C. Humborg et al., A box model approach for a long-term assessment of estuarine eutrophication, Szczecin Lagoon, southern Baltic, J MAR SYST, 25(3-4), 2000, pp. 387-403
We develop a layered "box, model" to evaluate the major effects of estuarin
e eutrophication of the Szczecin lagoon which can be compared with integrat
ing measures (chlorophyll a (Chl a), sediment burial, sediment oxygen consu
mption (SOC), input and output of total. nutrient loads) and use it to hind
cast the period 1950-1996 (the years when major increase in nutrient discha
rges by the Oder River took place). The following state variables are used
to describe the cycling of the limiting nutrients (nitrogen and phosphorus)
: phytoplankton (Phy), labile and refractory detritus (D-N, D-Nref, D-P, D-
Pref), dissolved inorganic nitrogen (DIN), dissolved inorganic phosphorus (
DIP), and oxygen (O-2). The three layers of the model include two water lay
ers and one sediment layer. Decrease of the carrying capacity with respect
to the increased supply of organic matter of the system with advancing eutr
ophication over the period studied is parameterized by an exponential decre
ase of the sediment nitrogen fluxes with increasing burial, simulating chan
ging properties from moderate to high accumulating sediments. The seasonal
variation as well as the order of magnitude of nutrient concentrations and
phytoplankton stocks in the water column remains in agreement with recent o
bservations. Calculated annual mean values of nutrient burial of 193 mmol N
m(-2) a(-1) and 23 mmol P m(-2) a(-1) are supported by observed values fro
m geological sediment records. Estimated DIN remineralization in the sedime
nts between 100 and 550 mmol N m(-2) a(-1) corresponds to SOC measurements.
Simulated DIP release up to 60 mmol P m(-2) a(-1) corresponds to recent me
asurements. The conceptual framework presented here can be used for a seque
ntial box model approach connecting small estuaries like the Szczecin lagoo
n and the open sea, and might also be connected with river box models. (C)
2000 Elsevier Science B.V. All rights reserved.