Ria de Aveiro is a very important area of the Portuguese coast, which has been under an
increasing anthropogenic pressure, for several decades, contributing to the degradation of
the lagoon’s water quality.
A water quality model was applied to predict concentrations of inorganic nutrients,
chlorophyll-a, and dissolved oxygen (DO) in the Ria de Aveiro lagoon, Portugal. Both data
and modelling results point out that the DO distribution in the lagoon is controlled by tidal
transport processes. The DO distribution in the Ria de Aveiro seems to bemainly controlled
by tidal processes, as its concentration remains relatively high and close to sea values. The
far end of the lagoon, where the intertidal salt marshes are important, the DO concentration
is dominantly affected by re-aeration and the flooding/drying processes over the
intertidal salt marshes, the phytoplankton activity, the nitrification processes and oxidation
of the organic matter. These processes play an important role in the creation of the
summer hypoxic/anoxic situations, when primary production and advective transport are
low. Data and modelling results show strong relationship between nutrients and the CHL-a
concentrations during spring–summer, but weak during winter–spring, evidencing the light
and nutrients limiting effect during, respectively the last and the former period. High NO3
and NH4 concentrations or important spikes in the concentration precede or coincide, in
general, with the CHL-a increase. The main results concerning the DO evolution and distribution
demonstrate that a generalized eutrophication state is unlikely to occur within the
lagoon, except near its very far end, during summer and in a situation of high BOD concentrations.
The good connection between Ria de Aveiro lagoon and the sea and the circulation
pattern inside the lagoon are, therefore, responsible for relatively high level of oxygen water
content in the water column, throughout its main channels
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