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the effect of the particle size distribution on non-newtonian turbulent ...

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Chapter 3 Experimental Work Page 3.22<br />

3.6.2 Rock Flour<br />

Rock Flour was obtained from Hippo Quarries from <str<strong>on</strong>g>the</str<strong>on</strong>g>ir quarry called Peninsula.<br />

3.6.3 Sand<br />

Sand was obtained from C<strong>on</strong>sol in 2Skg bags called No. 2 Foundry Sand. The <str<strong>on</strong>g>particle</str<strong>on</strong>g> <str<strong>on</strong>g>size</str<strong>on</strong>g><br />

<str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> sand was between 7S and 3S0 /Lm.<br />

3.7 ]',llXTURES<br />

3.7.1 Mixture Kaolin Clay and Rock Flour<br />

The rock flour was found to form a settling slurry when mixed with water. In order to<br />

obtain a homogeneous slurry kaolin clay was used as a suspending agent for <str<strong>on</strong>g>the</str<strong>on</strong>g> rock flour.<br />

Tests were <str<strong>on</strong>g>the</str<strong>on</strong>g>refore c<strong>on</strong>ducted to determine <str<strong>on</strong>g>the</str<strong>on</strong>g> amount <str<strong>on</strong>g>of</str<strong>on</strong>g> kaolin clay needed to suspend <str<strong>on</strong>g>the</str<strong>on</strong>g><br />

rock flour.<br />

Twenty sample bottles each c<strong>on</strong>taining 200g <str<strong>on</strong>g>of</str<strong>on</strong>g> water were used for <str<strong>on</strong>g>the</str<strong>on</strong>g> tests. For Test A,<br />

10 <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> sample bottles c<strong>on</strong>tained rock flour at a relative density <str<strong>on</strong>g>of</str<strong>on</strong>g> 1,1 and for Test B, <str<strong>on</strong>g>the</str<strong>on</strong>g><br />

remaining ten sample bottles c<strong>on</strong>tained rockflour at a relative density <str<strong>on</strong>g>of</str<strong>on</strong>g> 1,2.<br />

Kaolin clay was <str<strong>on</strong>g>the</str<strong>on</strong>g>n added to <str<strong>on</strong>g>the</str<strong>on</strong>g> sample bottles in Test A, starting at 5g <str<strong>on</strong>g>of</str<strong>on</strong>g> kaolin clay for<br />

L1e first sample bottle and increasing in Sg amounts per sample bottle until <str<strong>on</strong>g>the</str<strong>on</strong>g> last sample<br />

bottle c<strong>on</strong>tained SOg <str<strong>on</strong>g>of</str<strong>on</strong>g> kaolin clay. The rock flour and kaolin clay were <str<strong>on</strong>g>the</str<strong>on</strong>g>n thoroughly<br />

mixed and allowed to stand. This procedure was repeated for Test B.<br />

It Was found that in both Test A and Test B that 30g <str<strong>on</strong>g>of</str<strong>on</strong>g> kaolin clay was required to suspend<br />

<str<strong>on</strong>g>the</str<strong>on</strong>g> rock flour and form a homogeneous slurry. At 25g <str<strong>on</strong>g>of</str<strong>on</strong>g> kaolin clay added, <str<strong>on</strong>g>the</str<strong>on</strong>g> mixture<br />

formed a slow settling slurry and hence <str<strong>on</strong>g>the</str<strong>on</strong>g> critical point lay between <str<strong>on</strong>g>the</str<strong>on</strong>g>se two limits ie. 2Sg<br />

and 30g <str<strong>on</strong>g>of</str<strong>on</strong>g> kaolin. It was <str<strong>on</strong>g>the</str<strong>on</strong>g>refore decided to use <str<strong>on</strong>g>the</str<strong>on</strong>g> c<strong>on</strong>centrati<strong>on</strong> ratio <str<strong>on</strong>g>of</str<strong>on</strong>g> 30g <str<strong>on</strong>g>of</str<strong>on</strong>g> kaolin<br />

clay per 200g water to suspend <str<strong>on</strong>g>the</str<strong>on</strong>g> rock flour for <str<strong>on</strong>g>the</str<strong>on</strong>g> tests in <str<strong>on</strong>g>the</str<strong>on</strong>g> pipelines or a kaolin<br />

c<strong>on</strong>Centrati<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> at least Cv =S%.

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