上西里西亚工业区中部(波兰南部)历史铅锌矿开采和铁锌冶炼引起的土壤污染

A. Pasieczna
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引用次数: 0

摘要

这项工作的目的是确定上西里西亚工业区中部土壤中重金属、砷和硫的积累程度。重工业、金属矿石和硬煤的开采、铁和有色冶金以及工业和城市污水的排放造成了该地区自然环境的严重退化。测定了上西里西亚工业区中部地区土壤中Ag、Al、As、Ba、Ca、Cd、Co、Cr、Cu、Fe、Hg、Mg、Mn、Mo、Ni、P、Pb、S、Sr、Ti、V、i、Zn等21种元素的含量。根据污染因子、富集因子和地质堆积指数对土壤的污染程度进行了评价。测试显示,金属、砷和硫的含量升高,超过了区域地球化学背景的水平。因子分析使得将化学元素组合成组成为可能,这些化学元素可能来自相同的岩性或/和人为来源。
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SOIL CONTAMINATION INDUCED BY HISTORICAL ZINC-LEAD ORE MINING AND IRON AND ZINC SMELTING IN THE CENTRAL PART OF THE UPPER SILESIAN INDUSTRIAL REGION (SOUTHERN POLAND)
The purpose of the work was to determine the degree of accumulation of heavy metals, arsenic and sulphur in the soils of the central part of the Upper Silesian Industrial Region. Heavy industry, mining of metal ores and hard coal, iron and non-ferrous metallurgy as well as the discharge of industrial and municipal sewage caused a strong degradation of the natural environment of this area. The content of twenty one elements (Ag, Al, As, Ba, Ca, Cd, Co, Cr, Cu, Fe, Hg, Mg, Mn, Mo, Ni, P, Pb, S, Sr, Ti, V i Zn) have been assayed in the soils of central part Upper Silesian Industrial Region. The contamination of the soils was assessed on the basis of contamination factors, enrichment factors and geoaccumulation indexes. The tests revealed elevated content of metals, arsenic and sulphur exceeding the levels of the regional geochemical background. Factor analysis made it possible to combine chemical elements into groups, probably derived from the same lithological or/and anthropogenic sources.
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ZŁOTO W POTOKACH I PEGMATYCIE Z REJONU STRZELINA ROZPOZNANIE LOKALIZACJI WYROBISK PIASKÓW I ŻWIRÓW WZGLĘDEM GRANIC GZWP ORAZ CIEKÓW POWIERZCHNIOWYCH NA OBSZARZE WOJEWÓDZTWA ŚLĄSKIEGO INTERPRETACJA ZMIENNOŚCI TEMPERATURY WODY W ŹRÓDLE NA WSCHODNIM STOKU ZAMECZKÓW (TATRY ZACHODNIE) NA PODSTAWIE CIĄGŁYCH OBSERWACJI MONITORINGOWYCH I NUMERYCZNEGO MODELU TRANSPORTU CIEPŁA PARAMETRY MIGRACJI ZANIECZYSZCZEŃ W ODPADACH FLOTACYJNYCH NA PODSTAWIE TERENOWEGO EKSPERYMENTU ZNACZNIKOWEGO NA PRZYKŁADZIE OBIEKTU UNIESZKODLIWIANIA ODPADÓW WYDOBYWCZYCH „GILÓW” ZRÓŻNICOWANIE TŁA HYDROGEOCHEMICZNEGO WÓD PODZIEMNYCH EKSPLOATOWANYCH W ZLEWNI BIEBRZY
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