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pdf, 12 MiB - Infoscience - EPFL

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Bed topography in the bend<br />

ZIMMERMANN assumed a fully developed secondary flow, which is not always found in natural<br />

river bends. Furthermore, his formula gives a straight line for the transverse bed slope which does<br />

not really correspond to laboratory and field observations.<br />

7) Falcon & Kennedy (1983)<br />

FALCON & KENNEDY (1983) (see also FALCON, 1979) used DU BOYS approach of a sediment<br />

transport in layers. They considered a control volume in the armoring layer at equilibrium state.<br />

Based on the work of KARIM (1981), the authors gave the thickness of the control volume (thickness<br />

of the armoring layer) with:<br />

V∗<br />

z b = d 50 ⋅ ----------<br />

(3.104)<br />

Based on a vertical distribution of radial shear stresses, the primary flow velocity given by the<br />

power law vrz ( , ) ⁄ V = ( n + 1) ⁄ n⋅<br />

z 1 ⁄ n and the definition of the exponent 1 ⁄ n = f ⁄ 8 ⁄ κ,<br />

their equation for the lateral bed profile writes:<br />

dh s 8 ⋅ θ 1 + f h<br />

sinβ ≈ ------- --------------- --------------------- s<br />

= ⋅ ⋅Fr (3.105)<br />

dr ( 1 – p)<br />

d ⋅ ----<br />

1 + 2⋅<br />

f r<br />

with p, the porosity of the armoring layer, f = 8 ⋅ g⋅ h m<br />

⋅ S e<br />

⁄ V2<br />

m<br />

, where V m<br />

is the local depth<br />

averaged velocity. They assumed that κ = 0.354 and therefore n = f (see eq. 3.102).<br />

V∗ cr<br />

The approach of FALCON & KENNEDY is similar to the one of ZIMMERMANN. The difference<br />

resides in the fact that FALCON & KENNEDY considered a vertical control volume, while ZIM-<br />

MERMANN considered the whole cross-section. The formula of Zimmermann also accounts for<br />

the vertical shear stresses.<br />

8) Odgaard (1986)<br />

ODGAARD (1981, 1982, 1984 and 1986) considered the forces acting on a control volume in a stable<br />

armoring layer, without any sediment transport (nor in radial, nor in stream direction). Taking<br />

into account the equation of FALCON (1979) and FALCON & KENNEDY (1983) for the radial drag<br />

force, the following formula is obtained:<br />

β<br />

dh s<br />

≈ -------<br />

3<br />

sin ----------<br />

⋅ α<br />

------<br />

θ n + 1 h<br />

----------- s<br />

= ⋅ ⋅ ⋅ Fr (3.106)<br />

dr 2 κ n + 2 d ⋅ ----<br />

r<br />

where α = 1 ⁄ k 2<br />

is the ratio of the projected area of a sediment grain normalized by d 2 ,<br />

κ = 0.4 the von Karman constant, C the Chezy coefficient and n is given with:<br />

κ κ ⋅ C<br />

n = ------------ = ----------<br />

(3.107)<br />

8 ⁄ f g<br />

Putting α = 4 ⁄ π , κ = 0.4 and ( n + 1) ⁄ ( n + 2)<br />

≈ 1 , an earlier version of the same formula<br />

given in ODGAARD (1984) can be obtained:<br />

β<br />

dh s<br />

h<br />

sin ≈ ------- = 4.8 ⋅ θ ⋅ Fr s<br />

dr<br />

d ⋅ ----<br />

r<br />

(3.108)<br />

<strong>EPFL</strong> Ph.D thesis 2632 - Daniel S. Hersberger November 9, 2002 / page 53

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