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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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Literature Corpus work
6ac2a29c-a124-51da-9e8c-44a038b2453b
DOI
10.1016/j.soilbio.2016.02.008
Open publication

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Temperature sensitivity of organic matter decomposition of permafrost-region soils during laboratory incubationsDOI 10.1016/j.soilbio.2016.02.008
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