Isotope Source Signatures for a Primary Lead Smelter Located Close to Todos os Santos Bay, Brazil

From 1960 to 1993, a primary lead smelter operated in the Santo Amaro region, close to Todos os Santos Bay in Brazil, using the classical sinter-roasting process followed by smelting and refining. A high lead content was found in the sediments from Todos os Santos Bay, which has a large circulation...

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Bibliographic Details
Published in:Soil & sediment contamination 2011-01, Vol.20 (6), p.672-687
Main Authors: de Andrade Lima, L. R. P, Bernardez, L. A
Format: Article
Language:English
Subjects:
characterization
Contaminated sediments
Correlation analysis
effluents
Fractionation
Heavy metals
Isotope fractionation
isotope geochemistry
Isotopes
Lead
lead smelter
metallurgy
Mineralization
refining
Rivers
sediments
Slag
slags
Smelters
Smelting
soil
South America
Stable isotopes
X-radiation
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Summary:From 1960 to 1993, a primary lead smelter operated in the Santo Amaro region, close to Todos os Santos Bay in Brazil, using the classical sinter-roasting process followed by smelting and refining. A high lead content was found in the sediments from Todos os Santos Bay, which has a large circulation and receives the discharge from three rivers. Lead stable isotope ratios provide information about the ore mineralization and can be used to evaluate the origin and fate of the lead pollution. The objective of this study is to identify the isotopic signature of the major effluents of this lead smelter and correlate it with the origin of the galena concentrate that generated it. The X-ray microanalysis confirms that the lead occurs in the slag in the metallic state. The soil has a high lead content (about 0.90%) of oxidized lead. The lead isotopic ratios indicated that the slag isotopic ratios (²⁰⁸Pb/²⁰⁴Pb = 34.8; ²⁰⁷Pb/²⁰⁴Pb = 15.3; ²⁰⁶Pb/²⁰⁴Pb = 15.1) are close to the soil value (²⁰⁸Pb/²⁰⁴Pb = 36.2; ²⁰⁷Pb/²⁰⁴Pb = 15.9; ²⁰⁶Pb/²⁰⁴Pb = 16.4) and both agree with the values for the galena from the Boquira mine region (²⁰⁸Pb/²⁰⁴Pb = 34.6±1.1; ²⁰⁷Pb/²⁰⁴Pb = 15.3±0.4; ²⁰⁶Pb/²⁰⁴Pb = 14.7±0.2). These results indicate that no isotopic fractionation occurred in the roasting-smelting process, therefore the original Boquira isotope ratios can be used as the isotopic signature of the lead dispersed from the Santo Amaro smelter.
ISSN:1549-7887
1532-0383
1549-7887
DOI:10.1080/15320383.2011.594109