Mineralogical control on arsenic release during sediment?wáter interaction in abandoned mine wastes from the Argentina Puna

NIEVA NANCY EUGENIA, ; LAURA . BORGNINO; MARIA GABRIELA GARCIA

SCIENCE OF THE TOTAL ENVIRONMENT

ELSEVIER SCIENCE BV

Lugar: Amsterdam; Año: 2016 vol. 550 p. 1141 - 1151

0048-9697

The sulfide-rich residues of La Concordia mine, Argentina Puna, are accumulated in tailing dams that remained exposed to the weathering agents for almost 30 years. In such period of time, a complex sequence of redox and dissolution/precipitation reactions occurred, leading to the gradual oxidation of the wastes and the formation of weathering profiles. The sources of arsenic in the wastes were analyzed by XRD and SEM/EDS analysis while a standardized sequential extraction procedure was followed to define solid As associations. In addition, the release of As during sediment?water interaction was analyzed in a period of 10 months. The results indicate that primary As-bearing minerals are arsenian pyrite and polymetallic sulfides. As-jarosite and scarce arsenatesare the only secondary As-bearing minerals identified by XRD and SEM/EDS. However, the rapid release (i.e., b1 h) of arsenic from suspensions of the studied sediments in water, seems to be associated to the dissolution of highly soluble (hydrous)sulfates, as it was determined in samples of the efflorescences that cover the entire site. Contributions from the more abundant As-jarosite are also expected in longer periods of sediment? water interaction, due to its low rate of dissolution in acid and oxic conditions. Finally, near 30% of As remains