Present and potential nitrogen outputs from Norwegian soft water lakes – an assessment made by applying the steady-state First-order Acidity Balance (FAB) model

The steady-state First-order Acidity Balance (FAB) model for calculating critical loads of sulphur (S) and nitrogen (N) is applied to 609 Norwegian soft-water lakes to assess the future nitrate (NO<sub>3</sub><sup>&#8254;</sup>) leaching potential under present (1992-96)...

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Bibliographic Details
Main Authors: Ø. Kaste, A. Henriksen, M. Posch
Format: Article
Language:English
Published: Copernicus Publications 2002-01-01
Series:Hydrology and Earth System Sciences
Online Access:http://www.hydrol-earth-syst-sci.net/6/101/2002/hess-6-101-2002.pdf
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Summary:The steady-state First-order Acidity Balance (FAB) model for calculating critical loads of sulphur (S) and nitrogen (N) is applied to 609 Norwegian soft-water lakes to assess the future nitrate (NO<sub>3</sub><sup>&#8254;</sup>) leaching potential under present (1992-96) S and N deposition. The lakes were separated into five groups receiving<br> increasing levels of N deposition (<25, 25-49, 50-74, 75-99 and 100-125 meq m<sup>-2</sup>yr<sup>-1</sup>). Using long-term sustainable N sink rates presently recommended for FAB model applications, N immobilisation, net N uptake in forests, denitrification and in-lake N retention were estimated for each group of lakes. Altogether, the long-term N sinks constituted 9.9 &#177; 3.2 to 40.5 &#177; 11.4 meq m<sup>-2</sup>yr<sup>-1</sup> in the lowest and highest N deposition categories, respectively. At most sites, the current N deposition exceeds the amount of N retained by long-term sustainable N sinks plus the NO<sub>3</sub><sup>&#8254;</sup> loss via the lake outlets. This excess N, which is currently retained within the catchments may, according to the FAB model, leach as acidifying NO<sub>3</sub><sup>&#8254;</sup> in the future. If these predictions are fulfilled, NO<sub>3</sub><sup>&#8254;</sup> leaching at sites in the various N deposition categories will increase dramatically from present (1995) mean levels of 1-20 meq m<sup>-2</sup>yr<sup>-1</sup>, to mean levels of 7-70 meq m<sup>-2</sup>yr<sup>-1</sup> at future steady state. To illustrate the significance of such an increase in NO<sub>3</sub><sup>&#8254;</sup> leaching, the mean Acid Neutralising Capacity (ANC) at sites in the highest N deposition category may decrease from -18 &#177; 15 &#956;eq L<sup>-1</sup> at present, to -40 &#177; 20 &#956;eq L<sup>-1</sup>. Under present S and N deposition levels, the FAB model predicts that 46% of the Norwegian lakes may experience exceedances of critical loads for acidifying deposition. In comparison, the Steady-State Water Chemistry model (SSWC), which considers only the present N leaching level, estimates critical load exceedances in 37% of the lakes under the same deposition level. Thus far, there are great uncertainties regarding both the time scales and the extent of future N leaching, and it is largely unknown whether the FAB model predictions will ever be fulfilled. Hence, long-term monitoring and further studies on N immobilisation processes under varying N deposition levels and ecosystem types seem necessary to make better predictions of future NO<sub>3</sub><sup>&#8254;</sup> leaching.</p> <p style='line-height: 20px;'><b>Keywords: </b>Lakes, hydrochemistry, nitrogen, nitrate, sinks, leaching, acidification, critical loads, FAB model
ISSN:1027-5606
1607-7938