Interactions of soil components and their effects on speciation of chromium in soils

Citation
M. Pantsar-kallio et al., Interactions of soil components and their effects on speciation of chromium in soils, ANALYT CHIM, 439(1), 2001, pp. 9-17
Citations number
32
Categorie Soggetti
Spectroscopy /Instrumentation/Analytical Sciences
Journal title
ANALYTICA CHIMICA ACTA
ISSN journal
00032670 → ACNP
Volume
439
Issue
1
Year of publication
2001
Pages
9 - 17
Database
ISI
SICI code
0003-2670(20010717)439:1<9:IOSCAT>2.0.ZU;2-Q
Abstract
For evaluation of real risks of soil contaminated with chromium it is impor tant to identify and understand the reactions of Cr species with main soils components. In this research reactions of Cr(III) and Cr(VI) with Fe(OH)(3 ), MnO3, CaCO3, kaolinite and natural organic matter (NOM) were examined in batch experiments. Since the batches were compositions of soil component m ixtures the experimental design was carried out by applying Simplex algorit hm and the results of the experimental domain were interpreted by partial l east squares (PLS), The research confirmed the significance of studying all the soil components simultaneously instead of studying only the effects of one component at a time, The ability of pure components to change the speciation of Cr(III) an d Cr(VI) in liquid phase was different to that in mixtures, which indicated that the soil components interacted with each other. The order of pure com ponents to convert Cr(III) by adsorption, precipitation or oxidation was Fe (OH)(3) = kaolinite = CaCO3 > NOM > MnO2, while in mixtures the order was: Fe(OH)(3) > CaCO3 > kaolinite > MnO2 > NOM. This means that in mixtures wit h the highest amount of Fe(OH)(3) the conversion of Cr(III) was highest. In mixtures with the highest amount of NOM the changes in speciation of disso lved Cr(III) were the lowest. The order for the pure components to change t he speciation of Cr(VI) was: Fe(OH)(3) > NOM > kaolinite > CaCO3 > MnO2 and in mixtures the order was: NOM > Fe(OH)(3) > kaolinite > MnO2 > CaCO3. The reactions between different soil components also affected the oxidation /reduction ability of soils. As separate component MnO2 oxidized Cr(III) to Cr(VI). However, in mixtures with NOM or Fe(OH)3 the oxidation was hindere d, The effect of pH on speciation of Cr in mixtures was also examined and i s discussed. (C) 2001 Elsevier Science B.V. AU rights reserved.