New Perspectives on Nitrogen Cycling in the Temperate and by Alan R. Townsend

By Alan R. Townsend

Inputs of nitrogen to terrestrial and aquatic ecosystems have elevated several-fold during the last 100 and fifty years, with the steepest raises over the last 4 many years. the growth of fertilizer manu­ facture and use, the rise in fossil gas combustion, the intensification of animal husbandry, and common cultivation of N2 solving plants have all contributed to the dramatic bring up in N inputs. the rise has been so much quick in Northern Hemisphere (NH) temperate ecosystems, yet almost immediately subtropical and tropical areas of Asia also are experiencing an explosive bring up in N inputs to terrestrial ecosystems (W. Chameides, pers. comm. ; Galloway et al. 1996). Projected raises in N deposition for those trop­ ical and subtropical areas, with a excessive usual heritage of N inputs, exceed raises projected for temperate and arctic areas (Cleveland et al. submitted; Galloway et al. 1994; Holland & Lamarque 1997a). in comparison to organic N fixation, N deposition is changing into a proportionately higher resource of N to terrestrial and aquatic ecosystems world wide (Vitousek et al. 1997). 6 The nitrogen inside the surroundings as N , three. nine * 10 Tg (Tg = 2 12 10 g), is the most important reservoir of N within the Earth procedure (Warneck 1988). besides the fact that, this paper makes a speciality of the nitrogen emissions and deposition which were remodeled from N2 into reactive kinds which are biologically avail­ capable (e. g. Vitousek et al. 1997).

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