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Soil Carbon stocks and their rates of accumulation and loss in a boreal forest landscape
Author(s) -
Rapalee Gloria,
Trumbore Susan E.,
Davidson Eric A.,
Harden Jennifer W.,
Veldhuis Hugo
Publication year - 1998
Publication title -
global biogeochemical cycles
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.512
H-Index - 187
eISSN - 1944-9224
pISSN - 0886-6236
DOI - 10.1029/98gb02336
Subject(s) - environmental science , taiga , moss , boreal , soil water , sink (geography) , peat , soil carbon , soil horizon , ecosystem , wetland , hydrology (agriculture) , soil science , ecology , geology , forestry , geography , cartography , geotechnical engineering , biology
Boreal forests and wetlands are thought to be significant carbon sinks, and they could become net C sources as the Earth warms. Most of the C of boreal forest ecosystems is stored in the moss layer and in the soil. The objective of this study was to estimate soil C stocks (including moss layers) and rates of accumulation and loss for a 733 km 2 area of the BOReal Ecosystem‐Atmosphere Study site in northern Manitoba, using data from smaller‐scale intensive field studies. A simple process‐based model developed from measurements of soil C inventories and radiocarbon was used to relate soil C storage and dynamics to soil drainage and forest stand age. Soil C stocks covary with soil drainage class, with the largest C stocks occurring in poorly drained sites. Estimated rates of soil C accumulation or loss are sensitive to the estimated decomposition constants for the large pool of deep soil C, and improved understanding of deep soil C decomposition is needed. While the upper moss layers regrow and accumulate C after fires, the deep C dynamics vary across the landscape, from a small net sink to a significant source. Estimated net soil C accumulation, averaged for the entire 733 km 2 area, was 20 g C m −2 yr −1 (28 g C m −2 yr −1 accumulation in surface mosses offset by 8 g C m −2 yr −1 lost from deep C pools) in a year with no fire. Most of the C accumulated in poorly and very poorly drained soils (peatlands and wetlands). Burning of the moss layer in only 1% of uplands would offset the C stored in the remaining 99% of the area. Significant interannual variability in C storage is expected because of the irregular occurrence of fire in space and time. The effects of climate change and management on fire frequency and on decomposition of immense deep soil C stocks are key to understanding future C budgets in boreal forests.