DYNAMICS OF COPPER, LEAD, MERCURY AND ARSENIC CONCENTRATION IN SEDIMENTS OF THE COPIAPÓ RIVER, CHILE

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Sebastián Rojos
Germán Aguilar
Bernardo Sepúlveda
Osvaldo Pavez

Abstract

The Copiapó river basin, to the south of the Atacama desert, has a strong anthropic intervention due to mining, agricultural and urban activities. The presence of mining environmental tailings in the basin is relevant, mainly when they are close to watercourses and populated areas. In this work the relationship between the variations of copper, lead, mercury and arsenic concentrations related to the sediment transport dynamics along a year was studied. From five points along the Copiapó river, including areas of mining, agricultural and urban intervention, the sediments were analyzed for granulometry and chemical composition. The results show that the temporal variation of elements concentrations was proportionally inverse to the transport of the finest fraction of the sediment. This is related to changes in sediments transport, influenced by sporadic rains, snow melting, sediment supply from upstream sediments and wind events in areas with mining activity.

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Author Biographies

Germán Aguilar, Centro Avanzado de Tecnología para la Minería, AMTC- Universidad de Chile. Av. Tupper 2007, Santiago, Chile.

Dr. en Geología.

Bernardo Sepúlveda, Centro Regional de Investigación para el Desarrollo Sustentable de Atacama, CRIDESAT- Universidad de Atacama, Copayapu 485, Región de Atacama, Copiapó, Chile

Dr. Cs. Biológicas de la Universidad de Chile. Coordinador de investigación, Línea de Recursos Naturales, en el Centro Regional de Investigación para el Desarrollo Sustentable de Atacama (CRIDESAT) de la Universidad de Atacama, Región de Atacama, Tercera Región, chile.

Osvaldo Pavez, Centro Regional de Investigación para el Desarrollo Sustentable de Atacama, CRIDESAT- Universidad de Atacama, Copayapu 485, Región de Atacama, Copiapó, Chile Departamento de Ingeniería en Metalurgia, Universidad de Atacama, Chile.

Dr. en Metalurgia, Director del CRIDESAT.

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