Groundwater connectivity controls peat burn severity in the boreal plains

Author:

Hokanson K. J.12,Lukenbach M. C.1,Devito K. J.2,Kettridge N.3,Petrone R. M.4,Waddington J. M.

Affiliation:

1. School of Geography and Earth Sciences; McMaster University; Hamilton ON L8S 4K1 Canada

2. Department of Biological Sciences; University of Alberta; Edmonton AB T6G 2E3 Canada

3. School of Geography, Earth and Environmental Sciences; University of Birmingham; Edgbaston Birmingham B15 2TT UK

4. Department of Geography and Environmental Management; University of Waterloo; Waterloo ON N2L 3C5 Canada

Funder

Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada

Publisher

Wiley

Subject

Earth-Surface Processes,Ecology,Aquatic Science,Ecology, Evolution, Behavior and Systematics

Reference54 articles.

1. Interactive effects of vegetation, soil moisture and bulk density on depth of burning of thick organic soils;Benscoter;International Journal of Wildland Fire,2011

2. Variability in organic matter lost by combustion in a boreal bog during the 2001 Chisholm fire;Benscoter;Canadian Journal of Forest Research,2003

3. Carbon turnover in peatland mesocosms exposed to different water table levels;Blodau;Biogeochemistry,2004

4. Quantifying fire severity, carbon, and nitrogen emissions in Alaska's boreal forest;Boby;Ecological Applications,2010

5. Bothe RA Abraham C 1993 Evaporation and evapotranspiration in Alberta 1986 to 1992 addendum

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