Nitrogen deposition and its contribution to nitrogen cycling and associated soil processes

KWT Goulding*, NJ Bailey, NJ Bradbury, PR Hargreaves, M Howe, DV Murphy, PR Poulton, TW Willison

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

245 Citations (Scopus)
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Abstract

Human activity has greatly perturbed the nitrogen cycle through increased fixation by legumes, by energy and fertilizer production, and by the mobilization of N from long-term storage pools. This extra reactive N is readily transported through the environment, and there is increasing evidence that it is changing ecosystems through eutrophication and acidification. Rothamsted Experimental Station, UK has been involved in research on N cycling in ecosystems since its inception in 1843. Measurements of precipitation composition at Rothamsted, made since 1853, show an increase of nitrate and ammonium N in precipitation from 1 and 3 kg N ha−1 yr−1, respectively, in 1855 to a maximum of 8 and 10 kg N ha−1 yr−1 in 1980, decreasing to 4 and 5 kg N ha−1 yr−1 today. Nitrogen inputs via dry deposition do, however, remain high. Recent measurements with diffusion tubes and filter packs show large concentrations of nitrogen dioxide of c. 20 ug m−3 in winter and c. 10 ug m−3 in summer; the difference is linked to the use of central heating, and with variations in wind direction and pollutant source. Concentrations of nitric acid and particulate N exhibit maxima of 1±5 and 2 ug m−3 in summer and winter, respectively. Concentrations of ammonia are small, barely rising above 1 ug m−3. Taking deposition velocities from the literature gives a total deposition of all measured N species to winter cereals of 43±3 kg N ha−1 yr−1, 84% as oxidized species, 79% dry deposited. The fate of this N deposited to the very long-term Broadbalk Continuous Wheat Experiment at Rothamsted has been simulated using the SUNDIAL N-cycling model: at equilibrium, after 154 yr of the experiment and with N deposition increasing from c. 10 kg ha−1 yr−1 in 1843 to 45 kg ha−1 yr−1 today, c. 5% is leached, 12% is denitrified, 30% immobilized in the soil organic matter and 53% taken off in the crop. The `efficiency of use' of the deposited N decreases, and losses and immobilization increase as the amount of fertilizer N increases. The deposited N itself, and the acidification that is associated with it (from the nitric acid, ammonia and ammonium), has reduced the number of plant species on the 140-yr-old Park Grass hay meadow. It has also reduced methane oxidation rates in soil by c. 15% under arable land and 30% under woodland, and has caused N saturation of local woodland ecosystems: nitrous oxide emission rates of up to 1±4 kg ha−1 yr−1 are equivalent to those from arable land receiving "200 kg N ha−1 yr−1, and in proportion to the excess N deposited; measurements of N cycling processes and pools using "&N pool dilution techniques show a large nitrate pool and enhanced rates of nitrification relative to immobilization. Ratios of gross nitrification :gross immobilization might prove to be good indices of N saturation.
Original languageEnglish
Pages (from-to)49-58
Number of pages9
JournalNew Phytologist
Volume139
Publication statusFirst published - 1998
Externally publishedYes

Keywords

  • Nitrogen
  • Deposition
  • atmospheric

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