Influence of freeze-thaw events on carbon dioxide emission from soils at different moisture and land use

BACKGROUND: The repeated freeze-thaw events during cold season, freezing of soils in autumn and thawing in spring are typical for the tundra, boreal, and temperate soils. The thawing of soils during winter-summer transitions induces the release of decomposable organic carbon and acceleration of soil...

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Detalles Bibliográficos
Autores principales: Kurganova, Irina, Teepe, Robert, Loftfield, Norman
Formato: Texto
Lenguaje:English
Publicado: BioMed Central 2007
Materias:
Research
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC1808452/
https://www.ncbi.nlm.nih.gov/pubmed/17309792
http://dx.doi.org/10.1186/1750-0680-2-2

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC1808452/
https://www.ncbi.nlm.nih.gov/pubmed/17309792
http://dx.doi.org/10.1186/1750-0680-2-2

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