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首页> 外文期刊>Hydrology and Earth System Sciences >Modelling the effects of atmospheric sulphur and nitrogen deposition on selected lakes and streams of the Central Alps (Italy)
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Modelling the effects of atmospheric sulphur and nitrogen deposition on selected lakes and streams of the Central Alps (Italy)

机译:模拟大气硫和氮沉积对中部阿尔卑斯山(意大利)的部分湖泊和溪流的影响

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摘要

The dynamic model MAGIC was calibrated and applied to selected sites in north-western Italy (3 rivers, 10 alpine lakes) to predict the future response of surface water to different scenarios of atmospheric deposition of S and N compounds. Results at the study sites suggest that several factors other than atmospheric deposition may influence the long-term changes in surface water chemistry. At present the lumped approach of dynamic models such as MAGIC cannot represent all the processes occurring at the catchment scale. Climate warming in particular and its effects on surface water chemistry proved to be important in the study area. Furthermore the river catchments considered here showed clear signs of N saturation. This condition and the increasing concentrations of NO, in river water were simulated using N dynamics recently included in MAGIC. The modelling performed in this study re. presents the first application of MAGIC to Italian sites. The results show that inclusion of other factors specific to the Mediterranean area, such as dust deposition and climate change, may improve the fit to observed data and the reliability of the model forecast. Despite these limitations, the model captured well the main trends in chemical data in both rivers and lakes. The outputs clearly demonstrate the benefits of achieving the emission reductions in both S and N compounds as agreed under the Gothenburg Protocol rather than making no further emission reductions. It was also clear that, besides the substantial reduction of SO4 deposition from the peak levels of the 1980s, N deposition must also be reduced in the near future to protect freshwaters from further acidification. [References: 27]
机译:对动力学模型MAGIC进行了校准,并将其应用于意大利西北部的选定地点(3条河流,10个高山湖泊),以预测地表水对S和N化合物在大气中沉降的不同情景的未来响应。研究地点的结果表明,除了大气沉积以外,还有其他一些因素可能会影响地表水化学的长期变化。目前,像MAGIC这样的动态模型的集总方法不能代表流域尺度上发生的所有过程。在研究领域,气候变暖及其对地表水化学的影响尤其重要。此外,此处考虑的河流流域显示出明显的N饱和迹象。使用最近包括在MAGIC中的N动力学模拟了这种情况和河水中NO浓度的增加。在这项研究中进行了建模。展示了MAGIC在意大利网站上的首次应用。结果表明,包括其他特定于地中海地区的因素,例如沙尘沉积和气候变化,可能会改善对观测数据的拟合度以及模型预测的可靠性。尽管有这些限制,该模型仍很好地捕捉了河流和湖泊中化学数据的主要趋势。这些输出清楚地表明了实现《哥德堡议定书》所商定的S和N化合物减排的好处,而不是不再进一步减排。同样清楚的是,除了从1980年代的峰值大大减少SO4的沉积量之外,在不久的将来还必须减少N的沉积量,以保护淡水免受进一步的酸化。 [参考:27]

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