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首页> 外文期刊>Почвоведение >Trace Elements in AI-Fe-Humus Podzolic Soils Subjected to Aerial Pollution from the Copper-Nickel Production Industry in Conditions of Varying Lithogenic Background
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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:在成岩背景不同的条件下,受到铝-镍生产行业的空气污染的AI-Fe-腐殖质块状土壤中的微量元素

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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:考虑到大量的数据,这些数据来自不同类型的岩石,并且受到不同水平的空气污染,导致AI-Fe-腐殖质块状土壤中的微量元素浓度上升,而铜和镍生产行业却是如此。第四纪沉积物上土壤剖面的元素分布具有共同规律。稀土元素,act系元素,Rb,Cs和Sc显示出坡型分布,而Zr和Hf倾向于在最顶层的矿物层中积累。发现了Cu,Ni,Co,Ag,Au,Se,Sb和Ir的生物累积。在受污染的土壤中,这些元素在有机层中的积累尤为明显。在严重的大气污染条件下,有机土壤视野是这些元素的生物地球化学屏障,最终导致了工业贫瘠地带的发展。由于有机层的屏障作用,这些元素在矿质土壤层中的分布完全受成岩因子控制。

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