Nitrogen (N) concentrations and stable N isotope abundances (d 15 N) of common reed (Phragmites australis) planted in a constructed wetland were measured periodically between July 2001 and May 2002 to examine their seasonal variations in relation to N uptake and N translocation within common reed. Nitrogen concentrations in P. australis shoots were higher in the growing stage (7.5 to 24.8 g N kg 21 ) than in the senescence stage (4.2 to 6.8 g N kg 21 ), indicating N translocation from shoots to rhizomes. Meanwhile, the corresponding d 15 N values were higher in the senescence stage (þ12.2 to þ22.4‰) than in the growing stage (þ5.1 to þ11.3‰). Coupled with the negative correlation (R 2 ¼ 0.24, P , 0.05, n ¼ 18) between N concentrations and d 15 N values of shoots in the senescence stage, our results suggested that shoot N became enriched in 15 N due to N isotopic fractionation (with an isotopic fractionation factor, a s/p , of 1.012) during N translocation to 2719 rhizomes. However, the positive correlation between N concentrations and d 15 N values in the growing stage (R 2 ¼ 0.19, P , 0.001, n ¼ 54) suggested that P. australis relies on N re-translocated from rhizome in the early growing stage and on mineral N in the sediment during the active growing stage. Therefore, seasonal d 15 N variations provide N-isotopic evidence of N translocation within and N uptake from external N sources by common reed.