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Hydro-ecological relations in the Delta Waters

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- In addition to exist<strong>in</strong>g management measures, <strong>the</strong>re may well be<br />

future scope for a creative nespome to <strong>the</strong> ways <strong>in</strong> wbicb salt,<br />

stagnant lakes function. Such steps might <strong>in</strong>clude <strong>in</strong>creas<strong>in</strong>g<br />

denitrification <strong>in</strong> erde~ to remom nitrogen from <strong>the</strong> system. Thi8<br />

might be achieved by <strong>in</strong>flueno<strong>in</strong>g nirrifieation and denitrification<br />

processes <strong>in</strong> <strong>the</strong> bed by meam of stratification. Ano<strong>the</strong>r<br />

possibility Would 6e to make use sf <strong>the</strong> natural process, whereby<br />

organisms which <strong>in</strong>habit <strong>the</strong> salt lake bed act as an essential<br />

fater <strong>in</strong> <strong>the</strong> regulation of nutrients. The passibilit~ pf us<strong>in</strong>g<br />

sui3 organisms as an active policy irtstrument could be<br />

<strong>in</strong>vestigated.<br />

The water <strong>in</strong> <strong>the</strong> <strong>Delta</strong> sues its major significance to <strong>the</strong> marpholegy<br />

of <strong>the</strong> bas<strong>in</strong>s. The hydraulia conditions of <strong>the</strong> tidal waters have given<br />

rise to a m~rphological structure and dynamics, which contribute to<br />

<strong>the</strong> probuctlvify iard diversity of <strong>the</strong>se regions. Gomparmentalization<br />

hs9 sparked af* a process of ~lorphol~&iical change, which will lead to<br />

mme UdEaoourable donditions <strong>in</strong> <strong>the</strong> clesed compartme?ats. On <strong>the</strong> othsz<br />

hma, <strong>the</strong> morpholog%eal changes along <strong>the</strong> coast - <strong>the</strong> creation of <strong>the</strong><br />

Voordella - shwld he regarded <strong>in</strong> a favortlable light, because:<br />

- The morphhetry Of estaaries provideo an ideal start<strong>in</strong>g po<strong>in</strong>t fa:<br />

mmimiir<strong>in</strong>g <strong>the</strong> developent potential of campartmentalized syst-ems.<br />

This applies paftlcnlarly to tbt peesenee of lac:@ areas of<br />

shallows and <strong>the</strong>ir gradual transition to t b hanks. It is essential<br />

to preselnre <strong>the</strong> morphwetry of such areas as much as posp~ihle if<br />

<strong>the</strong>ir potential is to be exploited. Considetable experience has<br />

been amassed <strong>in</strong> <strong>the</strong> <strong>Delta</strong> <strong>in</strong> <strong>the</strong> constructian of out@? hank<br />

defences;<br />

- It is possible to create new and valuable areas through <strong>in</strong>fluenc<strong>in</strong>g<br />

processis of seclireantation and erosion. Tha Voordelta is a good.<br />

albeit un<strong>in</strong>tentional, example of this. Sowever, it shoatd be<br />

poaslble, given present know-har and experience, consciously to<br />

create snch as by work<strong>in</strong>g <strong>in</strong> harmwny with nat.ural processes and<br />

eseahIishFng <strong>the</strong> right parsmeters. In lipe with this approach, ways<br />

are cuzrently be+<br />

<strong>in</strong>vestigated of <strong>in</strong>fluensisg mud flat and salt

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