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Optimization and Computational Fluid Dynamics - Department of ...

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9 CFD-based optimization for papermaking 275<br />

<strong>of</strong> using the 3D geometry <strong>of</strong> the headbox slice channel, the depth-averaged<br />

Navier-Stokes equations are used. These equations are introduced next.<br />

Let the velocity vector U =(u,v,w) <strong>and</strong> the static pressure p be a solution<br />

<strong>of</strong> the 3D Navier-Stokes equations. The depth-averaged pressure P <strong>and</strong> the<br />

velocity components U <strong>and</strong> V are defined as averaged values in the vertical<br />

direction over the depth <strong>of</strong> the slice channel as follows<br />

U (x, z)=<br />

V (x, z)=<br />

P (x, z)=<br />

1<br />

D (x, z)<br />

1<br />

D (x, z)<br />

1<br />

D (x, z)<br />

�<br />

D(x,z)<br />

0<br />

�<br />

D(x,z)<br />

0<br />

�<br />

D(x,z)<br />

0<br />

u (x, y, z)dy<br />

v (x, y, z)dy<br />

p (x, y, z)dy<br />

(9.1)<br />

where D =(x, z) is the depth <strong>of</strong> the slice channel depending on a position<br />

(x, z). Then, by integrating the 3D continuity equation over the depth <strong>and</strong> by<br />

using the definitions (9.1), the following depth-averaged continuity equation<br />

is obtained<br />

∇·(DV ) = 0 (9.2)<br />

where V =(U,V ) is the reduced 2D velocity vector. The depth-averaged<br />

momentum equation is derived similarly, <strong>and</strong> it is<br />

where<br />

− 1<br />

D ∇·�2μDε (V ) � + ρC(m)V ·∇(DV )<br />

�<br />

4(m +1)μ<br />

+<br />

D2 �<br />

V + ∇P =0<br />

C (m)=<br />

2m +2<br />

2m +1<br />

(9.3)<br />

, m ≥ 2 (9.4)<br />

is a coefficient associated with the velocity pr<strong>of</strong>ile in the depth direction. For<br />

example, m = 2 corresponds to a parabolic velocity pr<strong>of</strong>ile, <strong>and</strong> m =7to<br />

a turbulent plug flow pr<strong>of</strong>ile. See also [33] for depth-averaging <strong>of</strong> the k–ε<br />

turbulence model.

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