Alpine grassland soils contain large proportion of labile carbon but indicate long turnover times
Alpine soils are expected to contain large amounts of labile carbon (C) which may become a further source of atmospheric carbon dioxide (CO<sub>2</sub>) as a result of global warming. However, there is little data available on these soils, and understanding of the influen...
| Main Authors: | , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2011-07-01
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| Series: | Biogeosciences |
| Online Access: | http://www.biogeosciences.net/8/1911/2011/bg-8-1911-2011.pdf |