Hyvönen, Riitta
- Department of Ecology and Environmental Research, Swedish University of Agricultural Sciences
Research article2007Peer reviewedOpen access
Hyvonen, R; Agren, GI; Linder, S; Persson, T; Cotrufo, MF; Ekblad, A; Freeman, M; Grelle, A; Janssens, IA; Jarvis, PG; Kellomaki, S; Lindroth, A; Loustau, D; Lundmark, T; Norby, RJ; Oren, R; Pilegaard, K; Ryan, MG; Sigurdsson, BD; Stromgren, M;
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Temperate and boreal forest ecosystems contain a large part of the carbon stored on land, in the form of both biomass and soil organic matter. Increasing atmospheric [CO2], increasing temperature, elevated nitrogen deposition and intensified management will change this C store. Well documented single-factor responses of net primary production are: higher photosynthetic rate (the main [CO2] response); increasing length of growing season (the main temperature response); and higher leaf-area index (the main N deposition and partly [CO2] response). Soil organic matter will increase with increasing litter input, although priming may decrease the soil C stock initially, but litter quality effects should be minimal (response to [CO2], N deposition, and temperature); will decrease because of increasing temperature; and will increase because of retardation of decomposition with N deposition, although the rate of decomposition of high-quality litter can be increased and that of low-quality litter decreased. Single-factor responses can be misleading because of interactions between factors, in particular those between N and other factors, and indirect effects such as increased N availability from temperature-induced decomposition. In the long term the strength of feedbacks, for example the increasing demand for N from increased growth, will dominate over short-term responses to single factors. However, management has considerable potential for controlling the C store
New Phytologist
2007, volume: 173, number: 3, pages: 463-480
Publisher: BLACKWELL PUBLISHING
Environmental Sciences and Nature Conservation
https://res.slu.se/id/publ/11182