Biotic soil-plant interaction processes explain most of hysteric soil CO(2) efflux response to temperature in cross-factorial mesocosm experiment

Ecosystem carbon flux partitioning is strongly influenced by poorly constrained soil CO(2) efflux (F(soil)). Simple model applications (Arrhenius and Q(10)) do not account for observed diel hysteresis between F(soil) and soil temperature. How this hysteresis emerges and how it will respond to variat...

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Detalles Bibliográficos
Autores principales: Dusza, Yann, Sanchez-Cañete, Enrique P., Galliard, Jean-François Le, Ferrière, Régis, Chollet, Simon, Massol, Florent, Hansart, Amandine, Juarez, Sabrina, Dontsova, Katerina, Haren, Joost van, Troch, Peter, Pavao-Zuckerman, Mitchell A., Hamerlynck, Erik, Barron-Gafford, Greg A.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2020
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6976568/
https://www.ncbi.nlm.nih.gov/pubmed/31969580
http://dx.doi.org/10.1038/s41598-019-55390-6

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6976568/
https://www.ncbi.nlm.nih.gov/pubmed/31969580
http://dx.doi.org/10.1038/s41598-019-55390-6

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