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首页> 外文期刊>The Science of the Total Environment >Water chemistry of tundra lakes in the periglacial zone of the Bellsund Fiord (Svalbard) in the summer of 2013
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Water chemistry of tundra lakes in the periglacial zone of the Bellsund Fiord (Svalbard) in the summer of 2013

机译:2013年夏季,贝松德峡湾(斯瓦尔巴特群岛)沿冰川带的苔原湖的水化学

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摘要

Climate changes observed in the Arctic (e.g. permafrost degradation, glacier retreat) may have significant influence on sensitive polar wetlands. The main objectives of this paper are defining chemical features of water within six small arctic lakes located in Bellsund (Svalbard) in the area of continuous permafrost occurrence. The unique environmental conditions of the study area offer an opportunity to observe phenomena influencing water chemistry, such as: chemical weathering, permafrost thawing, marine aerosols, atmospheric deposition and biological inputs. In the water samples collected during the summer 2013, detailed tundra lake water chemistry characteristics regarding ions, trace elements, pH and specific electrolytic conductivity (SEC25) analysis were determined. Moreover, water chemistry of the studied lakes was compared to the water samples from the Tyvjobekken Creek and precipitation water samples. As a final step of data analysis, Principal Component Analysis (PCA) was performed. Detailed chemical analysis allowed us to conclude what follows: (1) Ca2+, Mg2+, SO42−, Sr are of geogenic origin, (2) NO3−present in tundra lakes and the Tyvjobekken Creek water samples (ranging from 0.31 to 1.69mgL−1and from 0.25 to 1.58mgL−1respectively) may be of mixed origin, i.e. from biological processes and permafrost thawing, (3) high contribution of non-sea-salt SO42−>80% in majority of studied samples indicate considerable inflow of sulphate-rich air to the study area, (4) high content of chlorides in tundra lakes (range: 25.6–32.0% meqL−1) indicates marine aerosol influence, (5) PCA result shows that atmospheric transport may constitute a source of Mn, Co, Ni, Cu, Ga, Ba and Cd. However, further detailed inter-season and multi-seasonal study of tundra lakes in the Arctic are recommended. Especially in terms of detailed differentiation of sources influence (atmospheric transport vs. permafrost degradation).
机译:在北极观察到的气候变化(例如多年冻土退化,冰川退缩)可能会对敏感的极地湿地产生重大影响。本文的主要目的是确定连续多年冻土发生地区位于贝尔松(斯瓦尔巴特群岛)的六个小型北极湖中水的化学特征。研究区域的独特环境条件为观察影响水化学的现象提供了机会,例如:化学风化,多年冻土融化,海洋气溶胶,大气沉积和生物输入。在2013年夏季收集的水样本中,确定了苔原湖水的详细化学特性,涉及离子,微量元素,pH和比电导率(SEC25)分析​​。此外,将所研究湖泊的水化学与Tyvjobekken Creek的水样和降水水样进行了比较。作为数据分析的最后一步,执行了主成分分析(PCA)。详细的化学分析使我们可以得出以下结论:(1)Ca2 +,Mg2 +,SO42-,Sr是地质成因,(2)苔原湖和Tyvjobekken Creek水样品中的NO3-存在(范围为0.31至1.69mgL-1,以及分别从0.25到1.58mgL-1)可能是混合来源,即来自生物过程和多年冻土融化。(3)大多数研究样品中非海盐SO42-> 80%的高贡献表明大量富硫酸盐流入空气进入研究区域,(4)苔原湖中的氯化物含量高(范围:25.6–32.0%meqL-1)表明海洋气溶胶的影响,(5)PCA结果表明,大气迁移可能构成了Mn,Co, Ni,Cu,Ga,Ba和Cd。但是,建议对北极的苔原湖进行更详细的季节间和多季节研究。特别是在详细区分源影响方面(大气传输与多年冻土退化)。

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