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The likely direction of change in soil organic carbon (SOC) in the boreal forest biome, which harbors roughly 22% of the global soil carbon pool, is of marked concern because climate warming is projected to be greatest in high latitudes and temperature is the cardinal determinant of soil C mineralization. Moreover, the majority of boreal forest SOC is harbored in surficial organic horizons which are the most susceptible to consumption in wildfire. This research focuses on mechanisms of soil C accumulation in recently burned (2004) and unburned (61850-1950) black spruce (Picea mariana [Mill.] BSP) forests along gradients in stand productivity and soil temperature. The primary research questions in these three chapters...
    map background search result map search result map Controls on ecosystem and root respiration across a permafrost and wetland gradient in interior Alaska Source water controls on the character and origin of dissolved organic matter in streams of the Yukon River basin, Alaska Seasonal ice and hydrologic controls on dissolved organic carbon and nitrogen concentrations in a boreal-rich fen Evaluation of the composite burn index for assessing fire severity in Alaskan black spruce forests The response of soil organic carbon of a rich fen peatland in interior Alaska to projected climate change Mechanisms of soil carbon stabilization in black spruce forests of interior Alaska: Soil temperature, soil water, and wildfire Recovery of Carbon Pools a Decade Following Wildfire in Black Spruce Forests of Interior Alaska: Effects of Soil Texture and Landscape Position Controls on ecosystem and root respiration across a permafrost and wetland gradient in interior Alaska Seasonal ice and hydrologic controls on dissolved organic carbon and nitrogen concentrations in a boreal-rich fen The response of soil organic carbon of a rich fen peatland in interior Alaska to projected climate change Recovery of Carbon Pools a Decade Following Wildfire in Black Spruce Forests of Interior Alaska: Effects of Soil Texture and Landscape Position Evaluation of the composite burn index for assessing fire severity in Alaskan black spruce forests Mechanisms of soil carbon stabilization in black spruce forests of interior Alaska: Soil temperature, soil water, and wildfire Source water controls on the character and origin of dissolved organic matter in streams of the Yukon River basin, Alaska