2010
DOI: 10.1002/esp.1908
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Effects of vegetation on channel morphodynamics: results and insights from laboratory experiments

Abstract: A series of laboratory experiments demonstrates that riparian vegetation can cause a braided channel to self-organize to, and maintain, a dynamic, single-thread channel. The initial condition for the experiments was steady-state braiding in noncohesive sand under uniform discharge. From here, an experiment consisted of repeated cycles alternating a short duration high fl ow with a long duration low fl ow, and uniform dispersal of alfalfa seeds over the bed at the end of each high fl ow. Plants established on f… Show more

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Cited by 320 publications
(361 citation statements)
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“…More specifically, field observations suggest that a heavier sediment load tends to increase the aspect ratio of a thread, other things being equal (Smith and Smith, 1984;Tal and Paola, 2010;Métivier and Barrier, 2012). This proposition remains speculative though, and needs to be thoroughly tested against dedicated field measurements, which we believe should include both braided and meandering threads.…”
Section: Resultsmentioning
confidence: 95%
“…More specifically, field observations suggest that a heavier sediment load tends to increase the aspect ratio of a thread, other things being equal (Smith and Smith, 1984;Tal and Paola, 2010;Métivier and Barrier, 2012). This proposition remains speculative though, and needs to be thoroughly tested against dedicated field measurements, which we believe should include both braided and meandering threads.…”
Section: Resultsmentioning
confidence: 95%
“…Klaassen and Van der Zwaard, 1974). These include theoretical principles of the mathematical modelling of the phenomenon (Baptist et al, 2007;Horritt, 2006;Klopstra et al, 1997;Wu et al, 2001;Yang and Choi, 2010), numerical modelling with models of varying complexity (Crosato and Saleh, 2011;Perona et al, 2009;Velasco et al, 2008), flume experiments to verify models of vegetation roughness and in situ floodplain roughness estimations (Meijer and van Velzen, 1999;Murphy et al, 2007;Straatsma, 2009;Tal and Paola, 2010). Some studies focused on the accumulation of both thick and fine debris (Mazur et al, 2016) carried along with the flood wave.…”
Section: Introductionmentioning
confidence: 99%
“…Meanders create a low velocity zone adjacent to point bars that form through deposition of bedload and later suspended sediment. Vegetation growing on deposited coarse bedload material increases stability and roughness, decreases flow velocities, increases deposition of finer suspended sediment (figures 2e and 3b to 3g) (Robertson and Augspurger 1999;Steiger and Gurnell 2003;Rood et al 2003;Robertson 2006;Polzin and Rood 2006), and encourages meander development (Erskine et al 2009(Erskine et al , 2012Rominger et al 2010;Tal and Paola 2010), which decreases stream gradient and power (Bagnold 1966). Deposition of fine alluvial soil facilitates revegetation while it removes water pollution.…”
Section: Geomorphologymentioning
confidence: 99%