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...

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Detalles Bibliográficos
Autores principales: Yan, Zhifeng, Bond-Lamberty, Ben, Todd-Brown, Katherine E., Bailey, Vanessa L., Li, SiLiang, Liu, CongQiang, Liu, Chongxuan
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
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

Internet

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

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