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Membrane and Desalination Technologies - TCE Moodle Website

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122 L. Song <strong>and</strong> K.Guan Tay<br />

Permeate flux (m/s)<br />

1.6×10 –5<br />

1.4×10 –5<br />

1.2×10 –5<br />

1.0×10 –5<br />

8.0×10 –6<br />

6.0×10 –6<br />

4.0×10 –6<br />

2.0×10 –6<br />

0<br />

25<br />

50<br />

75<br />

100<br />

0.0<br />

0 1 2 3 4 5 6<br />

Distance from channel entrance (m)<br />

Fig. 3.14. Evolvement of evenly distributed permeate flux profile of the membrane channel with time.<br />

The reason for the decline in permeate flux along the membrane channel in Fig. 3.14 is the<br />

build-up of salt concentration as water is lost as permeate when the feed water travels along<br />

the channel. Figure 3.15 shows the variation of salt concentration along the membrane<br />

channel at different times. At the start of the operation, salt concentration is seen to increase<br />

along the membrane channel until the point about 4.5 m from the channel entrance, where it<br />

remains unchanged for the rest of the channel. The increase in salt concentration increases the<br />

osmotic pressure <strong>and</strong> reduces the net driving pressure. However, there is a limit for the salt<br />

concentration in the membrane channel. When the osmotic pressure reaches the driving<br />

pressure at some point in the membrane channel, salt concentration ceases to increase.<br />

Crossflow velocity is found in Fig. 3.16 to decrease along the channel due to water loss.<br />

Like the permeate flux <strong>and</strong> membrane resistance, the variations of both salt concentration <strong>and</strong><br />

crossflow velocity along the membrane channel became more moderate as fouling continues<br />

to develop in the membrane system.<br />

The changes in the patterns of the localized membrane resistance, permeate flux, salt<br />

concentration, <strong>and</strong> crossflow velocity in Figs. 3.13–3.16 give strong evidence that membrane<br />

fouling is occurring in the membrane channel. However, the initial stage of membrane<br />

fouling does not affect the average permeate flux of a long membrane channel. The length<br />

of the initial period of constant average flux is strongly affected by the driving pressure<br />

employed in the membrane process. The average permeate flux of the same membrane<br />

channel (using parameters given in Table 3.3) is simulated for two driving pressures of<br />

1.21 10 8 <strong>and</strong> 1.38 10 8 <strong>and</strong> the results are shown in Fig. 3.17. It can be seen that the 15%

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