Carbon Sequestration in Forest Ecosystems by Klaus Lorenz

By Klaus Lorenz

Carbon Sequestration in wooded area Ecosystems is a complete e-book describing the elemental methods of carbon dynamics in wooded area ecosystems, their contribution to carbon sequestration and implications for mitigating abrupt weather switch. This publication offers the data on methods, elements and factors influencing carbon sequestration in woodland ecosystems. Drawing upon newest references, this e-book summarizes the present knowing of carbon sequestration approaches in wooded area ecosystems whereas opting for wisdom gaps for destiny study, therefore, this booklet is a invaluable wisdom resource for college kids, scientists, woodland managers and coverage makers.

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2008; Lewis et al. 2009). Tropical forests can sequester larger amounts of C annually than temperate forests whereas boreal forests sequester the smallest amounts of C among global forest biomes (Bonan 2008). The current additional SOC sequestration potential appears to be tiny against the amount of C that can be potentially lost in the future (Reichstein 2007). Thus, the vulnerability of SOC to potential losses requires special attention. 02 Mg C ha−1 year−1), and 100 to 500 times slower than changes in litter pools (~2–10 Mg C ha−1 year−1) which occur on time scales of months to years (Trumbore and Czimczik 2008).

Contribution of working group III to the fourth assessment report of the intergovernmental panel on climate change. Cambridge University Press, Cambridge/New York, pp 541–584 Nieder R, Benbi DK, Isermann K (2003) Soil organic matter dynamics. In: Benbi DK, Nieder R (eds) Handbook of processes and modeling in the soil-plant system. Haworth, New York, pp 345–408 Odum EP (1967) The strategy of ecosystem development. Science 164:262–270 Ovington JD (1962) Quantitative ecology and the woodland ecosystem concept.

32 2 The Natural Dynamic of Carbon in Forest Ecosystems In humid regions, the photosynthetic rate can also be limited by light and, in particular, diffuse radiation beside CO2 and RUBISCO (Schulze 2006; Mercado et al. 2009). The surface solar radiation can be partitioned in diffuse and direct components but diffuse radiation is relevant for photosynthesis as it can penetrate deeper into the vegetation canopy (Wild 2009). The long term trends in the amount of solar radiation reaching photosynthetic active pigments are, however, not fully known (Romanou et al.

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