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poster - International Conference of Agricultural Engineering

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ps (cm·s)<br />

Water depth (m)<br />

Water depth (m)<br />

Water depth (m)<br />

Water depth (m)<br />

coverage. On the other hand, the power spectra shift greatly from Eq.1 in the case <strong>of</strong> Type A.<br />

This indicates that the development <strong>of</strong> water surface wave is significantly inhibited by the<br />

existence <strong>of</strong> the coverage in Type A. Moreover, the power spectra in the case <strong>of</strong> Type B and<br />

Type C demonstrate the wind is developed enough compared with Type A. This means that<br />

the development <strong>of</strong> the wind wave was not greatly intercepted because the progressive wave<br />

passed through the area where the coverage did not exist. These experimental results also<br />

indicate that the layout <strong>of</strong> floating object with respect to the wind direction significantly affects<br />

on the hydraulic structure in the waters.<br />

1.E-02<br />

1.E-02<br />

1.E-02<br />

1.E-02<br />

1.E-03<br />

1.E-03<br />

1.E-03<br />

1.E-03<br />

1.E-04<br />

1.E-04<br />

1.E-04<br />

1.E-04<br />

1.E-05<br />

1.E-05<br />

1.E-05<br />

1.E-05<br />

1.E-06<br />

1.E-06<br />

1.E-06<br />

1.E-06<br />

1.E-07<br />

1.E-07<br />

1.E-07<br />

1.E-07<br />

1.E-08<br />

1.E-08<br />

1.E-08<br />

1.E-08<br />

1 10 100 1 10 100 1 10 100 1 10 100<br />

f (Hz)<br />

f (Hz)<br />

f (Hz)<br />

f (Hz)<br />

(a) No coverage (b) Type A (c) Type B (d) Type C<br />

FIGURE 2: Experimental equipment<br />

To investigate the effect <strong>of</strong> floating object existence in detail, the characteristics <strong>of</strong> the flow<br />

velocity and the turbulent energy in the cases <strong>of</strong> Type A and no coverage are compared in<br />

Fig. 3. In the case <strong>of</strong> no coverage, the flow velocity decreases from the water surface to<br />

about 1/3 <strong>of</strong> depth (wind-induced current), and the flow reverses in deeper layer (return<br />

current). That is, it turns out that the vertical circulation flow arises in the test tank. The<br />

turbulent energy is largest near the water surface. On the other hand, in the case <strong>of</strong> Type A,<br />

the flow velocity under the coverage is very small and two wind-induced circulations are<br />

formed at both the upwind and downwind portions <strong>of</strong> the coverage. The distribution <strong>of</strong> the<br />

turbulent energy is also small in the downwind portion <strong>of</strong> coverage.<br />

3. Numerical simulation<br />

3.1 Material and Methods<br />

8cm/s<br />

0<br />

10<br />

20<br />

30<br />

40 0 100 200 300 400 500 600<br />

(a) Flow velocity (No coverage)<br />

0.5cm 2 /s 2<br />

0<br />

10<br />

20<br />

30<br />

40 0 100 200 300 400 500 600<br />

(b) Turbulent energy (No coverage)<br />

8cm/s<br />

0<br />

10<br />

20<br />

30<br />

40 0 100 200 300 400 500 600<br />

(c) Flow velocity (Type A)<br />

0.5cm 2 /s 2<br />

0<br />

10<br />

20<br />

30<br />

40 0 100 200 300 400 500 600<br />

(d) Turbulent energy (Type A)<br />

FIGURE 3: Experimental equipment

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