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

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

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Appendix B Conference Paper 2.4.6.3 Representative Particle Size The wall roughness and ong>particleong> ong>effectong> was taken into account in ong>theong> roughness Reynolds number as given by Slatter (1994). The ong>effectong> ong>ofong> roughness on turbulence can be thought ong>ofong> as an aggravation at ong>theong> wall which stimulates turbulence. Clearly ong>theong>n ong>theong> larger ong>particleong>s will have a more dominant ong>effectong> on turbulence than ong>theong> smaller ong>particleong>s. Also, ong>theong> larger ong>particleong>s will shield ong>theong> smaller ones, reducing ong>theong>ir ong>effectong>iveness in stimulating turbulence (Colebrook, 1939). For all ong>theong> slurries tested to date it was found that ong>theong> d S5 ong>sizeong> was a good representation ong>ofong> ong>theong> turbulent roughness ong>sizeong> ong>effectong> ong>ofong> ong>theong> solid ong>particleong>s in ong>theong> slurry ie

Appendix B Conference Paper IfRe, < 3,32 ong>theong>n smooth wall turbulent flow exists and ong>theong> mean velocity is given by :.Y.- = 2,5 In [-!.] + 2,5 In Re + 1,75 . V. dss • ' If Re,. > 3,32 ong>theong>n fully developed rough wall turbulent flow exists and ong>theong> mean velocity is given by Y.- [-!.] = 2,5 In + V. dss 4,75 , and ong>theong> friction factor is constant. This correlation produces a transition from ong>theong> smooth to ong>theong> rough flow condition which is abrupt. Tests conducted by Slatter (1994) confirmed ong>theong> model to be more accurate than ong>theong> Torrance (1963) model and Wilson & Thomas (1985, 1987) model, when evaluated against experimental data. 2.4.7 Data from ong>theong> Literature Experimental data obtained by Sive (1988) was used in ong>theong> analysis ong>ofong> ong>theong> various models under consideration. The tests conducted by Sive (1988) were done using a mixture ong>ofong> kaolin clay and a relatively coarse quartz sand, which resulted in a heterogeneous, settling slurry. The purpose ong>ofong> using this data was to see if ong>theong> coarse, settling ong>particleong>s contributed to ong>theong> turbulent flow headloss, as proposed by ong>theong> Slatter model. 3. EXPERIMENTAL WORK The test facility at ucr which was used had four different pipe diameters namely 25mm, 80mm, 150mm and 200mm nominal bore and slurries were tested at mean velocities ranging from 0, Imls to 8m/s. Slurries tested included kaolin clay and mixture ong>ofong> kaolin clay and fine sand at varying ratios. (10) (11) (12) B.9

Appendix B C<strong>on</strong>ference Paper<br />

IfRe, < 3,32 <str<strong>on</strong>g>the</str<strong>on</strong>g>n smooth wall <strong>turbulent</strong> flow exists and <str<strong>on</strong>g>the</str<strong>on</strong>g> mean velocity is given by<br />

:.Y.- = 2,5 In [-!.] + 2,5 In Re + 1,75 .<br />

V. dss • '<br />

If Re,. > 3,32 <str<strong>on</strong>g>the</str<strong>on</strong>g>n fully developed rough wall <strong>turbulent</strong> flow exists and <str<strong>on</strong>g>the</str<strong>on</strong>g> mean<br />

velocity is given by<br />

Y.- [-!.] = 2,5 In +<br />

V. dss<br />

4,75 ,<br />

and <str<strong>on</strong>g>the</str<strong>on</strong>g> fricti<strong>on</strong> factor is c<strong>on</strong>stant.<br />

This correlati<strong>on</strong> produces a transiti<strong>on</strong> from <str<strong>on</strong>g>the</str<strong>on</strong>g> smooth to <str<strong>on</strong>g>the</str<strong>on</strong>g> rough flow c<strong>on</strong>diti<strong>on</strong> which<br />

is abrupt.<br />

Tests c<strong>on</strong>ducted by Slatter (1994) c<strong>on</strong>firmed <str<strong>on</strong>g>the</str<strong>on</strong>g> model to be more accurate than <str<strong>on</strong>g>the</str<strong>on</strong>g><br />

Torrance (1963) model and Wils<strong>on</strong> & Thomas (1985, 1987) model, when evaluated<br />

against experimental data.<br />

2.4.7 Data from <str<strong>on</strong>g>the</str<strong>on</strong>g> Literature<br />

Experimental data obtained by Sive (1988) was used in <str<strong>on</strong>g>the</str<strong>on</strong>g> analysis <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> various<br />

models under c<strong>on</strong>siderati<strong>on</strong>. The tests c<strong>on</strong>ducted by Sive (1988) were d<strong>on</strong>e using a<br />

mixture <str<strong>on</strong>g>of</str<strong>on</strong>g> kaolin clay and a relatively coarse quartz sand, which resulted in a<br />

heterogeneous, settling slurry. The purpose <str<strong>on</strong>g>of</str<strong>on</strong>g> using this data was to see if <str<strong>on</strong>g>the</str<strong>on</strong>g> coarse,<br />

settling <str<strong>on</strong>g>particle</str<strong>on</strong>g>s c<strong>on</strong>tributed to <str<strong>on</strong>g>the</str<strong>on</strong>g> <strong>turbulent</strong> flow headloss, as proposed by <str<strong>on</strong>g>the</str<strong>on</strong>g> Slatter<br />

model.<br />

3. EXPERIMENTAL WORK<br />

The test facility at ucr which was used had four different pipe diameters namely<br />

25mm, 80mm, 150mm and 200mm nominal bore and slurries were tested at mean<br />

velocities ranging from 0, Imls to 8m/s. Slurries tested included kaolin clay and mixture<br />

<str<strong>on</strong>g>of</str<strong>on</strong>g> kaolin clay and fine sand at varying ratios.<br />

(10)<br />

(11)<br />

(12)<br />

B.9

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