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along with runoff from <strong>the</strong> flume. The fill<strong>in</strong>g period of <strong>the</strong> test stopped when ei<strong>the</strong>r <strong>the</strong><br />
water level <strong>in</strong> <strong>the</strong> flume reached 0.35 m or <strong>the</strong> slurry tank was emptied.<br />
5.1.2 The Soil and Suspended Solids Slurry<br />
Top soil (Aust<strong>in</strong> silty clay) was used to create <strong>the</strong> simulated runoff. Various<br />
properties of Aust<strong>in</strong> silty clay are presented <strong>in</strong> Table 5.1 and Table 5.2.<br />
Table 5.1 Soil Characteristics (SCS, 1974)<br />
Parent material<br />
Aust<strong>in</strong> chalk<br />
Hydraulic Conductivity 1.5-5 cm/hr<br />
Available water capacity 0.15-0.18 m/m<br />
pH 7.9-8.4<br />
Shr<strong>in</strong>kage limit 11.4 %<br />
Plasticity <strong>in</strong>dex 36 %<br />
Liquid limit 64 %<br />
L<strong>in</strong>eal shr<strong>in</strong>kage 20.9 %<br />
Volume shr<strong>in</strong>kage 50.5 %<br />
Table 5.2 Mechanical Sieve Analysis (SCS, 1974)<br />
Particle Size, mm Percent Pass<strong>in</strong>g<br />
4.7 100<br />
2.0 99<br />
0.42 98<br />
0.074 92<br />
0.05 89<br />
0.005 58<br />
0.002 42<br />
The soil was screened through a # 8 sieve (3 mm) be<strong>for</strong>e be<strong>in</strong>g mixed with water<br />
to make a slurry. At <strong>the</strong> outset of this work, we expected all <strong>the</strong> soil added to <strong>the</strong> slurry to<br />
become suspended; however, a fraction of <strong>the</strong> silty clay did not become suspended. This<br />
phenomenon created difficulties <strong>in</strong> proportion<strong>in</strong>g <strong>the</strong> soil and water <strong>in</strong> <strong>the</strong> slurry. The<br />
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