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Hydro-ecological relations in the Delta Waters

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Figsrlre 7<br />

Changes <strong>in</strong> <strong>the</strong> cadrnrum contenr 08 <strong>the</strong> Bb<strong>in</strong>e vater W) and fn<br />

river bed sed<strong>in</strong>eat from <strong>the</strong> Aari~wlieE (K) over <strong>the</strong> period<br />

1971-1W.9<br />

As flush<strong>in</strong>g +pexasrions ere vnly sebeduled hc cBmaenc@ Sn 1981, <strong>the</strong><br />

quuli@ oZ <strong>the</strong>! eediwn2 <strong>in</strong> take &m is *=ill <strong>the</strong> as that faund <strong>in</strong><br />

o~het part$ of <strong>the</strong> Eastern 5cheldt. %wener, <strong>the</strong>ue ia a small area<br />

Wtnd trhe Volketaklocke wMch has been afteored by <strong>the</strong> <strong>in</strong>flw Q£<br />

water From tke Hollaxrds Dig. For water management purposes it h@% been<br />

decl&d tu re~ttic<strong>the</strong> fld<strong>in</strong>p; qerationw <strong>in</strong> Lake Zom to a miaimum<br />

(<strong>the</strong> sal<strong>in</strong>ity level <strong>in</strong> eke lake *ill not eiceed 4170 &l),<br />

<strong>the</strong> iuput of ppollutants.<br />

to reduce

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