Trace element speciation in selected smelter-contaminated soils in Anaconda and Deer Lodge Valley, Montana, USA

• Published in: Advances in environmental research : an international journal of research in environmental science, engineering and technology Vol. 8; no. 1; pp. 51 - 67
• Main Authors: Burt, R, Wilson, M.A, Keck, T.J, Dougherty, B.D, Strom, D.E, Lindahl, J.A
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 01.10.2003
• Subjects: Anthropogenic; Fractionation; Heavy metals; USA, Montana, Deer Lodge Valley; USA, Montana, Anaconda; Fractionation; Anthropogenic; Heavy metals
• ISSN: 1093-0191; 1093-7927
• DOI: 10.1016/S1093-0191(02)00140-5

Long-term copper smelting in the Anaconda and Deer Lodge Valley area of Montana has resulted in an extensive area of trace element contamination. Aerial extent of contamination is generally established, but total analysis of soils does not correlate to relative degree of impact on vegetation growth. Three pedons (Beaverell, Cetrack and Judco) were analyzed by routine soil characterization methods, aqua regia microwave digestion, sequential chemical extraction, and X-ray diffraction analysis with the objective of providing a better understanding of chemical forms and potential reactivity of selected trace elements (Cd, Co, Cr, Cu, Hg, Mn, Ni, P, Pb). Surface horizons of soils are more acidic than subsoils, with pH for all horizons ranging from 4.0 to 8.7. Beaverell is the most contaminated in the upper 20 cm with the sum of total extractable (SUM TE) trace elements by microwave digestion ranging from 1836 to 3605 mg kg −1, largest H 2O-soluble (WS) and exchangeable (EX) fractions (e.g. 1.6 and 9.3%, respectively), and smallest residual (RES) fraction (e.g. 14.3%). Cetrack has greater SUM TE elements than Judco, though a lower WS+EX fraction due to the effects of alkaline pH, carbonates and high P. Oxide (OX), organic matter/sulfide (OM/S), and RES fractions predominate over WS, EX, and specially-sorbed/carbonate-bound fractions (SS/CAR) for all horizons. Copper, Zn, Pb and Cd are elevated in surface over subsurface horizons in these latter fractions, indicating these elements were anthropogenic additions. X-ray data indicate that Pb, Cu, Cr and Cd partially exists as both OX and sulfide mineral forms.