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View the Whole Report - Center for Research in Water Resources ...

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Flow per Area, cm/s<br />

40<br />

30<br />

20<br />

10<br />

0<br />

y = 22.322x 0.457<br />

R 2 = 0.9981<br />

0 0.1 0.2 0.3 0.4 0.5 0.6<br />

Level, m<br />

Figure 5.9 Flow vs. Head <strong>for</strong> Belton Woven Fabric (not vacuumed)<br />

root of <strong>the</strong> head. The data observed <strong>for</strong> <strong>the</strong> permeameter tests show that <strong>the</strong> actual<br />

dra<strong>in</strong>age behavior lies somewhere between <strong>the</strong>se two cases. At <strong>the</strong> low heads used <strong>in</strong><br />

ASTM D 4491, 10-75 mm, <strong>the</strong> relationship between flow rate and head could be<br />

approximated by a l<strong>in</strong>ear function.<br />

The velocity through <strong>the</strong> fabric dur<strong>in</strong>g <strong>the</strong> permeameter test was calculated us<strong>in</strong>g<br />

<strong>the</strong> Amoco 2125 (3.3% open area), <strong>the</strong> fabric specimen area, and <strong>the</strong> permeameter flow<br />

rate. This velocity and a pore diameter (AOS = 850 µm), were used to calculate <strong>the</strong><br />

Reynolds numbers shown <strong>in</strong> Table 5.8.<br />

Table 5.8 Velocities and Reynolds Number <strong>for</strong> Flow Through Amoco Woven Fabric<br />

Head, m Q/A, cm/s Velocity, m/s Re<br />

0.05 1.8 0.54 459<br />

0.1 3.2 1.0 825<br />

0.2 4.8 1.4 1,230<br />

0.3 5.2 1.9 1,610<br />

0.4 7.2 2.2 1,860<br />

0.5 8.0 2.4 2,060<br />

0.6 8.7 2.6 2,230<br />

The transition from lam<strong>in</strong>ar flow occurs <strong>in</strong> subsurface flow when <strong>the</strong> Reynolds<br />

number exceeds 10 and <strong>in</strong> pipe flow when <strong>the</strong> Reynolds number exceeds 2,000.<br />

Turbulent flow through a geotextile will occur when <strong>the</strong> Reynolds number is between<br />

51

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