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What’s New in Sedimentation and River Mechanics Pierre Julien Spring 2001
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Objectives n Bedforms and resistance to flow during floods. n Effects of dams on hydraulic geometry. n River response to deviations from equilibrium geometry of alluvial rivers.
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Rhine River flood in 1998
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Primary dune height vs discharge
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Roughness height vs discharge
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Darcy-Weisbach f vs discharge
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Manning n vs discharge
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Downstream hydraulic geometry
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Cochiti Dam Santa Fe River Rio Grande N
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Peak Annual Discharge
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Annual Average Daily Sediment Concentration
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1.1 1.9 2.1 4.6 3.5 4.1 3.1 2.6 26 Subreaches 284 Cross sections 4 Reaches
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Cross section CO-2
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Cross section CO-18
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Cross section CO-24
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Change in Mean Bed Elevation Reach 1 Reach 2 Reach 3Reach 4
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Bed material size
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Sinuosity
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Active channel width
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19351972 1992 N Planform geometry
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Planform Adjustments BraidedMeandering
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Lateral Adjustments
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Equilibrium? Hydraulic Geometry Equations
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19181992 (Julien & Wargadalam 1995)
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Modeling Lateral Movement Deviation from Equilibrium
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Modeling Width Change Deviation from equilibrium width
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Exponential Model Results
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Conclusions n Bedforms affect resistance to flow and Manning n can increase during floods. n The effects of Cochiti Dam on the Rio Grande are primarily degradation and armouring. There is relatively little effect on channel width. n The rate of change in channel width is proportional to the deviation from the equilibrium channel width.
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