Summary
A computer model of phytoplankton population dynamics is used to simulate artificial eutrophication of Canadian Shield experimental lake 227. The model predicts seston C, N, and P concentrations of 600–750, 40–50, and 1–3 μg/l before fertilization, and 3000–3500, 550–700, and 30–50 μg/l after weekly nutrient addition, in accord with actual findings (Schindler 1971 b). Simulations suggest that at nutrient loading rates and CO2 invasion rates measured in 227, N and P limited standing crop, but DIC concentrations affected plankton composition and species succession. Rates of nutrient addition three times higher than that used by Schindle produced carbon-limitation of phytoplankton standing crop. The high nutrient loading rates and low CO2 invasion rates necessary for this latter limitation, however, suggests that its natural occurrence should be unusual, but predictable.