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dc.contributor.authorFowler, D.
dc.contributor.authorCoyle, M.
dc.contributor.authorSkiba, U.
dc.contributor.authorSutton, M.A.
dc.contributor.authorCape, J.N.
dc.contributor.authorReis, S.
dc.contributor.authorSheppard, L.J.
dc.contributor.authorJenkins, A.
dc.contributor.authorGrizetti, B.
dc.contributor.authorGalloway, J.N.
dc.contributor.authorVitousek, P.
dc.contributor.authorLeach, A.
dc.contributor.authorBouwman, A.F.
dc.contributor.authorButterbach-Bahl, Klaus
dc.contributor.authorDentener, F.
dc.contributor.authorStevenson, D.
dc.contributor.authorAmann, M.
dc.contributor.authorVoss, M.l.
dc.date.accessioned2014-02-02T10:07:06Z
dc.date.available2014-02-02T10:07:06Z
dc.date.issued2013-05-27
dc.identifier.citationFowler D., Coyle M., Skiba U., Sutton M.A., Cape J.N., Reis S., Sheppard L.J., Jenkins A., Grizetti B., Galloway J.N., Vitousek P., Leach A., Bouwman A.F., Butterbach-Bahl K., Dentener F., Stevenson D., Amann M., Voss M.l. 2013. The global nitrogen cycle in the twenty-first century. Phil. Trans. R. Soc. B 368(1621): 1471-2970en_US
dc.identifier.issn0962-8436
dc.identifier.urihttp://hdl.handle.net/10568/34481
dc.description.abstractGlobal nitrogen fixation contributes 413 Tg of reactive nitrogen (Nr) 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 Nr 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)2SO4. 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 N2 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 Nr 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.en_US
dc.language.isoenen_US
dc.sourcePhilosophical Transactions of the Royal Society Ben_US
dc.subjectAGRICULTUREen_US
dc.subjectCLIMATIC CHANGEen_US
dc.subjectENVIRONMENTen_US
dc.titleThe global nitrogen cycle in the twenty-first centuryen_US
dc.typeJournal Articleen_US
cg.subject.ilriAGRICULTUREen_US
cg.subject.ilriCLIMATE CHANGEen_US
cg.subject.ilriENVIRONMENTen_US
cg.identifier.statusLimited Accessen_US
cg.targetaudienceSCIENTISTSen_US
cg.identifier.doihttps://dx.doi.org/10.1098/rstb.2013.0164en_US
cg.isijournalISI Journalen_US


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