
Pump trip is an important case for simulation. The initial pressure
drop downstream of a pumping station can produce unacceptably low
pressures but also a subsequent upsurge after flow has reversed is an
important event which requires to be predicted.
In a pumping station containing only a solo duty pump, trip of the
pump will be analysed over the range of suction levels.
In a multi-pump installation wherein several duty pumps may be oper-
ating together it is important to simulate the effect of different numbers of
duty pumps being tripped, again using the pertinent suction levels.
For a multi-pump installation the total amount of stored energy in
rotating elements
1
2
I!
2
varies directly in proportion to the number of
pumps in operation, whereas the increase in flow rate produced by starting
of each additional pump diminishes. The available ‘stored’ energy in
rotating elements per unit of flow, increases as total flow increases.
Thus it is not always obvious which pumping circumstance will produce
the ‘worst case’ as far as the system as a whole is concerned.
When pumping head is relatively high, the deceleration of flow after
pumps are switched off takes place with minimum head downstream of
the pumps remaining above suction levels. In this case the check valves
on each operating pump delivery branch will shut as flow ceases and
starts to reverse. Consider the long water pipeline shown in Fig. 10.15.
Figure 10.16 shows the predicted head downstream of the pumping
station when both operating pumps are tripped simultaneously at
time ¼1 s, simulating a station ‘blackout’. No protection is included
and head falls by almost 200 m at the pumping station over 4 s. At
this time, check valves close on each pump delivery branch. The
head drop is approximately given by aV
o
=g, where V
o
is the initial
steady flow velocity in the rising main. However, head was predicted
to continue falling gradually until around 22 s when the effects of
wave reflections start to influence conditions. This further reduction
in piezometric level is a consequence of pipeline resistance and is a
similar effect to ‘attenuation’ as described in Chapter 7. At 5 km the
effects of pump trip are experienced around 5 s after trip and the
decline in head follows the same pattern as at the pumping station.
The influence of wave reflection is noticeable at around 10 s. At
10 km the falling head is arrested by operation of nearby air valves.
Many pumping systems, particularly sewage schemes, operate at more
modest head and the response of the pumps can be influenced by the
prevailing level in a wet well.
Consider the variations of head shown in Fig. 10.17, downstream of
pumps and part way along sewage rising mains. After all three operating
147
Pumps