Soil surface CO<sub>2</sub> flux increases with successional time in a fire scar chronosequence of Canadian boreal jack pine forest

To fully understand the carbon (C) cycle impacts of forest fires, both C emissions during the fire and post-disturbance fluxes need to be considered. The latter are dominated by soil surface CO<sub>2</sub> flux (<i>F</i><sub>s</sub>), which is still subject to lar...

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Bibliographic Details
Main Authors: J. Curry, J. Studens, T. J. Lynham, G. N. Mottram, G. Hartley, M. J. Wooster, H. Balzter, J. D. Kaduk, D. R. Smith, B. J. Stocks
Format: Article
Language:English
Published: Copernicus Publications 2010-05-01
Series:Biogeosciences
Online Access:http://www.biogeosciences.net/7/1375/2010/bg-7-1375-2010.pdf