Article
Temperature sensitivity of organic matter decomposition of permafrost-region soils during laboratory incubations
2016-06-01
Abstract excerpt
Permafrost soils contain more than 1300 Pg of carbon (C), twice the amount of C in the atmosphere. Temperatures in higher latitudes are increasing, inducing permafrost thaw and subsequent microbial decomposition of previously frozen C, which will most likely feed back to climate warming through release of the greenhouse gases CO2 and CH4. Understanding the temperature sensitivity (Q10) and dynamics of soil organic...
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Identifiers and source
- Literature Corpus work
- 6ac2a29c-a124-51da-9e8c-44a038b2453b
- DOI
- 10.1016/j.soilbio.2016.02.008
