Atmospheric Pollution from a Storage of Tungsten–Molybdenum Ore Mining and Processing Wastes

IF 0.7 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS
A. M. Plyusnin, Yu. S. Voronina, A. V. Ukraintsev, M. K. Chernyavskii, E. G. Peryazeva, E. P. Chebykin
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Abstract

Experimental studies of the surface atmosphere pollution with mining and processing wastes of tungsten–molybdenum ore were carried out using an equipment devised for collecting aerosols above the surface of sands. It has been established that toxic components formed during the decomposition of residual sulfide mineralization and products of interaction between acidic waters and rocks are transported with water vapor from the sands to the surface. The moisture condensed over the sands contains high concentrations of aluminum, fluorine, iron, silicon, manganese, zinc, and phosphorus. These elements form an atmospheric pollution halo over the technogenic sands and are further dispersed by air currents over neighboring areas. In winter, the snow cover is polluted over a vast territory due to wind dispersion of the aerosols. The halo of pollution extends over tens of square kilometers. A dependence was identified of qualitative and quantitative composition of the components polluting the snow cover on the storage time of the ore processing products. It is shown that some of the toxic elements pass into solution during snow melting from suspended solids, which are brought by wind from the territory where the soil cover is disturbed by mining.

Abstract Image

钨钼矿开采和加工废料贮存产生的大气污染
摘要-- 利用一种用于收集沙地表面气溶胶的设备,对钨钼矿开采和加工废料造成的地表大气污染进行了实验研究。研究结果表明,残留硫化物矿化分解过程中形成的有毒成分以及酸性水与岩石相互作用的产物会随水蒸气从泥沙中飘移到地表。凝结在泥沙上的水汽含有高浓度的铝、氟、铁、硅、锰、锌和磷。这些元素在科技沙的上空形成大气污染晕,并通过气流进一步扩散到邻近地区。在冬季,由于气溶胶随风飘散,广袤的雪层受到污染。污染晕的范围达数十平方公里。研究发现,雪层污染成分的质量和数量组成与矿石加工产品的储存时间有关。研究表明,在融雪过程中,一些有毒元素会从悬浮固体中进入溶液,这些悬浮固体是由风从采矿扰动土壤覆盖层的地区带来的。
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来源期刊
Geochemistry International
Geochemistry International 地学-地球化学与地球物理
CiteScore
1.60
自引率
12.50%
发文量
89
审稿时长
1 months
期刊介绍: Geochemistry International is a peer reviewed journal that publishes articles on cosmochemistry; geochemistry of magmatic, metamorphic, hydrothermal, and sedimentary processes; isotope geochemistry; organic geochemistry; applied geochemistry; and chemistry of the environment. Geochemistry International provides readers with a unique opportunity to refine their understanding of the geology of the vast territory of the Eurasian continent. The journal welcomes manuscripts from all countries in the English or Russian language.
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