Numerous areas have been contaminated by heavy metals and metalloids due to
industrial and mining activities. Studies investigating the behavior of su
ch contaminants in the environment have identified speciation as a key fact
or controlling their mobility, availability and toxicity. Here we character
ize As- and Pb-bearing phases resulting from the oxidation of sulfide-rich
tailings of a former gold mine (La Petite Faye, France) in order to assess
the risk for water quality. Elements were first pre-concentrated by granulo
metric fractionation (sedimentation in deionized water) and then investigat
ed using X-ray diffraction and electron microprobe analyses. Two main As-Pb
-bearing minerals were clearly identified: scorodite (FeAsO4 . 2H(2)O) and
beudantite PbFe3(AsO4)(SO4)(OH)(6). Minor amounts of As and Pb were dissolv
ed in deionized water during granulometric fractionation, indicating the po
ssible presence of other soluble Pb-sulfates which could be some of the pri
mary metastable products of sulfide oxidation. This dissolution also provid
es information about the fate of these phases in the case of intensive leac
hing of the tailings. Scorodite may not be considered as a relevant candida
te for As on-site immobilization, because its solubility largely exceeds dr
inking water standards whatever the pH. Since beudantite solubility has not
yet been determined, an estimation of its solubility product was obtained
using the Gibbs free energy of formation of plumbojarosite [Pb0.5Fe3(SO4)(2
)(OH)(6)]. This estimation suggests that beudantite should efficiently main
tain low Pb concentration in waters. However, Pb dissolution in deionized w
ater during the granulometric fractionation led to Pb concentrations much h
igher than the French and US drinking water standards (2.4 x 10(-7) mol l(-
1)), which may be due to dissolution of the suspected metastable Pb-sulfate
s. Accurate determination of beudantite solubility is now required to impro
ve the Pb risk assessment on such polluted sites. (C) 2000 Elsevier Science
S.A. All rights reserved.