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Published byElmer Walton Modified over 6 years ago
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Stream Cross-Section for Q
Measure V (current-meter) at 0.2 and 0.8 of depth Average V and multiply by (width * depth) Sum up across stream to get total Q = S (Vi Di Wi)
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Rating curve hysteresis loop in Zenne river (Lot), July 2012 event: blue triangles – rising stage, green squares – falling stage
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Flume tests carefully conducted by Nomicos (1957) at CalTech:
constant-depth, unique sediment size d=0.152mm difficult to reconcile with the standard formulation for the ‘alluvial resistance coefficient’:
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Bed-material discharge
Buoyancy-affected turbulence Bed morphology adaptation Alluvial resistance
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Hyperbolic tangent of x = tanh x = (ex - e-x)/(ex + e-x)
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If lBF is the wavelength from crest to crest, the celerity of the associated gravity wave is given by Airy’s law:
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Facteur m Ok théorie m = 1, m = 1,2
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Discontinuity rating curve
original discontinuity rating curve Modified discontinuity rating curve
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