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Experiments in alluvial bed channel flow resistance

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Abstract

Experiments were done to develop a flow resistance equation for a rectangular channel with an alluvial bed. The purpose of the experiments was to produce a data set containing statistical bedform measurements from which an effective channel bed roughness could be derived. A tentative flow resistance equation containing a relative roughness term, a channel shape or aspect ratio term, and a Froude number term was produced.

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Abbreviations

A :

constant of integration

B :

constant of integration

b :

statistic for runs test

E(t*):

bed elevation time record

F :

Froude number

f :

Darcy-Weisbach resistance coefficient

G(t*):

autocorrelation function

g :

gravity field strength

I :

nondimensional integral time constant

k :

bed roughness height

L*:

normalized time to first zero crossing of the autocorrelation function

n :

proportionality coefficient

R :

hydraulic radius

r :

correlation coefficient of linear regression

S e :

energy gradient

t*:

time normalized by total record length

U :

local time-mean velocity

Ū :

mean flow velocity

U*:

shear velocity

Y :

composite dependent variable symbol

y :

elevation above the effective channel bottom

y t :

total depth of flow

z :

channel width

°:

boundary layer thickness

χ:

Karman coefficient

ν:

kinematic water viscosity

Π:

wake strength coefficient

σ:

standard deviation of the bed elevation time record

ω:

functional symbol

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Coleman, N.L. Experiments in alluvial bed channel flow resistance. Experiments in Fluids 1, 205–208 (1983). https://doi.org/10.1007/BF00266469

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  • DOI: https://doi.org/10.1007/BF00266469

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