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- W2319313587 abstract "The phenomenon of hysteresis in sediment transport explains cycles of scour and fill as floodwaves pass fine grained deposits along the margins of incised river channels. Increased sediment load on the rising limb of floods modifies channel shape and can transform normally depositional eddy recirculation cells into scouring zones. This process was documented on a naturally flowing reach of the Colorado River upstream of Glen Canyon Dam annually, and more frequently downstream on the regulated river. Considering this powerful process is important when managing flows to restore river processes and riverine habitats." @default.
- W2319313587 created "2016-06-24" @default.
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- W2319313587 date "1998-12-09" @default.
- W2319313587 modified "2023-09-25" @default.
- W2319313587 title "Sediment Hysteresis Effects on Fine Grained Deposits" @default.
- W2319313587 cites W2040652656 @default.
- W2319313587 doi "https://doi.org/10.1061/40382(1998)138" @default.
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