Element interactions limit soil carbon storage

Rising levels of atmospheric CO2 are thought to increase C sinks in terrestrial ecosystems. The potential of these sinks to mitigate CO2 emissions, however, may be constrained by nutrients. By using metaanalysis, we found that elevated CO2 only causes accumulation of soil C when N is added at rates well above typical atmospheric N inputs. Similarly, elevated CO2 only enhances N-2 fixation, the major natural process providing soil N input, when other nutrients (e.g., phosphorus, molybdenum, and potassium) are added. Hence, soil C sequestration under elevated CO2 is constrained both directly by IN availability and indirectly by nutrients needed to support N2 fixation.

Bibliographic Details

Main Authors:	van Groenigen, K.J., Six, J., Hungate, B.A., de Graaff, M.A., van Breemen, N., van Kessel, C.
Format:	Article/Letter to editor biblioteca
Language:	English
Subjects:	biological nitrogen-fixation, climate-change, cycles, ecosystem responses, elevated atmospheric co2, fine roots, forest, grassland, metaanalysis, model,
Online Access:	https://research.wur.nl/en/publications/element-interactions-limit-soil-carbon-storage
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