Abstract
Within terrestrial ecosystems, the soil C02 efflux is one of the largest carbon flux components. The global efflux of carbon from the soil is estimated between 50 and 75 Gt C year-1 and makes up 20–40 % of the total annual input of carbon dioxide into the atmosphere (Houghton and Woodwell 1989; Raich and Schlesinger 1992; Schimel 1995). The magnitude of the soil flux is similar to that of the net primary productivity (Houghton and Woodwell 1989). It has been suggested that as global temperature rises, enhanced decomposition of the large soil carbon stock (1580 x 1015 g; Schimel 1995), especially in the high northern latitudes, might increase the input of carbon into the atmosphere (Gordon et al. 1987; Kirschbaum 1995; Trumbore et al. 1996; Zimov et al. 1996). However, the effect of a temperature increase on the decomposition rate is still unsolved and a point of discussion. Others suggest that decomposition rates in forest soils are not controlled by temperature (Liski et al. 1999; Giardina and Ryan 2000). Besides the potential temperature-induced feedback, changes in land use and forest management, which do affect the storage of carbon in the soil, were important points of discussion throughout the negotiations of the Kyoto protocol. Therefore, understanding the processes underlying the exchange of carbon from and into the soil is needed to make “management of the net carbon budget” possible (IGBP Terrestrial Carbon Working Group 1998).
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Lankreijer, H., Janssens, I.A., Buchmann, N., Longdoz, B., Epron, D., Dore, S. (2003). Measurement of Soil Respiration. In: Valentini, R. (eds) Fluxes of Carbon, Water and Energy of European Forests. Ecological Studies, vol 163. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-05171-9_3
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