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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 />

37

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