Abstract

Relationships between runoff and water quality from the 1960s to the present time were studied in two adjacent, almost undisturbed forested catchments (Teeressuonoja, 0.69 km 2, and Yli-Knuutila, 0.07 km 2) in southern Finland. The concentrations of nitrate-nitrogen (NO 3N) in stream-water have clearly increased in both the catchments during the last 20–25 years. In Yli-Knuutila, the volume-weighted average concentration of NO 3N increased over twofold, from 580 μgl −1 in 1969–1979 to 1350 μgl −1 in 1980–1990. In Teeressuonoja, the nitrate levels were lower but the increasing trend was comparable with that of Yli-Knuutila. The largest increase of concentrations of NO 3N occurred from the mid-1970s to the mid-1980s. The total nitrogen stream-water output of Yli-Knuutila increased almost threefold, from 1.1 kg N ha −1 year −1 in 1969–1979 to 2.9 kg N ha −1 year −1 in 1980–1990. The average proportion of the NO 3N output of the total nitrogen output increased during the same period from 56% to 68%. The mean annual inorganic deposition of nitrogen increased from 6.2 kg ha −1 year −1 in 1971–1979 to 8.5 kg ha −1 year −1 in 1980–1990. Decreasing retention was reflected in the input-output budget of inorganic N at Yli-Knuutila; output divided by input increased from 12% during the 1970s to 24% during the 1980s. Increased leaching in the Yli-Knuutila and Teeressuonoja catchment streams indicates the effects of increased nitrogen deposition. The increase in nitrate leaching in Yli-Knuutila, particularly during the summer months, provides evidence of nitrogen saturation and the inability of the biomass to utilize the N available, whereas increase during snowmelt and the autumn period indicates the impact of N deposition.

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