Freeze–thaw cycles have minimal effect on the mineralisation of low molecular weight, dissolved organic carbon in Arctic soils

Warmer winters in Arctic regions may melt insulating snow cover and subject soils to more freeze–thaw cycles. The effect of freeze–thaw cycles on the microbial use of low molecular weight, dissolved organic carbon (LMW-DOC) is poorly understood. In this study, soils from the Arctic heath tundra, Arc...

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Detalles Bibliográficos
Autores principales: Foster, A., Jones, D. L., Cooper, E. J., Roberts, P.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Springer Berlin Heidelberg 2016
Materias:
Original Paper
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7346978/
https://www.ncbi.nlm.nih.gov/pubmed/32669755
http://dx.doi.org/10.1007/s00300-016-1914-1

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7346978/
https://www.ncbi.nlm.nih.gov/pubmed/32669755
http://dx.doi.org/10.1007/s00300-016-1914-1

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