CREAF, Cerdanyola del Vallès 08193, Spain.
CREAF, Cerdanyola del Vallès 08193, Spain; Universitat Autònoma de Barcelona, Cerdanyola del Vallès 08193, Spain.
Sci Total Environ. 2016 Feb 15;544:919-28. doi: 10.1016/j.scitotenv.2015.12.017. Epub 2015 Dec 17.
The abatement programs implanted in Europe to reduce SO2, NO2 and NH3 emissions are here evaluated by analyzing the relationships between emissions in Spain and neighboring countries and atmospheric deposition in a Mediterranean forest in the Montseny mountains (NE Spain) for the last 3decades. A canopy budget model was applied to throughfall data measured during a period of high emissions (1995-1996) and a period of lower emissions (2011-2013) to estimate the changes in dry deposition over this time span. Emissions of SO2 in Spain strongly decreased (77%) and that was reflected in reductions for nssSO4(2-) in precipitation (65% for concentrations and 62% for SO4(2)-S deposition). A lower decline was found for dry deposition (29%). Spanish NO2 emissions increased from 1980 to 1991, remained constant until 2005, and decreased thereafter, a pattern that was paralleled by NO3(-) concentrations in bulk precipitation at Montseny. This pattern seems to be related to a higher share of renewable energies in electricity generation in Spain in recent years. However, dry deposition increased markedly between 1995 and 2012, from 1.3 to 6.7 kg ha(-1) year(-)(1). Differences in meteorology between periods may have had a role, since the recent period was drier thus probably favoring dry deposition. Spanish NH3 emissions increased by 13% between 1980 and 2012 in Spain but NH4(+) concentrations in precipitation and NH4(+)-N deposition showed a decreasing trend (15% reduction) at Montseny, probably linked to the reduction ammonium sulfate and nitrate aerosols to be scavenged by rainfall. NH4(+)-N dry deposition was similar between the compared periods. The N load at Montseny (15-17 kg ha(-1)y ear(-1)) was within the critical load range proposed for Mediterranean sclerophyllous forests (15-17.5 kg ha(-1) year(-1)). The onset of N saturation is suggested by the observed increasing N export in streamwaters.
该研究通过分析过去 30 年来西班牙及其邻国的排放物与位于西班牙蒙桑尼山区(东北)的一片地中海森林的大气沉降之间的关系,评估了欧洲实施的减少 SO2、NO2 和 NH3 排放的减排计划。该研究应用冠层收支模型对高排放时期(1995-1996 年)和低排放时期(2011-2013 年)的穿透雨数据进行了分析,以估算这一时期干沉降的变化。西班牙的 SO2 排放量大幅减少(77%),这反映在降水(浓度减少 65%,SO4(2)-S 沉积减少 62%)中 nssSO4(2-)的减少。而干沉降的下降幅度较小(29%)。西班牙的 NO2 排放量从 1980 年到 1991 年增加,直到 2005 年保持不变,此后减少,这种模式与蒙桑尼地区的总降水的 NO3(-)浓度相吻合。这种模式似乎与近年来西班牙可再生能源在发电中所占份额的增加有关。然而,1995 年至 2012 年间,干沉降显著增加,从 1.3 至 6.7kg ha-1年-1。不同时期的气象条件可能发挥了作用,因为近期较为干燥,可能有利于干沉降。1980 年至 2012 年期间,西班牙的 NH3 排放量增加了 13%,但蒙桑尼地区的降水和 NH4(+)-N 沉降中 NH4(+)浓度呈下降趋势(减少 15%),这可能与被雨水清除的硫酸铵和硝酸盐气溶胶的减少有关。两个时期的 NH4(+)-N 干沉降相似。蒙桑尼的氮负荷(15-17kg ha-1年-1)在拟议的地中海硬叶林临界负荷范围内(15-17.5kg ha-1年-1)。观察到溪流中氮的输出不断增加,表明氮已经开始过饱和。