The global nitrogen cycle in the twenty-first century

David Fowler, Mhairi Coyle, Ute Skiba, Mark A. Sutton, J. Neil Cape, Stefan Reis, Lucy J. Sheppard, Alan Jenkins, Bruna Grizzetti, James N. Galloway, Peter Vitousek, Allison Leach, Alexander F. Bouwman, Klaus Butterbach-Bahl, Frank Dentener, David Stevenson, Marcus Amann, Maren Voss

Research output: Contribution to journalLiterature reviewpeer-review

Abstract

Global nitrogen fixation contributes 413 Tg of reactive nitrogen (N-r) to terrestrial and marine ecosystems annually of which anthropogenic activities are responsible for half, 210 Tg N. The majority of the transformations of anthropogenic Nr are on land (240 Tg N yr(-1)) within soils and vegetation where reduced Nr contributes most of the input through the use of fertilizer nitrogen in agriculture. Leakages from the use of fertilizer Nr contribute to nitrate (NO3-) in drainage waters from agricultural land and emissions of trace N-r compounds to the atmosphere. Emissions, mainly of ammonia (NH3) from land together with combustion related emissions of nitrogen oxides (NOx), contribute 100 Tg N yr(-1) to the atmosphere, which are transported between countries and processed within the atmosphere, generating secondary pollutants, including ozone and other photochemical oxidants and aerosols, especially ammonium nitrate (NH4NO3) and ammonium sulfate (NH4)(2)SO4. Leaching and riverine transport of NO3 contribute 40-70 Tg N yr(-1) to coastal waters and the open ocean, which together with the 30 Tg input to oceans from atmospheric deposition combine with marine biological nitrogen fixation (140 TgN yr(-1)) to double the ocean processing of Nr. Some of the marine Nr is buried in sediments, the remainder being denitrified back to the atmosphere as N-2 or N2O. The marine processing is of a similar magnitude to that in terrestrial soils and vegetation, but has a larger fraction of natural origin. The lifetime of N-r in the atmosphere, with the exception of N2O, is only a few weeks, while in terrestrial ecosystems, with the exception of peatlands (where it can be 102-103 years), the lifetime is a few decades. In the ocean, the lifetime of Nr is less well known but seems to be longer than in terrestrial ecosystems and may represent an important long-term source of N2O that will respond very slowly to control measures on the sources of Nr from which it is produced.

Original languageEnglish
Article number20130164
Pages (from-to)1-13
Number of pages13
JournalPhilosophical Transactions of the Royal Society B: Biological Sciences
Volume368
Issue number1621
DOIs
Publication statusPublished - 5 Jul 2013

Keywords

  • nitrogen fixation
  • denitrification
  • emissions
  • deposition
  • global budgets
  • CLIMATE-CHANGE
  • AIR-POLLUTION
  • DEPOSITION
  • AMMONIA
  • EMISSIONS
  • FIXATION
  • EUROPE
  • FUTURE
  • FLUXES
  • OZONE

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