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Hydro-ecological relations in the Delta Waters

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less predictable for water managers; <strong>the</strong> Veerse Meex is an eraple of<br />

phase 11.<br />

Relative dorn<strong>in</strong>once<br />

l SALT WATER I /<br />

I<br />

n<br />

I II m<br />

EutPophlccltion phase<br />

Figure 8 Tentative model for <strong>the</strong> relation between primary producers<br />

and nutriats and <strong>the</strong> snccessive stages <strong>in</strong> <strong>the</strong> eutmphication<br />

proce6s. Explanation see text.<br />

In hypereutrophicated systems (phase 111) heavy uncontrolled<br />

phytoplilnkton blooms alternate with mass growth of macro-algae.<br />

Nutrient concentrations are cont<strong>in</strong>uously high. Root<strong>in</strong>g waterplants hwe<br />

completely disappeared. Bottom sediments suffer from permanent anoxia.<br />

The lagoon of Venice is an example of phase 111, where E bimass<br />

-2<br />

reaches values of 1.5 kg dry weight m (Sfriso, et al. 1987; Sfriso,<br />

et al. 1988) which is 6 times higher as <strong>in</strong> <strong>the</strong> Veerse Meer.

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