NITREX: the timing of response of coniferous forest ecosystems to experimentally-changed nitrogen deposition

• Published in: WATER, AIR, & SOIL POLLUTION Vol. 85; no. 3; pp. 1623 - 1628
• Main Authors: Tietema, A, Wright, R.F, Blanck, K, Boxman, A.W, Bredemeier, M, Emmett, B.A, Gundersen, P, Hultberg, H, Kjonaas, O.J, Moldan, F
• Format: Journal Article Conference Proceeding
• Language: English
• Published: Dordrecht Springer 1995
• Subjects: air pollution; ammonium compounds; Animal, plant and microbial ecology; Applied ecology; biogeochemical cycles; Biological and medical sciences; conifer needles; coniferous forests; deposition; duration; Ecotoxicology, biological effects of pollution; environmental impact; forest soils; Fundamental and applied biological sciences. Psychology; magnesium; mineral content; mineralization; nitrogen; nutrient content; potassium; responses; runoff; simulation; soil chemistry; soil fertility; soil pollution; soil solution; Terrestrial environment, soil, air; throughfall; water quality; Scandinavia; Western European region; Europe; Forests; Saturation; Microflora; Forest soil; Atmospheric deposition; Nitrogen; Disturbed ecosystem; Mineralization; Vegetation; Nutrient; Models; Soil plant relation; Soil solution; Material balance; Coniferous forest
• ISSN: 0049-6979; 1573-2932
• DOI: 10.1007/BF00477212

In large regions of Europe and eastern North America atmospheric deposition of inorganic nitrogen (N) compounds has greatly increased the natural external supply to forest ecosystems. This leads to N saturation, in which availability of inorganic N is in excess of biological demand and the ecosystem is unable to retain all incoming N. The large-scale experiments of the NITREX project (NITRogen saturation EXperiments) are designed to provide information regarding the patterns and rates of responses of coniferous forest ecosystems to increases in N deposition and the reversibility and recovery of impacted ecosystems following reductions in N deposition. The timing of ecosystem response generally followed a hypothesized "cascade of response". In all sites N outputs have responded markedly but to very different degrees within the first three years of treatment. Within this time significant effects on soil processes and on vegetation have only been detected at two sites. This delayed response is explained by the large capacity of the soil system to buffer the increased N supply by microbial immobilization and adsorption. We believe that this concept provides a framework for the evaluation and prediction of the ecosystem response to environmental change.