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Titel |
Estimating net anthropogenic nitrogen inputs (NANI) in the Lake Dianchi basin of China |
VerfasserIn |
W. Gao, R. W. Howarth, B. Hong, D. P. Swaney, H. C. Guo |
Medientyp |
Artikel
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Sprache |
Englisch
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ISSN |
1726-4170
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Digitales Dokument |
URL |
Erschienen |
In: Biogeosciences ; 11, no. 16 ; Nr. 11, no. 16 (2014-08-28), S.4577-4586 |
Datensatznummer |
250117568
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Publikation (Nr.) |
copernicus.org/bg-11-4577-2014.pdf |
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Zusammenfassung |
Net anthropogenic nitrogen inputs (NANI) with components of atmospheric N
deposition, synthetic N fertilizer, agricultural N fixation and N in net food
and feed imports from 15 catchments in the Lake Dianchi basin were determined
over an 11-year period (2000–2010). The 15 catchments range in size from
44 km2 to 316 km2 with an average of 175 km2. To reduce
uncertainty from scale change methodology, results from data extraction by
area-weighting and land use-weighting methods were compared. Results show
that the methodology for extrapolating data from the county scale to
watersheds has a great influence on NANI computation for catchments in the
Lake Dianchi basin, and that estimates of NANI between the two methods have
an average difference of 30% on a catchment basis, while a smaller
difference (15%) was observed on the whole Lake Dianchi basin basis. The
riverine N export has a stronger linear relationship with NANI computed by
the land use-weighting method, which we believe is more reliable. Overall,
nitrogen inputs assessed by the NANI approach for the Lake Dianchi basin are
9900 kg N km−2 yr−1, ranging from 6600 to
28 000 kg N km−2 yr−1 among the 15 catchments. Synthetic N
fertilizer is the largest component of NANI in most subwatersheds. On
average, riverine flux of nitrogen in catchments of the Lake Dianchi basin
averages 83% of NANI, far higher than generally observed in North
America and Europe. Saturated N sinks and a limited capacity for
denitrification in rivers may be responsible for this high percentage of
riverine N export. Overall, the NANI methodology should be applicable in
small watersheds when sufficiently detailed data are available to estimate
its components. |
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