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• W2149083610 abstract "Fire directly releases carbon (C) to the atmosphere through combustion of biomass. An estimated 1470 ± 59 km 2 of peatland burns annually in boreal, western Canada, releasing 4.7 ± 0.6 Tg C to the atmosphere via direct combustion. We quantified within-site variation in organic matter lost via combustion in a bog peatland in association with the 116 000-ha Chisholm, Alberta, fire in 2001. We hypothesized that for peatlands with considerable small-scale microtopography (bogs and treed fens), hummocks will burn less than hollows. We found that hollows exhibit more combustion than hummocks, releasing nearly twice as much C to the atmosphere. Our results suggest that spatial variability in species composition and site hydrology within a landform and across a landscape could contribute to considerable spatial variation in the amounts of C released via combustion during peatland fire, although the magnitude of this variation may be dependent on fire severity." @default.
• W2149083610 created "2016-06-24" @default.
• W2149083610 creator A5041125469 @default.
• W2149083610 creator A5054063389 @default.
• W2149083610 date "2003-12-01" @default.
• W2149083610 modified "2023-09-30" @default.
• W2149083610 title "Variability in organic matter lost by combustion in a boreal bog during the 2001 Chisholm fire" @default.
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• W2149083610 doi "https://doi.org/10.1139/x03-162" @default.
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