Abstract
Nitrogen dynamics in semi-natural environments is crucial for the development and ecological
stability of these systems. The present paper shows the results of the reinvestigation of a 15N-tracer
experiment, which was established in the Grossglockner massif in Austria at 2300ma.s.l. in 1974=1975.
We show that large quantities of nitrogen introduced by a single pulse labelling (amounting to approximately
1.7% of the nitrogen in the system) into an alpine grassland remain in the soil-plant system, with
only 55% being lost during 27-28 years. In the first 10 cm of the four investigated soil profiles 40% of 15N
was recovered, being mainly bound in organic forms. A simple site specific model was established on the
basis of the results considering a biological, residual and labile N-pool, the latter being the source for
N-losses. By the model a long mean residence time close to 100 years was derived for the remaining 15N.
Originalsprache | Englisch |
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Seiten (von - bis) | 1-11 |
Seitenumfang | 11 |
Fachzeitschrift | Biogeochemistry |
Volume | 0 |
Publikationsstatus | Veröffentlicht - 2003 |
Research Field
- Nicht definiert
Schlagwörter
- Alpine grassland
- Cambisol
- 15N
- N dynamics
- N-pools