Sediment core samples were collected in the largest urban Lake Donghu (Stations I and II) in China, and the activities of 210 Pb, 226 Ra and 137 Cs were measured by gamma-ray spectrometry. The sedimentation rates, calculated by 210 Pb constant rate of supply (CRS) model, ranged from 0.11 to 0.65 (average 0.39) cm . y -1 at Station I, and from 0.21 to 0.78 (average 0.46) cm . y -1 at Station II. Sedimentation rate calculated by 137 Cs as a time marker was 0.55 cm . y -1 at Station II. Based on the average sedimentation rate, we obtained 769 and 147 t . y -1 for nitrogen and phosphorus retentions in Lake Donghu sediments, respectively.