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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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| Publicado no: | PLoS One |
|---|---|
| Main Authors: | , , , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Public Library of Science
2015
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4437981/ https://ncbi.nlm.nih.gov/pubmed/25992875 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1371/journal.pone.0123774 |
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