Little effects on soil organic matter chemistry of density fractions after seven years of forest soil warming

Rising temperatures enhance microbial decomposition of soil organic matter (SOM) and thereby increase the soil CO(2) efflux. Elevated decomposition rates might differently affect distinct SOM pools, depending on their stability and accessibility. Soil fractions derived from density fractionation hav...

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Detalles Bibliográficos
Autores principales: Schnecker, Jörg, Borken, Werner, Schindlbacher, Andreas, Wanek, Wolfgang
Formato: Online Artículo Texto
Lenguaje:English
Publicado: 2016
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5198888/
https://www.ncbi.nlm.nih.gov/pubmed/28042178
http://dx.doi.org/10.1016/j.soilbio.2016.09.003

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5198888/
https://www.ncbi.nlm.nih.gov/pubmed/28042178
http://dx.doi.org/10.1016/j.soilbio.2016.09.003

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