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Long-term changes of acidifying deposition in Finland (1973-2000)

机译:芬兰酸化沉积物的长期变化(1973-2000年)

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The long-term changes of acidifying deposition in Finland during the period 1973-2000 were studied using bulk deposition data from 19 stations belonging to the national monitoring network. The regional-scale approach (southern, central and northern Finland) was used for trend assessment with respect to implementation of European sulphur (S) emission reduction amendments involving deposition changes prior to (1973-1985) and after (1986-2000) the agreements (S protocols in 1985 and 1994). There were no marked changes in sulphate deposition between the 1970s and 1980s and consistent trends in 1973-1985 were not observed. Deposition of nitrogen (N) compounds, particularly NO_3-N, were increasing between the 1970s and 1980s. Deposition of base cations exhibited a slight decline throughout the 1970s and 1980s. Decrease of calcium and magnesium deposition without corresponding decrease in sulphate resulted in increased acidifying potential (AP) of deposition. Due to successful implementation of S (and N) emission reduction measures, sulphate deposition has decreased substantially (30% in northern and up to 60% in southern Finland) since the late 1980s. N deposition also decreased, but less than S deposition. Base cation deposition has also declined substantially, but this decline appeared to be leveling off during the 1990s, accounting for the decrease of AP in deposition. The observed deposition pattern is in agreement with the on-going biochemical recovery of acidified small Finnish lakes taking place since the early 1990s.
机译:利用来自国家监测网络的19个站点的大量沉积数据,研究了1973-2000年期间芬兰酸化沉积的长期变化。在执行协定之前(1973-1985年)和协定之后(1986-2000年),采用了欧洲范围内的方法(南部,中部和北部)来进行趋势评估,以评估涉及沉积物变化的欧洲减少硫磺排放的修正案(1985年和1994年的S协议)。在1970年代和1980年代之间,硫酸盐的沉积没有显着变化,并且没有观察到1973-1985年的一致趋势。在1970年代至1980年代之间,氮(N)化合物(尤其是NO_3-N)的沉积量有所增加。在整个1970年代和1980年代,碱性阳离子的沉积量略有下降。钙和镁沉积的减少而硫酸盐的相应减少却导致沉积酸化电位(AP)的增加。由于成功实施了S(和N)减排措施,自1980年代后期以来,硫酸盐的沉积已大大减少(北部为30%,南部为60%)。 N沉积也减少,但少于S沉积。碱性阳离子沉积量也大幅下降,但这种下降在1990年代似乎趋于平稳,这说明了沉积物中AP的减少。自1990年代初以来,观察到的沉积模式与酸化的小型芬兰湖泊正在进行的生化恢复一致。

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