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Conclusions
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•A
reduction of 50% of the discharge of nitrate
from the rivers Mondego e Pranto
shown that the has no consequences in
terms of trophic activity, reducing the
concentrations of nitrate in the estuary, but
not the production of phytoplankton. This is a
consequence of the limitation growth by the
residence time.
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•The
results have shown also that the “bay behaviour”
of the southern channel induces the deposition
of particulate organic matter in the channel and
the consequent enrichment of the sediments,
enhancing the conditions for the development of
macro-algae. The growth of these algae is also
facilitated by the low values of the velocity. A
sensitivity study of the hydrodynamics of that
channel to the re-opening of the communication
between the channels was performed and it was
verified that it clearly modifies the flow.
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