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Atmospheric deposition chemistry in a subalpine area of the Julian alps, North-West Slovenia

机译:斯洛文尼亚西北部朱利安阿尔卑斯山亚高山地区的大气沉积化学

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Wet-only precipitation was collected in Rate?e, a remote village in the outskirts of the Julian Alps (Nort-West Slovenia) during 2003-2011, in order to characterise atmospheric deposition chemistry. The samples were collected on a daily basis and combined into weekly samples that were analysed for pH, conductivity and major anions and cations. Ammonium, nitrate and sulphate were the most abundant ions, exhibiting volume-weighted mean values (2003-2011) of 22, 17 and 17 μeq L~(-1), respectively. Furthermore, the trends of the major parameters in the precipitation were assessed using a simple linear regression. A significant downward trend of both nitrate and sulphate was observed, explained by evident reductions in NO_x and SO_x emissions in the region. The decline of nitrate and sulphate was also reflected in a significant and downward trend of conductivity. While the trend of ammonium could also be downward, the trends of other major ions were not significant. Atmospheric nitrogen deposition, representing inorganic forms of nitrogen (i.e., ammonium and nitrate), was calculated to examine potential threats that the deposition of nitrogen may cause on lake ecosystems. Nitrogen deposition in Rate?e ranged from 5.5 to 9.5 kg N ha~(-1) yr~(-1). Although this was below the critical threshold that might cause an impact on surface waters, nitrogen deposition in the nearby Julian Alps, where sensitive mountain lakes are situated, might be higher and its impact on the ecosystem greater. In fact, several studies performed on water chemistry, sedimentary organic matter and stable isotopes in Slovenian mountain lakes have shown progressive changes in their water columns and sediments that can be attributed to nitrogen deposition.
机译:为了表征大气沉积化学特征,2003年至2011年期间,朱利安阿尔卑斯山郊区(诺特-西斯洛文尼亚)的偏远村庄Rate?e收集了仅湿润的降水。每天收集样品,并合并成每周样品,分析其pH值,电导率以及主要的阴离子和阳离子。铵离子,硝酸根离子和硫酸根离子是最丰富的离子,其体积加权平均值(2003-2011年)分别为22、17和17μeqL〜(-1)。此外,使用简单的线性回归评估了降水中主要参数的趋势。观察到硝酸盐和硫酸盐都有明显的下降趋势,这可以通过该地区NO_x和SO_x排放量的明显减少来解释。硝酸盐和硫酸盐的减少也反映在电导率的显着和下降趋势中。虽然铵的趋势也可能下降,但其他主要离子的趋势并不明显。计算了代表氮的无机形式(即铵和硝酸盐)的大气氮沉积量,以研究氮沉积可能对湖泊生态系统造成的潜在威胁。氮的沉积速率为5.5至9.5 kg N ha〜(-1)yr〜(-1)。尽管这低于可能对地表水造成影响的临界阈值,但附近敏感的高山湖泊所在的朱利安阿尔卑斯山的氮沉降可能更高,并且对生态系统的影响更大。实际上,在斯洛文尼亚山区湖泊中对水化学,沉积有机质和稳定同位素进行的多项研究表明,其水柱和沉积物的逐步变化可能归因于氮的沉积。

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