Exceedance of critical loads for lakes in Finland, Norway, and Sweden: Reduction requirements for acidifying nitrogen and sulfur deposition

被引:47
作者
Posch, M
Kamari, J
Forsius, M
Henriksen, A
Wilander, A
机构
[1] FINNISH ENVIRONM INST,FIN-00251 HELSINKI,FINLAND
[2] NORWEGIAN INST WATER RES,N-0411 OSLO,NORWAY
[3] SWEDISH UNIV AGR SCI,CTR ENVIRONM MONITORING,S-75007 UPPSALA,SWEDEN
关键词
acidification; critical load; exceedance; sulfur; nitrogen; deposition; lake;
D O I
10.1007/s002679900028
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The main objectives of this study were to identify the regions in Fennoscandia where the critical loads of sulfur (S) and acidifying nitrogen (N) for lakes are exceeded and to investigate the consequences for deposition 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 exceedances, 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 other. Comparing the present N and S deposition with the critical load function for each lake allows determination of the percentage of lakes in the different regions of Fennoscandia where: (1) S reductions alone can achieve nonexceedance, (2) N reductions alone are sufficient, and (3) both N and S reductions are required but to a certain degree interchangeable. Secondly, deposition reduction requirements were assessed by fixing the N deposition to the present level, in this way analyzing the reductions required for S, and by computing the percentage of lakes exceeded in Finland, Norway and Sweden for every possible percent deposition reduction in S and N, in this way showing the (relative) effectiveness of reducing S and/or N deposition. The results showed clear regional patterns in the S and N reduction requirements. In practically the whole of Finland and the northern parts of Scandinavia man-made acidification of surface waters could be avoided by reducing S deposition alone. In the southern parts of Sweden some reductions in N deposition are clearly needed in addition to those for S. In southern Norway strong reductions are required for both N and S deposition.
引用
收藏
页码:291 / 304
页数:14
相关论文
共 55 条
[1]   NITROGEN SATURATION IN NORTHERN FOREST ECOSYSTEMS [J].
ABER, JD ;
NADELHOFFER, KJ ;
STEUDLER, P ;
MELILLO, JM .
BIOSCIENCE, 1989, 39 (06) :378-386
[2]  
[Anonymous], ACIDIFICATION FINLAN, DOI DOI 10.1007/978-3-642-75450-0_
[3]   DYNAMIC-MODEL OF IN-LAKE ALKALINITY GENERATION [J].
BAKER, LA ;
BREZONIK, PL .
WATER RESOURCES RESEARCH, 1988, 24 (01) :65-74
[4]  
Bernes C., 1991, ACIDIFICATION LIMING
[5]  
BRAKKE DF, 1990, VERH INT VEREIN LIMN, V24, P146
[6]   MODELING THE EFFECTS OF ACID DEPOSITION - ASSESSMENT OF A LUMPED PARAMETER MODEL OF SOIL-WATER AND STREAMWATER CHEMISTRY [J].
COSBY, BJ ;
HORNBERGER, GM ;
GALLOWAY, JN ;
WRIGHT, RF .
WATER RESOURCES RESEARCH, 1985, 21 (01) :51-63
[7]   SIMULATION OF THE LONG-TERM SOIL RESPONSE TO ACID DEPOSITION IN VARIOUS BUFFER RANGES [J].
DEVRIES, W ;
POSCH, M ;
KAMARI, J .
WATER AIR AND SOIL POLLUTION, 1989, 48 (3-4) :349-390
[8]   ASSESSMENT OF CRITICAL LOADS AND THEIR EXCEEDANCE ON EUROPEAN FORESTS USING A ONE-LAYER STEADY-STATE MODEL [J].
DEVRIES, W ;
REINDS, GJ ;
POSCH, M .
WATER AIR AND SOIL POLLUTION, 1994, 72 (1-4) :357-394
[9]  
DEVRIES W, 1991, 36 DLO WIN STAR CTR
[10]  
DILLON PJ, 1990, BIOGEOCHEMISTRY, V11, P23, DOI 10.1007/BF00000850