Element interactions limit soil carbon storage

  • Kees Jan Van Groenigen
  • , Johan Six
  • , Bruce A. Hungate
  • , Marie Anne De Graaff
  • , Nico Van Breemen
  • , Chris Van Kessel

Research output: Contribution to journalArticlepeer-review

321 Scopus citations

Abstract

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.

Original languageEnglish
Pages (from-to)6571-6574
Number of pages4
JournalProceedings of the National Academy of Sciences of the United States of America
Volume103
Issue number17
DOIs
StatePublished - 25 Apr 2006

UN SDGs

This output contributes to the following UN Sustainable Development Goals (SDGs)

  1. SDG 13 - Climate Action
    SDG 13 Climate Action
  2. SDG 15 - Life on Land
    SDG 15 Life on Land

Keywords

  • Global climate change
  • N fixation
  • Soil organic matter

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