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Hydro-ecological relations in the Delta Waters

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Plan, <strong>the</strong>n it is apparent tbt <strong>the</strong> separatian of <strong>the</strong> Grwel<strong>in</strong>gen and<br />

Eastern Scheldt estuaries occurred prior to <strong>the</strong> peak polluttan years of<br />

<strong>the</strong> early seventies. The formation of sedimentation regians I and 11, a<br />

result of <strong>the</strong> closure of <strong>the</strong> Rarhgvliet, took place hediately before<br />

<strong>the</strong> major wave of pollution occurred, while sedimentation rsgion 111,<br />

wbich d l be created by <strong>the</strong> fluehiq operatians of Lake Zoom, will be<br />

affected now that contamLRatiDn levels have been greatly reduced.<br />

Figure 4<br />

Associated cadmium <strong>in</strong> suspended river sedimeots ar <strong>the</strong> po<strong>in</strong>ts<br />

where <strong>the</strong> rivers Rh<strong>in</strong>e, Meuse and Scheldt cross <strong>the</strong> border

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