Hydro-ecological relations in the Delta Waters
Hydro-ecological relations in the Delta Waters
Hydro-ecological relations in the Delta Waters
Create successful ePaper yourself
Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.
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.