Trace elements in Al-Fe-humus podzolic soils subjected to aerial pollutionfrom the copper-nickel production industry in conditions of varying lithogenic background

Citation
Vv. Nikonov et al., Trace elements in Al-Fe-humus podzolic soils subjected to aerial pollutionfrom the copper-nickel production industry in conditions of varying lithogenic background, EURAS SOIL, 32(3), 1999, pp. 338-349
Citations number
24
Categorie Soggetti
Agriculture/Agronomy
Journal title
EURASIAN SOIL SCIENCE
ISSN journal
10642293 → ACNP
Volume
32
Issue
3
Year of publication
1999
Pages
338 - 349
Database
ISI
SICI code
1064-2293(199903)32:3<338:TEIAPS>2.0.ZU;2-6
Abstract
Numerous data on the concentration of trace elements (Rb, Cs, Ag, Au, Sr, B a, Zn, Cd, Sc, La, Ce, Nd, Sm, Eu, Gd, Tb, Yb, Th, U, Zr, Hf, As, Sb, V, Ta , Se, Cr, Mo, W, Co, Ni, Br, and Ir) in Al-Fe-humus podzolic soils developi ng from different types of rocks and subjected to different levels of aeria l pollution from the copper and nickel production industry are considered. The distribution of elements by the profiles of soils on Quaternary sedimen ts has common regularities. Rare-earth elements, actinides, Rb, Cs, and Sc display an eluvial type of distribution, whereas Zr and Hf tend to accumula te in topmost mineral horizons. Biogenic accumulation is found for Cu, Ni, Co, Ag, Au, Se, Sb, and Ir. In polluted soils, the accumulation of these el ements in organic horizons becomes especially well manifested. Organic soil horizons are biogeochemical barriers for these elements in conditions of s evere atmospheric pollution that, eventually, leads to the development of i ndustrial barrens. Owing to the barrier effect of organic horizons, the dis tribution of these elements in mineral soil horizons is fully controlled by the lithogenic factor.