TY - JOUR
T1 - Element interactions limit soil carbon storage
AU - Van Groenigen, Kees Jan
AU - Six, Johan
AU - Hungate, Bruce A.
AU - De Graaff, Marie Anne
AU - Van Breemen, Nico
AU - Van Kessel, Chris
PY - 2006/4/25
Y1 - 2006/4/25
N2 - Rising levels of atmospheric CO2 are thought to increase C sinks in terrestrial ecosystems. The potential of these sinks to mitigate CO 2 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 N2 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 N availability and indirectly by nutrients needed to support N2 fixation.
AB - Rising levels of atmospheric CO2 are thought to increase C sinks in terrestrial ecosystems. The potential of these sinks to mitigate CO 2 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 N2 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 N availability and indirectly by nutrients needed to support N2 fixation.
KW - Global climate change
KW - N fixation
KW - Soil organic matter
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U2 - 10.1073/pnas.0509038103
DO - 10.1073/pnas.0509038103
M3 - Article
C2 - 16614072
AN - SCOPUS:33646232989
SN - 0027-8424
VL - 103
SP - 6571
EP - 6574
JO - Proceedings of the National Academy of Sciences of the United States of America
JF - Proceedings of the National Academy of Sciences of the United States of America
IS - 17
ER -