:3EF59A4ABA977DCA739765359406EF1BEDA16087
ArticleID:GRL52241
ark:/67375/WNG-DPK2P8C6-P
ISSN:0094-8276
1944-8007
DOI:10.1002/2014GL060991