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pdf, 12 MiB - Infoscience - EPFL

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Chapter 3 - Theoretical considerations<br />

3.5 Bed topography in the bend<br />

3.5.1 Introduction<br />

In general scour formulae are established based on equilibrium considerations of the forces acting<br />

on a grain. Taking the water depth h (free water surface to bed surface) and the radius r as<br />

variables, the local lateral bed slope is usually given by:<br />

sinβ<br />

K h s<br />

= ⋅ ----<br />

r<br />

(3.54)<br />

h s<br />

h m<br />

β<br />

r<br />

R c<br />

B<br />

B<br />

θ<br />

r<br />

R c<br />

Figure 3.6: Definition sketch; situation and cross-section<br />

In order to obtain the cross-section at the location of maximum scour,<br />

sinβ≈<br />

tanβ<br />

= dh ⁄ dr and yields (after integration):<br />

h s<br />

r<br />

----- = ⎛-----<br />

⎝ ⎠<br />

h m<br />

R c<br />

⎞ K<br />

sinβ<br />

is approached with<br />

(3.55)<br />

3.5.2 Scour formulae<br />

1) Fargue (1868) and Williams (1899)<br />

LOUIS JÉRÔME FARGUE (1872-1910) (cited in FARGUE, 1868 and in WILLIAMS, 1899) was probably<br />

the first to establish a scour formula for river bends. He established six laws based on observations<br />

of a 22 km long reach of the Garonne River in France, derived with momentum<br />

considerations. Two of them are given hereafter:<br />

1. Law of displacement: The deepest and the highest point of the bed topography in a bend are<br />

located towards half the opening angle between beginning and end of the bend or in downstream<br />

direction of this point.<br />

2. Law of depth: The greater the curvature, the greater the depth.<br />

page 40 / November 9, 2002<br />

Wall roughness effects on flow and scouring

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