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Model analysis of the effects of soil age, fires and harvesting on the carbon storage of boreal forest soils
Author(s) -
LISKI J.,
ILVESNIEMI H.,
MÄKELÄ A.,
STARR M.
Publication year - 1998
Publication title -
european journal of soil science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.244
H-Index - 111
eISSN - 1365-2389
pISSN - 1351-0754
DOI - 10.1046/j.1365-2389.1998.4930407.x
Subject(s) - chronosequence , taiga , soil water , environmental science , boreal , soil carbon , soil science , decomposition , agronomy , forestry , ecology , geography , biology
Summary Potential causes for changes in the amounts of carbon (C) stored in the soils of boreal forests were studied by measuring the C in the soil along a 5000‐year chronosequence in coastal western Finland and using a simple dynamic model of decomposition. The amount of soil C stabilized at an age of about 2000 years. This suggests that the youth of many boreal soils does not make them sinks for atmospheric C. Simulated repeated fires kept the amount of soil C reduced by about 25%, but if fires were prevented then the C in the soil increased. Stored C may thus be less than the potential storage where fires are frequent, and it could be increased by preventing fires. Simulated clear‐cutting caused a temporary 5–10% decrease in the amount of soil C over a 20‐year period after the harvesting. It also caused a long‐term decrease in the amount of soil C such that, after two 100‐year rotations, the amount had been decreased by 14%. Stored C is almost certainly less than the potential storage and decreasing where forests are harvested.