Lomonosov Moscow State University, Leninskie gory 1, Moscow 119991, Russia.
Lomonosov Moscow State University, Leninskie gory 1, Moscow 119991, Russia.
Sci Total Environ. 2018 Nov 15;642:63-76. doi: 10.1016/j.scitotenv.2018.06.042. Epub 2018 Jun 18.
Mining of mineral resources exerts strong impact on the environment and leads to irreversible changes in vegetation, soils, atmosphere, surface and ground waters. The aim of this study is to assess the modern geochemical state of soil cover in Zakamensk, a city located in Buryat Republic (Russia) and known as one of the biggest ore mining center in the former Soviet Union. The center was operating for 68 years and closed 17 years ago. Soil-geochemical survey was conducted in 2012 and included collection of 103 soil samples in Zakamensk and 27 samples in the background areas. The bulk contents of 16 potentially toxic elements (PTEs) in the soil samples were determined by mass spectrometry and by atomic emission spectrometry with inductively coupled plasma. Background sites are characterized by increased concentrations of ore elements W and Mo. The mineral deposit development and physical and chemical weathering of tailings' material have led to a sharp increase in Bi, Cd, Cu, Mo, Pb, Sb, W and Zn levels in the soils of different land-use areas. Near the tailings, the concentration of Sb in soils was 356 times higher than in the background area; Cd - 70 times; Mo, Bi, Cu, and W - 42-55 times; Pb and As - 34-37 times; and Zn and Sn - 6-12 higher. In the north of the city a prominent anomaly of PTEs occurs in sandy sediments of the Modonkul floodplain. It was formed due to the washout and subsequent sedimentation of suspended matter carried by the Modonkul River from the Barun-Naryn, the Dzhida, and emergency tailings. So, the anthropogenic activities are the most important source of ore and accompanying elements in the urban soils. High levels of accessory elements also depends on natural factors such as physicochemical properties of soils, position in the landscape, and genesis of parent materials. The environmental assessment of topsoils in Zakamensk showed that Pb, Sb, Cd, and As concentrations exceeds the Russian MPCs by 1.7-7.8 times, which creates a significant hazard for the environment and adversely affects human health.
采矿活动对环境产生强烈影响,导致植被、土壤、大气、地表水和地下水发生不可逆转的变化。本研究旨在评估俄罗斯布里亚特共和国扎卡缅斯克(Zakamensk)的土壤覆盖的现代地球化学状况,该市是前苏联最大的矿石开采中心之一。该中心运营了 68 年,17 年前关闭。土壤地球化学调查于 2012 年进行,包括在扎卡缅斯克采集 103 个土壤样本和在背景区采集 27 个样本。通过质谱法和电感耦合等离子体原子发射光谱法测定了土壤样品中 16 种潜在有毒元素(PTE)的总量。背景区的矿石元素 W 和 Mo 浓度较高。矿床的开发和尾矿物质的物理化学风化导致不同土地利用区土壤中 Bi、Cd、Cu、Mo、Pb、Sb、W 和 Zn 水平急剧增加。在尾矿附近,土壤中 Sb 的浓度比背景区高 356 倍;Cd 为 70 倍;Mo、Bi、Cu 和 W 为 42-55 倍;Pb 和 As 为 34-37 倍;Zn 和 Sn 为 6-12 倍。在城市北部,莫东库勒洪泛区的沙质沉积物中出现了显著的 PTE 异常。这是由于莫东库勒河从巴伦-纳伦河、吉达河和应急尾矿中冲刷和随后沉积悬浮物而形成的。因此,人为活动是城市土壤中矿石和伴生元素的最重要来源。辅助元素的高含量也取决于自然因素,如土壤的物理化学性质、景观位置和母质的成因。扎卡缅斯克表层土壤的环境评估表明,Pb、Sb、Cd 和 As 的浓度比俄罗斯 MPC 高出 1.7-7.8 倍,这对环境构成了重大威胁,并对人类健康产生不利影响。