For the pipeline and conditions described in Example 6.9, calculate the mean velocity using the Manning equation.
V = ({0.397}/{n}) D^{{2}/{3}} S_{F}^{{1}/{2}} (6.24)
The pipe is described as ‘smooth’ so use a low concrete roughness value from Table 8.1, say n = 0.012 {s}/{m^{{1}/{3}}} (for rough concrete use a higher value). As before, D = 1.2 m and S_{F} = 1 in 250 = 0.004.
V = ({0.397}/{0.012}) \times 1.2^{{2}/{3}} \times 0.004^{{1}/{2}}V = 2.361 m/s
In Example 6.9, the Colebrook-White equation gave V = 2.363 m/s. The simple Manning equation gives almost the same answer, although it obviously depends upon the assumed value of n.
Table 8.1 Typical values of Manning’s n for different types of surface | ||
Conduit type, surface roughness and channel alignment | n(s/m^{{1}/{3}}) | |
Canals | Earth, straight | 0.018 – 0.025 |
Earth, meandering | 0.025 – 0.040 | |
Rock, straight | 0.025 – 0.045 | |
Lined | Perspex | 0.009 |
channels | Glass | 0.009 – 0.010 |
Cement mortar | 0.011 – 0.015 | |
Concrete | 0.012 – 0.017 | |
Dressed, jointed stone | 0.013 – 0.020 | |
Swale | Water depth ≤ height of grass | 0.250 |
Water depth > height of grass | 0.100 | |
Rivers | Earth, straight | 0.020 – 0.025 |
Earth, poor alignment | 0.030 – 0.050 | |
Earth, with weeds and poor alignment | 0.050 – 0.150 | |
Stones 75 – 150 mm diameter, straight, good condition | 0.030 – 0.040 | |
Stones 75 – 150 mm diameter, poor alignment | 0.040 – 0.080 | |
Stones > 150 mm, boulders, steep slope, good condition | 0.040 – 0.070 | |
Floodplain | Short grass | 0.025 – 0.035 |
Long grass | 0.030 – 0.050 | |
Medium to dense brush, in winter | 0.045 – 0.110 | |
Pipes | Cast iron | 0.010 – 0.014 |
Concrete | 0.011 – 0.015 |