Assessment of the Distribution of Heavy Metals in Soils of Severny Island (Novaya Zemlya)

Q4 Environmental Science
S. S. Popov
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引用次数: 1

Abstract

Global warming occurs the fastest in polar latitudes, increasing their economic accessibility and, consequently, entailing risks of technogenic contamination. Heavy metals (HM) are among the most common technogenic pollutants that may negatively affect the functioning of the Arctic's soil-based terrestrial ecosystems. There is almost no research on the actual HM content in the soils of Novaya Zemlya (NZ), and the purpose of this work is to assess the HM content in the soils of Severny Island in the NZ archipelago. The study was performed at Russkaya Gavan, Ledyanaya Gavan, Blagopoluchiya Bay, and Cape Zhelaniya. The soil cover in the northern part of Severny Island has a mosaic structure. On Severny Island, Cryosols (Loamic) are the most common soils among the soils studied in this work. Soils of the study regions on Severny Island are mostly loamy and clayey. The proportion of physical clay increases down the profiles. All study soils of NZ are alkaline and highly alkaline. In general, study soils have an acceptable level of HM contamination. The weighted average HM gross content in them varies insignificantly; however, the following elements exceed their threshold concentrations: Fe (1.1 clarke) – Russkaya Gavan bay; Fe (1.2 clarke), Cr (1.1 clarke), V (1.1 maximum permissible concentration (MPC)), Ti (1.1 clarke) – Blagopoluchiya bay; Fe (1.3 clarke) – Ledyanaya Gavan bay. This, apparently, is caused by their high contents in the soil-forming rock. The results obtained confirm the necessity to monitor the study territories in order to be able to assess the degree of pollution and prevent the risk of an environmental disaster in the future
新地岛塞弗尼岛土壤重金属分布评价
全球变暖在极地纬度地区发生得最快,增加了这些地区的经济可及性,因此带来了技术污染的风险。重金属(HM)是最常见的技术污染物之一,可能对北极土壤陆地生态系统的功能产生负面影响。关于新地岛(new Zemlya, NZ)土壤中HM含量的实际研究几乎没有,本研究的目的是评估新西兰群岛塞弗尼岛(Severny Island)土壤中HM含量。这项研究是在Russkaya Gavan, Ledyanaya Gavan, Blagopoluchiya湾和Zhelaniya角进行的。塞弗尼岛北部的土壤覆盖层呈马赛克结构。在塞弗尼岛,低温土(Loamic)是本研究中最常见的土壤。塞弗尼岛研究区的土壤以壤土和粘土为主。物理粘土的比例沿剖面增加。新西兰所有的研究土壤都是碱性和高碱性的。一般来说,研究土壤的HM污染水平是可以接受的。加权平均HM总含量差异不显著;然而,以下元素超过其阈值浓度:铁(1.1 clarke) - Russkaya Gavan bay;Fe (1.2 clarke), Cr (1.1 clarke), V(1.1最大允许浓度(MPC)), Ti (1.1 clarke) - Blagopoluchiya bay;Fe (1.3 clarke) - Ledyanaya Gavan海湾。这显然是由于它们在造土岩石中的高含量造成的。所获得的结果证实了监测研究区域的必要性,以便能够评估污染程度并防止未来发生环境灾害的风险
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Journal of Siberian Federal University - Biology
Journal of Siberian Federal University - Biology Agricultural and Biological Sciences-Agricultural and Biological Sciences (all)
CiteScore
0.80
自引率
0.00%
发文量
8
审稿时长
24 weeks
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