Which rotation length is favourable to carbon sequestration

By Jari Liski, A. Pussinen, K. Pingoud, R. Mäkipää, T. Karjalainen. 2001

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Soil CO 2 efflux from a podzolic forest soil before and after forest clear-cutting and site preparation (2004, background): “Recent studies on the carbon balance of young forest stands have shown that boreal coniferous forests change from a carbon source to a sink no earlier than at an age of about 15 years (Karjalainen 1996a, 1996b, Schulze et al. 1999, Liski et al. 2001).”
A model for regional analysis of carbon sequestration and timber production (2005, methodology): “Harvest operations and timber transportation are other sources of carbon emissions and are considered by, e.g., Liski et al. (2001).”
Carbon credits and management of Scots pine and Norway spruce stands in Finland (2007, methodology): “More detailed models of stand development have been used in a simulation setting to analyse rotation length effects on carbon flows and timber returns (Pussinen et al., 2002; Liski et al., 2001; Masera et al., 2003).”