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Hydrology and Earth System Sciences An interactive open-access journal of the European Geosciences Union
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Volume 3, issue 3
Hydrol. Earth Syst. Sci., 3, 395–408, 1999
https://doi.org/10.5194/hess-3-395-1999
© Author(s) 1999. This work is licensed under
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.
Hydrol. Earth Syst. Sci., 3, 395–408, 1999
https://doi.org/10.5194/hess-3-395-1999
© Author(s) 1999. This work is licensed under
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.

  30 Sep 1999

30 Sep 1999

Spatial variability of nitrate concentration in lakes in Snowdonia, North Wales, UK

M. R. Kernan and T. E. H. Allott M. R. Kernan and T. E. H. Allott
  • Environmental Change Research Centre, Department of Geography, University College London, 26 Bedford Way, London WC1H 0AP.
  • e-mail address for correspondin author: mkernan@geog.ucl.ac.uk

Abstract. At a regional scale, high nitrate (NO3) concentrations in upland surface waters generally occur in tandem with high nitrogen (N) deposition levels. However, significant differences in the patterns of surface water NO3 concentration have been observed within areas of similar N deposition yet relatively few studies have been undertaken which examine within-region variation of NO3 concentrations. A study of 76 lakes in Snowdonia, north Wales, an area of high deposition and sensitive catchments, was undertaken to assess variation in surface water NO3 concentration across a 20 x 20 km grid square and to identify catchments vulnerable to NO3 leaching. Nitrate concentrations vary considerably, particularly during winter when values range from 0.7 to 70 μeq l-1. Although retention by vegetation and soil microbes in summer reduces the amount of NO3 reaching the lakes, 37 % of sites are characterised by NO3 concentrations greater then 4 μeq l-1. The elevated concentrations occurring in summer suggests that N breakthrough has occurred. By examining the ratio of NO3 to total strong acid anions, it is shown that NO3 contributes significantly to freshwater acidity, particularly during the winter. Redundancy analysis shows that NO3 leaching is greatest, both in winter and summer, in catchments with high proportions of bare rock where soil and vegetation cover is limited. Nitrogen cycling in these catchments, generally at higher altitudes, may no longer be governed by seasonal biological controls. They are likely to be saturated with respect to nitrogen (i.e. incapable of further N retention) as a result of the elevated deposition levels in the area. The contribution of NO3 to acidity is also greatest at these sites. In winter, significant positive relationships are also evident between NO3 concentration and soil pH and coniferous woodland. The study demonstrates the importance of catchment factors in modifying the relationship between N deposition and N leaching in upland catchments.

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