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Mercury and Other Trace Metals in the Surface Soils of Ny-Alesund, Arctic

机译:纽约 - 亚莱森,北极地表土壤中的汞和其他痕量金属

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Mercury contamination and its rate of transformation and transport are increasing in the environment due to climatic variations. The mercury contamination is also rising in the polar ecosystems too. The present study assessed the content of mercury and other metals in the surface soils of tundra ecosystem of Ny-angstrom lesund, Svalbard. The samples were taken during summer months of 2015-2018 as part of Indian Arctic expedition. Mercury content in the surface soils were ranged from 0.01 to 0.14 mu g/g and is comparable with the earlier studies carried out in the circumpolar regions. Total mercury content in plant samples was also comparable and the mean concentration was 83.45 ng/g. The mercury content is significantly varied from site to site; however, no significant variation was found between years. The interrelationship shown by mercury and other metals indicated a common contaminant pathway. The results indicated that the metals might have influenced by the local variations in the environment especially the increased thawing of permafrost as it led to more runoff of accumulated as well as atmospherically deposited metals. Hence, more detailed studies are required to understand the effect of thawing and atmospheric conditions on the cycling of metals in the polar environment.
机译:由于气候变化,环境污染及其转型和运输速度正在增加。汞污染也在极性生态系统中也在上升。本研究评估了斯瓦尔巴特卫生间苔原苔原生态系统的汞和其他金属含量。作为印度北极远征的一部分,在2015-2018夏季采取了样品。表面土壤中的汞含量为0.01至0.14μg/ g,并且与在环块区域中进行的早期研究相当。植物样品中的总汞含量也可比,平均浓度为83.45ng / g。汞含量明显不同于地点;但是,多年来没有发现显着的变化。汞和其他金属显示的相互关系表示常见的污染途径。结果表明,金属可能受到环境中局部变化的影响,特别是由于它导致累积以及大气沉积的金属的更多径流而导致永久冻土的增加。因此,需要更详细的研究来了解解冻和大气条件对极性环境中金属循环的影响。

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