Fractions and background concentrations of potentially toxic elements in Hungarian surface soils

被引:22
|
作者
Rekasi, Mark [1 ]
Filep, Tibor [1 ]
机构
[1] Agr Res Ctr, Inst Soil Sci & Agr Chem, H-1022 Budapest, Hungary
关键词
Soil quality standards; Soil contamination limit; Toxic elements; Element mobility; HEAVY-METALS; TRACE-ELEMENTS; AVAILABILITY; EXTRACTION; CADMIUM; CD; RYEGRASS; MOBILITY; COPPER; ZINC;
D O I
10.1007/s10661-011-2513-9
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
This work established background concentrations for the pseudo total (HNO3 + H2O2-soluble), mobilisable (NH4-acetate + EDTA-soluble) and mobile (1 M NH4NO3-soluble) element fractions of Hungarian surface soils that can be used as reference values for the soil quality standards. The 193 soils investigated were taken from the Hungarian Soil Information and Monitoring System. The background values for Al, As, B, Cd, Co, Cr, Cu, Mn, Ni, Pb, Sr and Zn were given as a range covering 95% of the variance of the representative samples. The differences between observed element concentrations and the calculated background values indicated anthropogenic or pedogenic impact in each fraction. The comparison of the calculated background values with the Hungarian quality standards and the contamination limit values of other countries showed that the limit values of a certain region or country are not suitable for other areas. Generally, Mn and Al had the highest, while Cd had the lowest concentration in each fraction. Cr and Al were the least and Sr was the most mobile element. The principal component analysis indicated different geochemical and physico-chemical behaviour of the elements in the fractions; the pseudo total fraction was influenced more by the geological behaviour, while mobilisable and mobile fraction explained a much higher proportion of the total variance of soil physico-chemical properties than soil geochemical properties. The Cd-Ni and Co-Mn element pairs were always in the same principal component in each fractions indicating similar geogenic origin and showing that their solubility changes are similar in function of soil properties.
引用
收藏
页码:7461 / 7471
页数:11
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