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Retention of atmospherically-derived nitrogen in subcatchments of the Bjerkreim River in southwestern Norway
During the period 1993-1995 an extensive study on N inputs and losses to streamwater was carried out in 19 subcatchments of the Bjerkreim river$(685\ {\rm km}^{2})$in southwestern Norway. Total N fluxes in the main river outlet were 8.1-10.7 (mean: 9.8) kg ha-1yr-1. Of this total, about 70% was esti...
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Published in: | Ambio 1997-08, Vol.26 (5), p.296-303 |
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Main Authors: | , , |
Format: | Article |
Language: | English |
Subjects: | |
Online Access: | Get full text |
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Summary: | During the period 1993-1995 an extensive study on N inputs and losses to streamwater was carried out in 19 subcatchments of the Bjerkreim river$(685\ {\rm km}^{2})$in southwestern Norway. Total N fluxes in the main river outlet were 8.1-10.7 (mean: 9.8) kg ha-1yr-1. Of this total, about 70% was estimated to be of atmospheric origin. Average N fluxes for forested catchments, heathlands, and mountainous catchments were 2.3-4.2; 4.2-5.0; and 6.3-8.7 kg N ha-1yr-1, respectively. Average retention of total N (calculated as$1\text{-}({\rm N}_{\text{out}}/{\rm N}_{\text{in}})$) was 0.75-0.90 in forested catchments, 0.65-0.70 in heathlands, and 0.55-0.70 in mountainous areas. Possible hypotheses for the relatively high N leaching, especially from the mountainous areas in the Bjerkreim catchment, may be: (i) low N-uptake capacity due to shallow soils, sparse vegetation and short growing season; (ii) N loss during hydrologic events; and (iii) limitation of vegetation growth by other factors than N (e.g. P). In southern Norway, which is dominated by nonforested and mountainous areas, leaching of NO3
-is probably a widespread phenomenon leading to increased acidification and altered nutrient balance in the aquatic environment. |
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ISSN: | 0044-7447 1654-7209 |