Arsenic and trace metals in river water and sediments from the southeast portion of the Iron Quadrangle, Brazil

• Autor(a) principal: Varejão, Eduardo V. V.
• Data de Publicação: 2010
• Outros Autores: Bellato, Carlos R., Fontes, Maurício P. F., Mello, Jaime W. V.
• Tipo de documento: Artigo
• Idioma: eng
• Título da fonte: LOCUS Repositório Institucional da UFV
• Texto Completo: http://dx.doi.org/10.1007/s10661-010-1361-3; http://www.locus.ufv.br/handle/123456789/19812
• topic: Fractionation; Sequential extraction; Bioavailability

The Iron Quadrangle has been one of the most important gold production regions in Brazil since the end of the seventeenth century. There, arsenic occurs in close association with sulfide-rich auriferous rocks. The most abundant sulfide minerals are pyrite and arsenopyrite, yet trace metal sulfides occur in subordinate phases as well. Historical mining activities have been responsible for the release of As and trace metals to both aquatic and terrestrial environments close to mining sites in the region. Therefore, this study was aimed to evaluate the distribution and mobility of As, Cd, Co, Cr, Cu, Ni, Pb, and Zn in streams in the southeast portion of the Iron Quadrangle between the municipalities of Ouro Preto and Mariana, the oldest Brazilian Au mining province. Total concentrations of some trace metals and arsenic in water were determined. The four-stage sequential extraction procedure proposed by the commission of the European Communities Bureau of Reference (BCR) was used to investigate the distribution of these elements in stream sediments. Arsenic concentration in water was >10 μg L ^− 1 (maximum limit permitted by Brazilian environmental regulations for water destined for human consumption) at all sampling sites, varying between 36.7 and 68.3 μg L ^− 1. Sequential extraction in sediments showed high concentrations of As and trace metals associated with easily mobilized fractions.