Effects of fire and fire-induced changes in soil properties on post-burn soil respiration

Journal Article · 30 September 2024 · Fire Ecology (Online)

DOI: https://doi.org/10.1186/s42408-024-00328-1 · OSTI ID:2462857

Johnson, Dana B. ^[1]; Yedinak, Kara M. ^[2]; Sulman, Benjamin N. ^[3]; Berry, Timothy D. ^[1]; Kruger, Kelsey ^[1]; Whitman, Thea  ^[1]

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1. Univ. of Wisconsin, Madison, WI (United States)
2. USDA Forest Service, Madison, WI (United States). Forest Products Laboratory (FPL)
3. Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States)

Boreal forests cover vast areas of land in the northern hemisphere and store large amounts of carbon (C) both aboveground and belowground. Wildfires, which are a primary ecosystem disturbance of boreal forests, affect soil C via combustion and transformation of organic matter during the fire itself and via changes in plant growth and microbial activity post-fire. Wildfire regimes in many areas of the boreal forests of North America are shifting towards more frequent and severe fires driven by changing climate. As wildfire regimes shift and the effects of fire on belowground microbial community composition are becoming clearer, there is a need to link fire-induced changes in soil properties to changes in microbial functions, such as respiration, in order to better predict the impact of future fires on C cycling. We used laboratory burns to simulate boreal crown fires on both organic-rich and sandy soil cores collected from Wood Buffalo National Park, Alberta, Canada, to measure the effects of burning on soil properties including pH, total C, and total nitrogen (N). We used 70-day soil incubations and two-pool exponential decay models to characterize the impacts of burning and its resulting changes in soil properties on soil respiration. Laboratory burns successfully captured a range of soil temperatures that were realistic for natural wildfire events. We found that burning increased pH and caused small decreases in C:N in organic soil. Overall, respiration per gram total (post-burn) C in burned soil cores was 16% lower than in corresponding unburned control cores, indicating that soil C lost during a burn may be partially offset by burn-induced decreases in respiration rates. Simultaneously, burning altered how remaining C cycled, causing an increase in the proportion of C represented in the modeled slow-cycling vs. fast-cycling C pool as well as an increase in fast-cycling C decomposition rates. Together, our findings imply that C storage in boreal forests following wildfires will be driven by the combination of C losses during the fire itself as well as fire-induced changes to the soil C pool that modulate post-fire respiration rates. Moving forward, we will pair these results with soil microbial community data to understand how fire-induced changes in microbial community composition may influence respiration.

• Research Organization: Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States)
• Sponsoring Organization: USDOE
• Grant/Contract Number: AC05-00OR22725; SC0021022
• OSTI ID: 2462857
• Journal Information: Fire Ecology (Online), Journal Name: Fire Ecology (Online) Journal Issue: 1 Vol. 20; ISSN 1933-9747
• Publisher: Association for Fire Ecology (AFE)Copyright Statement
• Country of Publication: United States
• Language: English