Earth System Processes 2 (8–11 August 2005)

Paper No. 2
Presentation Time: 2:10 PM

THE SOIL CARBON CO2 FERTILIZATION FACTOR: THE MEASURE OF AN ECOSYSTEM’S CAPACITY TO INCREASE SOIL CARBON STORAGE IN RESPONSE TO ELEVATED CO2 LEVELS


HARRISON, Kevin Geyer, Earth and Environmental Sciences, Northeastern University, 350 Huntington Avenue, 14 Holmes Hall, Boston, MA 02115-5000, k.harrison@neu.edu

This research introduces the concept of a "CO2 fertilization factor for soil carbon" (sCF). The sCF is a measure of an ecosystem's capacity to increase soil carbon storage in response to elevated carbon dioxide levels. This research describes the mathematical derivation of sCF and illustrates how sCF can be determined experimentally, using data from three different CO2 enrichment experiments. I have developed this concept to compare the results of carbon dioxide enrichment experiments having different soil carbon turnover times, different levels of CO2 enrichment, and different lengths of exposure to elevated carbon dioxide levels. The sCF can also be used to estimate increases in soil carbon uptake due to observed contemporary increases in atmospheric carbon dioxide levels. This approach approximates the extent to which elevated carbon dioxide levels increase soil carbon storage. I calculated sCF for three experimental settings -- a mixed forest, and stands of loblolly pine and white oak trees -- by measuring changes in carbon inventories and radiocarbon ratios. The forest had a sCF of 1.8, which would imply a global sequestration of 5.5 billion tons C/year during the 1990's (in the highly-unlikely event that all terrestrial vegetation shows this same response to elevated carbon dioxide levels). The loblolly pine stand had a sCF of 0.9 (2.8 billion tons C/year) and the white oak stand had a sCF of 1.18 (3.5 billion tons C/year). These results show that elevated carbon dioxide levels in the atmosphere are increasing the flux of carbon from the atmosphere to soil.