Abstract
Using variations of the BPI model by Cole & Cloern (1987), primary production in the Scheldt Estuary’s two contrasting regions (Oosterschelde and Westerschelde) was first modelled using in-situ values and calibrated for. Primary production was successfully modelled using in-situ values, returning r2 values of 0.75 and 0.89 for the Oosterschelde
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