Journal
JOURNAL OF GEOCHEMICAL EXPLORATION
Volume 111, Issue 3, Pages 160-171Publisher
ELSEVIER
DOI: 10.1016/j.gexplo.2011.04.009
Keywords
Trace element mobility; Geochemical speciation; Sequential extraction; Mining soils; Ervedosa mine
Categories
Funding
- FCT (Portuguese Foundation for Science and Technology) [PTDC/CTE-GEX/66710/2006]
- Fundação para a Ciência e a Tecnologia [PTDC/CTE-GEX/66710/2006] Funding Source: FCT
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Total concentrations of chemical elements in soils may not be enough to understand the mobility and bioavailability of the elements. It is important to characterise the degree of association of chemical elements in different physical and chemical phases of soil. Another geochemical characterisation methodology is to apply sequential selective chemical extraction techniques. A seven-step sequential extraction procedure was used to investigate the mobility and retention behaviour of Al, Fe, Mn, Cu. Zn, Pb, Cr, Co, Ni, Mo, Cd, Bi. Sn, W, Ag, As and U in specific physical-chemical and mineral phases in mine tailings and soils in the surroundings of the abandoned Ervedosa mine. The soil geochemical data show anomalies associated with mineralised veins or influenced by mining. Beyond the tailings, the highest recorded concentrations for most elements are in soils situated in mineralised areas or under the influence of tailings. The application of principal components analysis allowed recognition of (a) element associations according to their geochemical behaviour and (b) distinction between samples representing local geochemical background and samples representing contamination. Some metal cations (Mn, Cd, Cu, Zn, Co, Cr, Ni) showed important enrichment in the most mobilisable and bioavailable (i.e., water-soluble and exchangeable) fractions due likely to the acidic conditions in the area. In contrast, oxy-anions such as Mo and As showed lower mobility because of adsorption to Fe oxy-hydroxides. The residual fraction comprised largest proportions of Sn and Al and to a lesser extent Zn, Pb, Ni, Cr, Bi, W, and Ag, which are also present at low concentrations in the bioavailable fractions. The elements in secondary mineral phases (mainly Fe, Mn, Cu, Zn, Cd, Pb, W, Bi, Mo, Cr, Ni, Co, As and U) as well as in organic matter and sulphides are temporarily withheld, suggesting that they may be released to the environment by changes in physico-chemical conditions. (C) 2011 Elsevier B.V. All rights reserved.
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