Variations in the architecture of hydraulic-jump bar complexes on non-eroding beds
Sediment accumulation downstream of hydraulic jumps can occur in many settings but the architectures of such deposits are poorly documented. Here, three flume runs were used to examine the influence of sediment grain size and transport rate on the characteristics of hydraulic‐jump unit bars. In one...
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Veröffentlicht in: | Sedimentology 2013-08, Vol.60 (5), p.1291-1312 |
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Format: | Artikel |
Sprache: | eng |
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