2017
DOI: 10.5194/esurf-5-239-2017
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Self-similar growth of a bimodal laboratory fan

Abstract: Abstract.Using laboratory experiments, we investigate the growth of an alluvial fan fed with two distinct granular materials. Throughout the growth of the fan, its surface maintains a radial segregation, with the less mobile sediment concentrated near the apex. Scanning the fan surface with a laser, we find that the transition between the proximal and distal deposits coincides with a distinct slope break. A radial cross section reveals that the stratigraphy records the signal of this segregation. To interpret … Show more

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Cited by 19 publications
(27 citation statements)
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“…We believe that this suggests that the size of the largest sediment in the bed may determine the deposition threshold for a mixture, at least for those situations in which competence controls sediment deposition, not sediment transport capacity. The implication of which is that the gradient of self-formed alluvial deposits is likely to be related to the mobility of the largest sediment in transport not the median grain size, as evidenced in bimodal fan experiments (Reitz and Jerolmack, 2012;Delorme et al, 2017).…”
Section: Differential Mobilitymentioning
confidence: 99%
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“…We believe that this suggests that the size of the largest sediment in the bed may determine the deposition threshold for a mixture, at least for those situations in which competence controls sediment deposition, not sediment transport capacity. The implication of which is that the gradient of self-formed alluvial deposits is likely to be related to the mobility of the largest sediment in transport not the median grain size, as evidenced in bimodal fan experiments (Reitz and Jerolmack, 2012;Delorme et al, 2017).…”
Section: Differential Mobilitymentioning
confidence: 99%
“…We know that surficial adjustment, bedforms, and macroforms modulate bed material sediment transport rate, acting to dissipate energy and provide stability to the overall channel (Cherkauer, 1973;Montgomery and Buffington, 1997;Venditti et al, 2017). For example, it has been thought that grains may stabilise through rotation (Masteller and Finnegan, 2017), their organisation into cells (Church et al, 1998;Monsalve and Yager, 2017), and the formation of alternate bars and patches (Lisle et al, 1991;Dietrich et al, 2006;Nelson et al, 2010). One of the most well studied of these adjustment phenomena is the coarsening of the bed surface due to the preferential removal of fines or their kinetic sieving into the subsurface, until an armour layer develops that approximately equalises the threshold entrainment stress of the bed (Parker and Klingeman, 1982;Parker et al, 1982b;Andrews, 1983).…”
Section: Introductionmentioning
confidence: 99%
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“…A sediment transport law was calibrated to compare the experimental results with theory using the methods of Seizilles et al (2013) and Delorme et al (2017). A series of runs were carried out with constant water and sediment feed rates in a 3 cm wide flume.…”
Section: Sediment Transport Lawmentioning
confidence: 99%
“…A sediment transport law was calibrated to compare the experimental results with theory using the methods of Seizilles 2013and Delorme et al, (2017). A series of runs were carried out with constant water and sediment feed rates in a 3cmwide flume.…”
Section: Sediment Transport Lawmentioning
confidence: 99%