Abstract
Existing phosphorus retention models are shown to overestimate retention in lakes where the areal water load (qs) is < 10 m/yr, thereby leading to low predictions of phosphorus concentration. This is caused, in part, by inconsistent assumptions in the overall modeling sequence. New empirical equations are presented that give better predictions of phosphorus for lakes with qs < 10 m, and equally good predictions for lakes with qs > 10 m. Key words: retention, phosphorus, empirical model, areal water load