Soil organic carbon and total nitrogen gains in an old growth deciduous forest in Germany.
Temperate forests are assumed to be organic carbon (OC) sinks, either because of biomass increases upon elevated CO2 in the atmosphere and large nitrogen deposition, or due to their age structure. Respective changes in soil OC and total nitrogen (TN) storage have rarely been proven. We analysed OC,...
Tallennettuna:
| Päätekijät: | , , |
|---|---|
| Aineistotyyppi: | Artigo |
| Kieli: | Inglês |
| Julkaistu: |
Public Library of Science (PLoS)
2014-01-01
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| Sarja: | PLoS ONE |
| Linkit: | https://doi.org/10.1371/journal.pone.0089364 |
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