Articles | Volume 8, issue 3
https://doi.org/10.5194/esurf-8-717-2020
https://doi.org/10.5194/esurf-8-717-2020
Short communication
 | 
31 Aug 2020
Short communication |  | 31 Aug 2020

Short communication: Field data reveal that the transport probability of clasts in Peruvian and Swiss streams mainly depends on the sorting of the grains

Fritz Schlunegger, Romain Delunel, and Philippos Garefalakis

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Cited articles

Bekaddour, T., Schlunegger, F., Attal, M., and Norton, K. P.: Lateral sediment sources and knickzones as controls on spatio-temporal variations of sediment transport in an Alpine river, Sedimentology, 60, 342–357, 2013. 
Bunte, K., Abt, S. R., Swingle, K. W., Cenderelli, D. A., and Schneider, M.: Critical Shields values in coarse-bedded steep streams, Water Res. Res., 49, 7427–7447, 2013. 
Brooke, S. A. S., Whittaker, A. C., Armitage, J. J., D'Arcy, M., and Watkins, S.: Quantifying Sediment Transport Dynamics on Alluvial Fans From Spatial and Temporal Changes in Grain Size, Death Valley, California, J. Geophys. Res.-Earth, 123, 2019–2067, https://doi.org/10.1029/2018JF004622, 2018. 
Buffington, J., Dietrich, W. E., and Kirchner, J. W.: Friction angle measurements on a naturally formed gravel streambed: Implications for critical boundary shear stress, Water Res. Res., 28, 411–425, 1992. 
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Short summary
We calculated the probability of sediment transport in coarse-grained mountainous streams in the Alps and the Andes where data on water discharge is available. We find a positive correlation between the predicted probability of sediment transport and the grain size sorting of the bed material. We suggest that besides sediment discharge, the bedload sorting exerts a significant influence on the mobility of sediment and thus on the stability of gravel bars in mountainous streams.
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