EXCEEDANCE OF CRITICAL LOADS FOR LAKES IN FINLAND, NORWAY, AND SWEDEN- REDUCTION REQUIREMENTS FOR ACIDIFYING NITROGEN AND SULFUR DEPOSITION

Citation
M. Posch et al., EXCEEDANCE OF CRITICAL LOADS FOR LAKES IN FINLAND, NORWAY, AND SWEDEN- REDUCTION REQUIREMENTS FOR ACIDIFYING NITROGEN AND SULFUR DEPOSITION, Environmental management, 21(2), 1997, pp. 291-304
Citations number
55
Categorie Soggetti
Environmental Sciences
Journal title
ISSN journal
0364152X
Volume
21
Issue
2
Year of publication
1997
Pages
291 - 304
Database
ISI
SICI code
0364-152X(1997)21:2<291:EOCLFL>2.0.ZU;2-P
Abstract
The main objectives of this study were to identify the regions in Fenn oscandia where the critical loads of sulfur (S) and acidifying nitroge n (N) for lakes are exceeded and to investigate the consequences for d eposition reductions, with special emphasis on the possible trade-offs between S and N deposition in order to achieve nonexceedance, in the steady-state model for calculating critical loads and their exceedance s, all relevant processes acting as sinks for N and S are considered. The critical loads of N and S are interrelated (defining the so-called critical load function), and therefore a single critical load for one pollutant cannot be defined without making assumptions about the othe r. Comparing the present N and S deposition with the critical load fun ction for each lake allows determination of the percentage of lakes in the different regions of Fennoscandia where: (1) S reductions alone c an achieve nonexceedance, (2) N reductions alone are sufficient, and ( 3) both N and S reductions are required but to a certain degree interc hangeable. Secondly, deposition reduction requirements were assessed b y fixing the N deposition to the present level, in this way analyzing the reductions required for S, and by computing the percentage of lake s exceeded in Finland, Norway and Sweden for every possible percent de position reduction in S and N, in this way showing the (relative) effe ctiveness of reducing S and/or N deposition. The results showed clear regional patterns in the S and N reduction requirements. In practicall y the whole of Finland and the northern parts of Scandinavia man-made acidification of surface waters could be avoided by reducing S deposit ion alone. In the southern parts of Sweden some reductions in N deposi tion are clearly needed in addition to those for S. In southern Norway strong reductions are required for both N and S deposition.