Volume 18, Issue 3 p. 175-183

A modelling analysis of the potential for soil carbon sequestration under short rotation coppice willow bioenergy plantations

P. Grogan

Corresponding Author

P. Grogan

Institute of Water and Environment, Cranfield University, Silsoe, Bedfordshire, MK45 4DT, UK

Corresponding author. Fax: 01525 863344. E-mail: [email protected]Search for more papers by this author
R. Matthews

R. Matthews

Institute of Water and Environment, Cranfield University, Silsoe, Bedfordshire, MK45 4DT, UK

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First published: 19 January 2006
Citations: 52

Abstract

Abstract. Rising atmospheric CO2 concentrations and their association with global climate change have led to several major international initiatives to reduce net CO2 emissions, including the promotion of bioenergy crops such as short rotation coppice (SRC) willow. Although the above-ground harvested bio-fuel is likely to be the major contributor to the CO2 mitigation potential of bioenergy crops, additional carbon may be sequestered through crop inputs into plantation soils.  Here, we describe a process-based model specifically designed to evaluate the potential for soil carbon sequestration in SRC willow plantations in the UK. According to the model predictions, we conclude that the potential for soil carbon sequestration in these plantations is comparable to, or even greater than, that of naturally regenerating woodland. Our preliminary, site-specific model output suggests that soil carbon sequestration may constitute about 5% of the overall carbon mitigation benefit arising from SRC plantations. Sensitivity analyses identified the following factors as the principal controls on rates and amounts of soil carbon sequestration under SRC: carbon inputs (net primary production), decomposition rates of the major soil carbon pools, initial soil carbon content (an inverse relationship with rates of soil carbon sequestration), crop/plantation management, and depth of soil being influenced by the bioenergy crop. Our results suggest that carbon sequestration potential is greatest in soils whose carbon content has been depleted to relatively low levels due to agricultural land use practices such as annual deep ploughing of agricultural soils.