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Discolouration in drinking water systems - TU Delft

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distribution network is on the smaller sized pipes, 150 mm and smaller, at which the house<br />

connections are made. In fact this is the <strong>water</strong> that actually enters the properties and is<br />

experienced by the customers. The colour of the l<strong>in</strong>es (red, blue and green) <strong>in</strong> this thesis are<br />

often used to represent the flow direction with red the upstream location, green the<br />

downstream location and blue somewhere <strong>in</strong> between.<br />

The first process presented <strong>in</strong> Fig 2-3 is settl<strong>in</strong>g of particles, represented by the decreas<strong>in</strong>g<br />

turbidity <strong>in</strong> the flow direction. With settl<strong>in</strong>g, particles are lost and that leads to a decrease <strong>in</strong><br />

turbidity <strong>in</strong> the flow direction. This phenomenon can often be observed when <strong>in</strong> the turbidity<br />

trace at the treatment plant irregularities occur. These can be the result of a backwash of filters<br />

or resuspension as result of a pump switch.<br />

The spikes <strong>in</strong> the turbidity can be used as natural tracers to monitor the residence time <strong>in</strong> a<br />

network. The peak values at each locations are used to identify the orig<strong>in</strong> of the <strong>water</strong> and that<br />

‘package’ of <strong>water</strong> can be followed through the network. This has proven to be a very<br />

powerful tool to actually measure the residence time without add<strong>in</strong>g tracers to the <strong>water</strong>.<br />

In Fig 2-4 the turbidity trace <strong>in</strong> the three locations are drawn <strong>in</strong> separate graphs. The three<br />

stylistic traces represent resuspension of particles manifested by local peaks <strong>in</strong> turbidity,<br />

<strong>in</strong>dependent of turbidity elsewhere <strong>in</strong> the network. Mostly the peaks <strong>in</strong> turbidity can be related<br />

to <strong>in</strong>creased velocity <strong>in</strong> the pipes, for <strong>in</strong>stance as result of a hydraulic <strong>in</strong>cident. In this case the<br />

resuspension is caused by the <strong>in</strong>creased flow dur<strong>in</strong>g the morn<strong>in</strong>g peak demand. The <strong>in</strong>crease<br />

starts at 7:00 AM or even earlier and ends after roughly three hours. Resuspension can be<br />

observed both <strong>in</strong> the transport network and <strong>in</strong> the distribution network, though <strong>in</strong> the transport<br />

network there are fewer and mostly lower spikes <strong>in</strong> turbidity. First, the variation <strong>in</strong> velocity <strong>in</strong><br />

the transport network is less than <strong>in</strong> the distribution network (Blokker et al., 2006), allow<strong>in</strong>g<br />

for a more regular settl<strong>in</strong>g and resuspension. Second, the sampl<strong>in</strong>g po<strong>in</strong>t is at the top of the<br />

pipe and usually some stratification of the resuspended sediment can be observed. This means<br />

that part of the resuspended sediment will not reach the measur<strong>in</strong>g po<strong>in</strong>t at the top of the pipe.<br />

The peaks <strong>in</strong> turbidity <strong>in</strong> the distribution network follow the household demand, with high<br />

peaks <strong>in</strong> the morn<strong>in</strong>g and vary<strong>in</strong>g peaks <strong>in</strong> the late afternoon and early even<strong>in</strong>g. The day<br />

peaks are also related to the weather conditions and the types of connections: <strong>in</strong> hot, dry<br />

weather <strong>in</strong> areas with gardens the peak <strong>in</strong> the even<strong>in</strong>g can be much larger compared to the<br />

morn<strong>in</strong>g peaks. That also expla<strong>in</strong>s why discolouration <strong>in</strong>cidents are often associated with<br />

extreme weather conditions.<br />

The graphs <strong>in</strong> Fig 2-5 are aga<strong>in</strong> separated for the three locations and present the turbidity trace<br />

that can be measured when active corrosion occurs. Active corrosion changes the <strong>water</strong><br />

quality (McNeill and Edwards, 2001). The typical pattern is that the turbidity <strong>in</strong> distribution<br />

pipes rises dur<strong>in</strong>g the night hours when the <strong>water</strong> stagnates because of low night use. In the<br />

morn<strong>in</strong>g hours the <strong>water</strong> consumption <strong>in</strong>creases, flush<strong>in</strong>g out <strong>water</strong> with an <strong>in</strong>creased<br />

turbidity. The rise <strong>in</strong> turbidity is caused by the particles that are released through the corrosion<br />

process. The phenomenon has also been observed when a stable corrosion products scale is<br />

damaged by aggressive clean<strong>in</strong>g action (Vreeburg, 1996). The typical difference between<br />

resuspension and corrosion is that with the resuspension phenomenon, the turbidity rises when<br />

demand <strong>in</strong>creases while with corrosion the turbidity drops with <strong>in</strong>creas<strong>in</strong>g demands. It can,<br />

however, be difficult to dist<strong>in</strong>guish the two processes <strong>in</strong> the case of a comb<strong>in</strong>ation of settl<strong>in</strong>g<br />

and resuspension <strong>in</strong> a distribution pipe. The pattern of fall<strong>in</strong>g and ris<strong>in</strong>g turbidity can look the<br />

same, but the difference is the tim<strong>in</strong>g of the peaks <strong>in</strong> turbidity. In the case of settl<strong>in</strong>g and<br />

resuspension the turbidity decreases <strong>in</strong> the night hours and <strong>in</strong>creases <strong>in</strong> the day hours, while <strong>in</strong><br />

the corrosion case this is just the other way around, with <strong>in</strong>creas<strong>in</strong>g turbidity <strong>in</strong> the night and a<br />

Measur<strong>in</strong>g methods - 15 -

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