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Table 3. Focal length and control volume dimensions, in back scatter, of the lenses employed<br />

Probe Focal length Diameter dx1 Diameter dx2 Length dx3<br />

Blue Probe 240 mm 0.05 mm 0.05 mm 0.37 mm<br />

Green probe 310 mm 0.07 mm 0.07 mm 0.63 mm<br />

Red Probe<br />

310 mm 0.07 mm 0.07 mm 0.63 mm<br />

500 mm 0.125 mm 0.124 mm 1.7 mm<br />

X 3<br />

X 2<br />

X 1<br />

X 2<br />

X 3 X 1<br />

(a)<br />

(b)<br />

2<br />

Figure 2 Probe arrangement to measure the velocity gradients: (a) ( ∂ u x ) , ( ∂ u ∂ ) 2<br />

; (b) ( u ∂ ) 2<br />

( u ∂ ) 2<br />

∂ .<br />

3<br />

x 1<br />

1<br />

∂<br />

1<br />

1<br />

x 3<br />

∂ ,<br />

3<br />

x 3<br />

The probes are aligned in air using a pinhole of 50 µm. Once in water, to overcome the effect of refraction, it is<br />

necessary to adjust the relative position of the three control volumes along the X 2 axis by a known distance. As<br />

suggested by Benedict & Gould (1996) a further optimisation of the alignment is achieved computing the spatial<br />

correlation coefficient R ii (0) for different relative positions of the probes until a maximum is found.<br />

The spatial gradients ( u ∂ ) 2<br />

∂ are estimated calculating the function f ii (∆x j ) defined in (9) for the different<br />

i<br />

x j<br />

positions examined around the reference point x i :<br />

f<br />

2<br />

( x ) = (u (x , t) − u (x + ∆x<br />

, t))<br />

ii j<br />

i j<br />

i j j<br />

∆ (9)<br />

When computing the coefficient f ij (∆x j ), the velocity fluctuations u i in the two different points of measurement<br />

must come from particles which cross the two control volumes at the same time. This condition is imposed by<br />

finding the couples of particles that satisfy the following simultaneity criterion:<br />

|t 1 -t 2 | < τ w , (10)<br />

where t 1 and t 2 are the arrival time and τ w is a time coincidence window.<br />

Once the function f ij (∆x j ) is known, the spatial gradient can be calculated from (11)<br />

2<br />

( u ( x , t) − u ( x + ∆x<br />

, t<br />

)<br />

2<br />

⎛ u ⎞<br />

i j<br />

i j j<br />

⎜<br />

∂<br />

i<br />

⎟ = lim<br />

(11)<br />

x 0<br />

2<br />

j<br />

x<br />

∆ ⇒<br />

⎝ ∂<br />

j ⎠<br />

∆x<br />

j<br />

The spatial gradient can be evaluated by finding the slope of the straight line which best fits the points (∆x 2 j ,<br />

f ii (∆x j )) for ∆x j values close to zero. Once all the gradients have been determined, the value obtained for the<br />

dissipation rate estimated from equation (6) for homogenous flow is compared with the value obtained from<br />

equation (7) for grid turbulence flow.<br />

5

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