Nitrex: The timing of response of coniferous forest ecosystems to experimentally-changed nitrogen deposition
| Autor: | Michael Bredemeier, Bridget A. Emmett, A.W. Boxman, Richard F. Wright, O.J. Kjønaas, Jan G. M. Roelofs, Arne O. Stuanes, Hans Hultberg, N. van Breemen, Per Gundersen, Filip Moldan, Albert Tietema, Patrick Schleppi, K. Blanck |
|---|---|
| Rok vydání: | 1995 |
| Předmět: |
0106 biological sciences
Nitrogen deposition Hydrology Environmental Engineering 010504 meteorology & atmospheric sciences Environmental change Ecological Modeling chemistry.chemical_element 15. Life on land 010603 evolutionary biology 01 natural sciences Pollution Nitrogen Deposition (aerosol physics) Nutrient chemistry 13. Climate action Environmental chemistry Forest ecology Environmental Chemistry Environmental science Ecosystem Saturation (chemistry) 0105 earth and related environmental sciences Water Science and Technology |
| Zdroj: | Water, Air & Soil Pollution, 85, 3, pp. 1623-1628 Water, Air & Soil Pollution, 85, 1623-1628. Kluwer academic publ |
| ISSN: | 1573-2932 0049-6979 |
| DOI: | 10.1007/bf00477212 |
| Popis: | 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. |
| Databáze: | OpenAIRE |
| Externí odkaz: |
|
Full text from SpringerLink