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CLASS PLAN
• RIVER BEHAVIOR
• FLOW GAUGING
• MANNING’S EQUATION
• BANKFULL DISCHARGE
• DISCUSS MCPHEE
RIVERS
• On Huntington, in water
• Warm clothes, food, $, Daily Bread
• Measure discharge - survey and velocity
• Trace flow
• Compare pools and riffles
• Field estimate of bankfull stage
FLOW GAUGING
• QUANTIFY VOLUME OF WATER MOVING THROUGH CHANNEL
• NEED CHANNEL GEOMETRY
• NEED VELOCITY
Sediment Transport Through Rivers
Bedload -- material moving along the bed, shear forces exerted by water sufficient to move clasts
Suspended Load -- material kept in the water column by turbulence and lift forces
Bedload usually <<< than suspended load and ignored
Dissolved Load -- material kept in the water column by turbulence and lift forces
Dissolved load varies, usually <<< than suspended load
Mass Loadings and Erosion Rate Estimation
Integrate suspended load over all flows (mass/time)
Integrate bedload load over all flows (mass/time)
Integrate dissolved load over all flows (mass/time)
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Integration over all flows is a non trivial problem!
Need Rating Curves (suspended, dissolved, bedload)
SEDIMENT YIELD - What comes out
SEDIMENT GENERATION - Material generated by erosion
= or ≠TimescaleSteady stateHuman impactEpisodic disturbance