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Mechanics of Fluids

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250 Flow and losses in pipes and fittings<br />

Fig. 7.3<br />

in the form shown in Fig. 7.3. One <strong>of</strong> the first to present results in this way<br />

was Sir Thomas E. Stanton (1865–1931) who, with J. R. Pannell, conducted<br />

experiments on a number <strong>of</strong> pipes <strong>of</strong> various diameters and materials, and<br />

with various fluids. Figure 7.3 is based on results obtained by the German<br />

engineer Johann Nikuradse using circular pipes that had been artificially<br />

roughened using sand grains.<br />

At the left-hand side <strong>of</strong> the diagram is a single line corresponding to<br />

Reynolds numbers ud/v less than 2000. In this range the flow is laminar and<br />

is governed by Poiseuille’s equation (6.7). A rearrangement <strong>of</strong> that equation<br />

gives<br />

h f = �p∗<br />

ϱg<br />

8Qlµ<br />

=<br />

πR4 8ulµ<br />

=<br />

ϱg R2ϱg since the mean velocity u = Q/πR 2 . But a rearrangement <strong>of</strong> eqn 7.1 gives<br />

f = (2gd/4lu 2 )h f and so, for laminar flow,<br />

f = 2gd<br />

4lu2 8ulµ<br />

(d/2) 2 16µ 16<br />

= =<br />

ϱg udϱ Re<br />

(7.4)<br />

With the logarithmic scales used in Fig. 7.3, eqn 7.4 is represented by a<br />

straight line. Experimental results confirm the equation and the fact that<br />

laminar flow is independent <strong>of</strong> the roughness <strong>of</strong> the pipe walls (unless the<br />

roughness is so great that the irregularities constitute an appreciable change<br />

<strong>of</strong> diameter).<br />

For Reynolds numbers greater than about 2000, that is, for turbulent flow,<br />

the flow does depend on the roughness <strong>of</strong> the pipe, and different curves are<br />

obtained for different values <strong>of</strong> the relative roughness. In Nikuradse’s experiments,<br />

grains <strong>of</strong> sand <strong>of</strong> uniform size were glued to the walls <strong>of</strong> pipes <strong>of</strong><br />

various diameters, which were initially very smooth. Thus a value <strong>of</strong> the<br />

relative roughness was readily deduced since k could be said to correspond<br />

to the diameter <strong>of</strong> the sand grains. Such uniform artificial roughness is, <strong>of</strong>

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