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We studied the nitrogen retention capacity of six peatland buffer areas constructed in forested catchments in southern and central Finland. The buffers (0.1-4.9% of the total catchment area) were either undrained mires or drained peatlands rewetted 4-7 years before the present study. The N retention capacity was studied by adding ammonium nitrate (NH 4 NO 3 -N) solution into the inflow waters of the buffers once (one area) or twice (five areas) during a period of 4-6 years. Except for the first N addition in one area, the three largest buffer areas (relative size [ 1%) retained the added inorganic N almost completely; their retention efficiencies during the year of addition were [93% for both NO 3 -N and NH 4 -N. Two of the three small buffers (relative size \ 0.25%) were also able to reduce inorganic N from the through-flow waters effectively; their retention capacities for inorganic nitrogen varied between 58 and 89%. However, one small buffer area had a retention capacity of only \20%. The factors contributing to efficient N retention were hydrological load during N addition, relative size of the buffer area, and its length, i.e. the distance between the inflow and outflow points. If there was any release of the added N, it mostly occurred within a relatively short-time period (\100 days) after the treatment. The buffer areas appeared to be efficient and longterm sinks for inorganic nitrogen because the release of N during the 2-4 years after N addition was minor.