This will include the separation of different soil surface CO2 flux components, explicitly separating C derived from plant roots directly and that derived from mycorrhizas. By correlating soil CO2 flux components (including soil priming) with plant assimilation fluxes under present climatic conditions, we aim to resolve the direct interaction of above-ground and below-ground C exchange processes. The effect of soil drought and re-wetting on priming and other soil CO2 efflux components, as well as the effect of elevated CO2 forms a further experimental approach of this project.

Recent evidence indicates that additional sequestration of CO2 by plants does not result in an increase in biomass and thus complex compounds that are likely to become stabilised, but simply in an increase in the amount of carbon (C) entering the soil from roots as labile compounds. In a process called “soil C priming”, it has long been known that the addition of a labile substrate for decomposition can result in the additional release of C as CO2 from other soil organic matter. In the light of likely increases in the input of labile compounds in the future (due to higher atmospheric CO2 concentrations and warmer temperatures), it is not known if soil priming may constitute a significant source of CO2 released from soils, which may mitigate or even reverse any potential benefit from increased CO2 sequestration by plants under a changed climate.

Mycorrhizal fungi, organisms that live in close association with plant roots in a symbiotic relationship, form a dense network of hyphae along which the transport of C and nutrients takes place. The role of these organisms in the distribution and release of C derived from plant roots has so far received insufficient attention to allow a complete understanding of their role in total soil CO2 efflux dynamics. Due to their physical location between tree roots and the soil organic matter, and owing to the extensive network of their hyphae, they are however likely to play a key role in potential soil priming effects.

Results of this project will be incorporated into current ecosystem models in order to address the present lack of positive feedback interactions between plant and soil C exchange processes. These models are instrumental in predicting future changes in the storage of carbon in terrestrial ecosystems, and therefore also the potential of mitigating climatic change. By investigating the dependence of soil CO2 efflux components on soil types, the results will also directly inform decision makers in forestry management, since tree plantations aimed at sequestering C in the long term may be significantly constrained by local soil conditions, if tree plantations actually result in a net release of C.