The Scheldt, Gironde and Sado estuaries exhibit quite different characteris
tics regarding the annual river discharges, nutrient loads and oxygen condi
tions. Distribution patterns of nutrients, dissolved oxygen, suspended matt
er and chlorophyll a as well as the nutrient ratios and half saturation con
stants, allow the identification and comparison of specific processes. The
Scheldt emerges as the most eutrophic estuary being, in general, not nutrie
nt limited and functions as a source of phosphorus and nitrogen. Intense bi
ogeochemical processes take place in this system. The Sado is shown to be a
moderately productive system, the upper part being enriched in nutrients a
nd chlorophyll a and showing a tendency for oxygen depletion in summer. Dif
ferent factors seem to control phytoplankton production along the salinity
gradient: light regime landwards and nitrogen seawards. By contrast, the Gi
ronde does not show clearly the presence of sinks or sources regarding nutr
ients and exhibits a reduced productivity essentially controlled by turbidi
ty, The high amounts of particles seem also to be responsible for localized
processes such as phosphate sorption/desorption and silicate regeneration.
(C) 1999 Elsevier Science Ltd. All rights reserved.