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 CO(2) 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...

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Detalles Bibliográficos
Autores principales: Schrumpf, Marion, Kaiser, Klaus, Schulze, Ernst-Detlef
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Public Library of Science 2014
Materias:
Research Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3930723/
https://www.ncbi.nlm.nih.gov/pubmed/24586720
http://dx.doi.org/10.1371/journal.pone.0089364

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3930723/
https://www.ncbi.nlm.nih.gov/pubmed/24586720
http://dx.doi.org/10.1371/journal.pone.0089364

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