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Deposition and critical loads of nitrogen in Switzerland

机译:瑞士氮的沉积和临界负荷

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Many ecosystems in Switzerland suffer from eutrophication due to increased atmospheric nitrogen (N) input. In order to get an overview of the problem, critical loads for nutrient N were mapped with a resolution of 1×1 km applying two methods recommended by the UN/ECE: the steady state mass balance method for productive forests, and the empirical method for seminatural vegetation, such as natural forests, (sub-)alpine or species-rich grassland and raised bogs. The national forest inventory and a detailed atlas of vegetation types were used to identify the areas sensitive to N input. The total N input was calculated as the sum of NO{sub}3{sup}-, NH{sub}4{sup}+, NH{sub}3, NO{sub}2 and HNO{sub}3 wet and dry deposition. Wet deposition was determined on the basis of a precipitation map and concentration measurements. Dry deposition was calculated with inferential methods including land-use specific deposition velocities. The concentration fields for NH{sub}3 and NO{sub}2 were obtained from emission inventories combined with dispersion models. Reduced N compounds account for 63% of total deposition in Switzerland. As indicated by exceeded critical loads, the highest risk for harmful effects of N deposition (decrease of ecosystem stability, species shift and losses) is expected on forests and raised bogs in the lowlands, where local emissions are intense. At high altitudes and in dry inner-alpine valleys, deposition rates are significantly lower.
机译:由于大气氮气(n)投入增加,许多瑞士的生态系统患有富营养化。为了了解问题的概述,营养N的临界载荷被映射,分辨率为1×1 km,应用了联合国/ ece推荐的两种方法:生产森林的稳态质量平衡方法以及实证方法种类植被,如天然森林,(亚)高山或富含种类的草原和凸起的沼泽。国家森林库存和植被类型的详细地图集用于识别对N个输入敏感的区域。计算总N个输入作为NO {sub} 3 {sup},nh {sub} 4 {sup} +,nh {sub} 3,no {sub} 2和hno {sub} 3湿干燥沉积。湿沉积在沉淀图和浓度测量的基础上确定。用借调方法计算干沉积,包括土地使用特异性沉积速度。从分散模型结合的排放清单获得NH {Sub} 3和No {Sub} 2的浓度字段。减少的N化合物占瑞士总沉积的63%。如超出临界载荷所表明的,N沉积(生态系统稳定性,物种稳定性,物种转变和损失减少)的最高风险预计在森林和低地升起的沼泽地,当地排放是激烈的。在高海拔和干燥的内高山谷,沉积率明显较低。

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