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Trace Elements in AI-Fe-Humus Podzolic Soils Subjected to Aerial Pollution from the Copper-Nickel Production Industry in Conditions of Varying Lithogenic Background

机译:AI-Fe-Humus豆荚土壤中的微量元素对铜镍生产工业的空中污染,改变岩性背景条件

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摘要

Numerous data on the concentration of trace elements in AI-Fe-humus podzolic soils developing from fifferent types of rocks and subjected to different levels of aerial pollution froom the copper and nickel production industry are considered. The distribution of elements by the profiles of soils on Quaternary sediments has common regularities. Rare-earth elements, actinides, Rb, Cs, and Sc display an eluvial type of distribution, whereas Zr and Hf tend to accumulate in topmost mineral horizons. Biogenic accumulation is found for Cu, Ni, Co, Ag, Au, Se, Sb, and Ir. In polluted soils, the accumulation oof these elements in organic horizons becomes especial ly well manifested. Organic soil horizons are biogeochemical barriers for these elements in conditions of severe atmospheric pollution that, eventually, leads to the development of industrial barrens. Owing to the barrier effect of organic horizons, the distribution of these elements in mineral soil horizons in fully controlled by the lithogenic factor.
机译:众多关于从消融类型的岩石中发育的AI-Fe-Humus豆类土壤中微量元素浓度的数据,考虑了铜和镍生产行业的不同水平的岩石污染。季沉积物上土壤谱分布的元素分布具有共同规则。稀土元素,散氨酸,RB,CS和SC显示出一种抗菌类型的分布,而Zr和Hf倾向于在最顶层矿物视野中积聚。发现了铜,Ni,Co,Ag,Au,Se,Sb和Ir的生物累积。在污染的土壤中,有机视野中这些元素的积累OOF变得特别好。有机土壤视野是这些元素在严重大气污染条件下的生物地球化学障碍,最终导致工业贫瘠的发展。由于有机视野的阻隔效果,通过岩油原因受到矿物土地区的这些元素的分布。

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