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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...
| Autores principales: | , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Public Library of Science
2015
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| Materias: | |
| 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 |