pdf, 12 MiB - Infoscience - EPFL
pdf, 12 MiB - Infoscience - EPFL
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