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A moisture function of soil heterotrophic respiration that incorporates microscale processes
Soil heterotrophic respiration (HR) is an important source of soil-to-atmosphere CO(2) flux, but its response to changes in soil water content (θ) is poorly understood. Earth system models commonly use empirical moisture functions to describe the HR–θ relationship, introducing significant uncertaint...
| Autores principales: | , , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2018
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6028431/ https://www.ncbi.nlm.nih.gov/pubmed/29967415 http://dx.doi.org/10.1038/s41467-018-04971-6 |