Microscale Heterogeneity Explains Experimental Variability and Non-Linearity in Soil Organic Matter Mineralisation

Soil respiration represents the second largest CO(2) flux from terrestrial ecosystems to the atmosphere, and a small rise could significantly contribute to further increase in atmospheric CO(2). Unfortunately, the extent of this effect cannot be quantified reliably, and the outcomes of experiments d...

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Detalles Bibliográficos
Autores principales: Falconer, Ruth E., Battaia, Guillaume, Schmidt, Sonja, Baveye, Philippe, Chenu, Claire, Otten, Wilfred
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Public Library of Science 2015
Materias:
Research Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4437981/
https://www.ncbi.nlm.nih.gov/pubmed/25992875
http://dx.doi.org/10.1371/journal.pone.0123774

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4437981/
https://www.ncbi.nlm.nih.gov/pubmed/25992875
http://dx.doi.org/10.1371/journal.pone.0123774

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